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Journal of Medicine and Pharmacy","Tạp chí Y Dược học Cần Thơ",{"EN":575,"VI":576},"\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">04\u002F10\u002F2015 Ministry of Information and Communications allowed Can Tho journal of medicine and pharmacy to operate (102 \u002FGP-BTTTT)\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">07\u002F16\u002F2015 Can Tho journal of medicine and pharmacy is internationally recognized: ISSN 2354-1210\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">In 2016, The journal has been included in the list of medical science journals by The State Council for professorship which is awarded a work score of 0-0.5 points for a published article.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Can Tho Journal of Medicine and Pharmacy welcome original works that haven’t been submitted or published in other medical journals. Posts must contain content related to one of the journal’s categories.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">The content published\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">The journal is divided into 3 categories:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Scientific research article: are valuable scientific works, which have been researched and accepted.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Overview of medicine, biology and pharmacy: serving the objective of continuing training in the fields of medicine, biology and pharmacy; to systematize classical and modern knowledge.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Update information on new knowledge about medicine, biology, pharmacy in the country and in the world.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Scope\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Publication and introduction of scientific research in the fields:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">+ Medicine (internal medicine, surgery, pediatrics, obstetrics and gynecology, odonto-stomatology, laboratory, oncology, traditional medicine, nursing).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">+ Biology (genetics, biotechnology).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">+ Pharmacology (pharmaceutics, drug quality analysis-control, synthetic pharmaceutical chemistry, biochemistry, pharmacognosy, botany, clinical pharmacy).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- To enhance the quality of undergraduate, postgraduate education, scientifically researching and meet the necessary treatment in hospital.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Introducing the updated domestic and oversea information about science technology to promote scientific research and exchanging technology in local, other universities.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Exchanging pharmaceutical and medical information for social health developing in the Mekong Delta and Vietnam.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">The object\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Postgraduate students, student of Can Tho University of Medicine and Pharmacy, scientists from schools, research institutes, hospitals, health centers, pharmaceutical companies of the Mekong Delta; other provinces and regions in Vietnam and other country.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Address\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Headquarters of Can Tho Journal of Medicine and Pharmacy, located Scientific Research and International Cooperation Office: 179 Nguyen Van Cu Street, An Khanh Ward, Ninh Kieu District, Can Tho City, Vietnam.\u003C\u002Fspan>\u003C\u002Fp>","\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Ngày 16\u002F7\u002F2015, Tạp chí Y Dược học Cần Thơ được cấp chỉ số quốc tế: ISSN 2354-1210.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Từ tháng 4\u002F2016, Tạp chí đã được Hội đồng Giáo sư ngành Y đưa vào danh sách các tạp chí khoa học Y học được tính điểm công trình 0-0,5 điểm cho một bài báo đăng.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Năm 2020 Tạp chí Y Dược học Cần Thơ đã được phê duyệt vào danh mục của các Hội đồng Giáo sư ngành Dược học được tính điểm công trình 0-0,5 điểm cho một bài báo đăng.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ ra 12 số\u002Fnăm, 180-200 trang\u002Fsố.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Từ tháng 12\u002F2022 Tạp chí Y Dược học Cần Thơ là thành viên của hệ thống Crossref và từ tháng 01\u002F2023 tạp chí thực hiện bình duyệt online kín 2 chiều nhằm tăng tính minh bạch, tin cậy của các công trình nghiên cứu khoa học và đảm bảo tốt nhất chất lượng khoa học của bài viết.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tôn chỉ, mục đích và phạm vi của tạp chí\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tôn chỉ và mục đích hoạt động của tạp chí: xuất bản nhằm mục đích phổ biến kết quả từ các đề tài nghiên cứu khoa học; giao lưu trao đổi khoa học, chia sẻ kinh nghiệm, học tập, đồng thời cập nhật thông tin khoa học mới trong các lĩnh vực y, sinh, dược học trong và ngoài nước.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Phạm vi của tạp chí: Tạp chí xuất bản được chia thành 3 chuyên mục: (i) Bài báo nghiên cứu khoa học là kết quả công trình nghiên cứu khoa học có giá trị đã được triển khai nghiên cứu, (ii) Bài tổng quan y, sinh, dược học: phục vụ mục tiêu đào tạo liên tục trong lĩnh vực y, sinh, dược học; nhằm hệ thống hóa những kiến thức kinh điển và hiện đại; (iii) Thông tin cập nhật kiến thức mới về y, sinh, dược học trong nước và trên thế giới.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Chính sách truy cập mở\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ áp dụng chính sách truy cập mở đối với các bài báo đã xuất bản đến với độc giả, nhằm mở rộng cơ hội tiếp cận các kết quả nghiên cứu chất lượng cao và tăng cường trao đổi kiến thức. Tạp chí đăng tải trực tuyến (miễn phí) toàn văn các bài báo được công bố trên website của Tạp chí (https:\u002F\u002Ftapchi.ctump.edu.vn).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Đạo đức xuất bản\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ cam kết tuân thủ đạo đức xuất bản phù hợp với các hướng dẫn và tiêu chuẩn của the Committee on Publication Ethics (COPE), tuân thủ các nguyên tắc của COPE’s Core Practices, Best Practices Guidelines for Journal Editors và Guidelines on Good Publication Practices.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Bản thảo bài báo chỉ được chấp nhận khi được tác giả chịu trách nhiệm chính cam kết các nội dung sau: Các nội dung của bản thảo chưa được đăng tải toàn bộ hoặc một phần ở các tạp chí khác; Tất cả các tác giả đều có đóng góp một cách đáng kể vào quá trình nghiên cứu hoặc chuẩn bị bản thảo và cùng chịu trách nhiệm về các nội dung của bản thảo; Tuân thủ các biện pháp đảm bảo đạo đức nghiên cứu (ví dụ thỏa thuận đồng ý tham gia nghiên cứu).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Cam kết bảo mật\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí cam kết thực hiện và tuân thủ các quy định của luật và các văn bản hướng dẫn liên quan đến bảo mật thông tin cá nhân trên không gian mạng. Các thông tin mà người dùng (tác giả, độc giả, biên tập viên, người phản biện) nhập vào các biểu mẫu trên Hệ thống Quản lý xuất bản trực tuyến của tạp chí chỉ được sử dụng vào các mục đích đã được tuyên bố rõ ràng và sẽ không được cung cấp cho bất kỳ bên thứ ba nào khác, hay dùng vào bất kỳ mục đích nào khác.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Phí gửi bài\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Lệ phí gửi đăng bài: 1.000.000đ\u002Fbài báo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Lệ phí gửi đăng nhanh: 1.500.000đ\u002Fbài báo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Đối với tác giả là cán bộ viên chức thuộc Trường Đại học Y Dược Cần Thơ thì được hỗ trợ 50% lệ phí gửi đăng bài.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Đối với sinh viên thực hiện đề tài nghiên cứu khoa học cấp trường được hỗ trợ 100% lệ phí đăng bài ( Tác giả gửi đính kèm “ Quyết định về việc giao tổ chức thực hiện đề tài nghiên cứu khoa học cấp Trường của sinh viên”).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Hình thức nộp lệ phí:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Tiền mặt:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Nộp trực tiếp tại Phòng Tài chính - Kế toán, Trường Đại học Y Dược Cần Thơ, số 179 Nguyễn Văn Cừ, P. An Khánh, Q. Ninh Kiều, thành phố Cần Thơ.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Chuyển khoản:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tên Tài khoản: Trường ĐHYD Cần Thơ, Số TK: 0111000115668, tại ngân hàng Vietcombank chi nhánh Cần Thơ.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Thời gian: Áp dụng từ ngày 01\u002F02\u002F2023.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">* Phí gửi bài không được hoàn trả khi bài viết bị từ chối hoặc tác giả xin rút bài viết.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Quy trình phản biện bài báo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ thực hiện quy trình phản biện kín hai chiều nghiêm ngặt. Danh tính của những người phản biện không được tiết lộ cho các tác giả và ngược lại. Quy trình thẩm định bài báo đăng gồm các bước sau:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tiếp nhận bản thảo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tác giả liên hệ gửi bản thảo đến Tạp chí qua hệ thống trực tuyến tại website: https:\u002F\u002Ftapchi.ctump.edu.vn. Hướng dẫn về cách đăng ký, gửi bài và chuẩn bị bản thảo được cung cấp trên website của Tạp chí.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Sàng lọc sơ bộ\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Sau khi Tòa soạn nhận được bài báo của tác giả, Ban Thư ký sẽ tiến hành kiểm tra sơ bộ bài báo (các yêu cầu về nội dung và hình thức). Những bài báo không đúng quy cách hoặc có nội dung không phù hợp hoặc vi phạm bản quyền sẽ bị từ chối (Ban Thư ký thông báo phản hồi đến tác giả trong vòng 1 tuần). Những bài báo đủ điều kiện, được Ban Thư ký tòa soạn chuyển đến Ban Biên tập có cùng chuyên môn với nội dung bài báo để đề xuất người phản biện. Thời gian kể từ khi Ban Biên tập nhận bài báo đến khi đề xuất người phản biện bài báo chậm nhất là 5 ngày.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Vòng phản biện\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Ban Thư ký gửi bài và yêu cầu phản biện đến 02 phản biện độc lập.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Các phản biện gởi nhận xét cho Ban Thư ký. Thời gian từ khi gửi bài cho phản biện đến khi nhận ý kiến của phản biện tối đa là 20 ngày.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Xử ký kết quả phản biện\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Nếu ý kiến đồng ý cho đăng và không cần chỉnh sửa, Ban Thư ký tiếp tục đăng bài theo qui trình.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Nếu ý kiến đồng ý đăng và cần chỉnh sửa, Ban Thư ký sẽ thông tin đến tác giả chỉnh sửa theo yêu cầu của người phản biện. Thời gian chỉnh sửa và gửi lại kéo dài không quá 2 tuần, từ khi tác giả bài báo nhận được thông tin (Quá trình này có thể lặp lại tối đa 2 lần\u002F1 bài báo). Khi có sự thống nhất, đồng ý của người phản biện; bài báo được tiếp tục đăng theo qui trình.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">3. Những bài báo có chất lượng không đạt yêu cầu, cả 2 phản biện không đồng ý cho đăng sẽ bị Tòa soạn từ chối đăng.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Xuất bản\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Ban Thư ký tổng hợp các bản thảo đã được tác giả hoàn thiện sau thẩm định trình Ban Biên tập xem xét, Tổng Biên tập phê duyệt, quyết định bài đăng theo các tiêu chí: sự phù hợp nội dung với tôn chỉ và mục đích, thể loại bài viết (ưu tiên các bài có bài có nghiên cứu chuyên sâu, hàm lượng khoa học cao), đóng góp mới bài báo, bài báo được ưu tiên đăng trong số gần nhất của Tạp chí theo thứ tự: tính thời sự, chất lượng bài báo và thời gian gửi bài.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Ban Biên tập và Ban Thư ký biên tập bản thảo, chế bản, đọc rà soát lỗi. Thời gian hoàn thành từ 10-15 ngày.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">3. Ban Thư ký có trách nhiệm thông báo cho tác giả bài báo (bằng e-mail) về tình hình phê duyệt bài báo, thời gian, số kỳ, tập xuất bản bài báo theo qui định.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">4. Danh sách bài báo theo số Tạp chí được in ấn và phát hành trong năm định kỳ được công bố chính thức trên website: https:\u002F\u002Ftapchi.ctump.edu.vn\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>",{"VOID":578},"wcQ1uqwAAAAJ","2023-05-30T08:17:21.868+00:00",[],[582],{"id":583,"createTime":22,"updateTime":22,"relativeEntities":584,"slug":22,"properties":585,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":595,"parentIds":596,"statistic":22},"6413896b-eca9-442b-a73f-182a58a0ce40",[],{"title":586,"address":589,"country":592,"abbreviation":593},{"EN":587,"VI":588},"Can Tho University of Medicine and Pharmacy","Trường Đại học Y Dược Cần Thơ",{"EN":590,"VI":591},"No 179, Nguyen Van Cu street, An Khanh ward, Ninh Kieu district, Can Tho city, Vietnam","Số 179, đường Nguyễn Văn Cừ, phường An Khánh, quận Ninh Kiều, thành phố Cần Thơ, Việt Nam",{"VOID":109},{"VOID":594},"ctump","http:\u002F\u002Fwww.ctump.edu.vn\u002F",[],[],"https:\u002F\u002Ftapchi.ctump.edu.vn\u002Findex.php\u002Fctump",{"impactFactor":23,"impactFactorByYear":600,"i10Index":23,"i10IndexLast5Year":23,"totalPublication":602,"totalPublicationByYear":603,"totalCitation":608,"totalCitationByYear":609,"totalCitationPerPublication":197,"totalCitationPerPublicationByYear":611,"hindexLast5Year":135,"hindex":135},{"2022":601,"2023":200,"2024":195},0.01,1556,{"2020":137,"2021":604,"2022":605,"2023":606,"2024":607,"2025":211},57,306,801,358,161,{"2021":234,"2022":368,"2023":610},99,{"2021":612,"2022":406,"2023":193},0.23,{"impactFactor":22,"impactFactorByYear":22,"i10Index":91,"i10IndexLast5Year":91,"totalPublication":614,"totalPublicationByYear":615,"totalCitation":614,"totalCitationByYear":616,"totalCitationPerPublication":93,"totalCitationPerPublicationByYear":619,"hindexLast5Year":139,"hindex":139},476,{"0":293,"2019":91,"2021":227,"2022":547,"2023":539,"2024":445,"2025":139,"2026":138},{"2021":132,"2022":91,"2023":249,"2024":617,"2025":448,"2026":618},136,83,{"2021":194,"2022":601,"2023":620,"2024":215,"2025":621,"2026":622},0.62,25.43,13.83,{"id":624,"createTime":625,"updateTime":470,"relativeEntities":626,"slug":627,"properties":628,"entityType":20,"verifyStatus":119,"verifyTime":22,"verifyNote":22,"languages":640,"translateLanguages":22,"viewCount":221,"subjectFields":641,"manageAffiliations":642,"indexDatabases":643,"url":644,"thumbnailPath":645,"statistic":646,"gsStatistic":682,"type":96,"analyzePriority":22},"6984a56a-db70-403b-9cc4-4013e1ceaffa","2023-05-09T06:47:40.346+00:00",[],"T%E1%BA%A1p%20ch%C3%AD%20Nghi%C3%AAn%20c%E1%BB%A9u%20n%C6%B0%E1%BB%9Bc%20ngo%C3%A0i",{"country":629,"issn":630,"title":632,"introduce":635,"gsId":638},{"VOID":109},{"VOID":631},"25252445",{"EN":633,"VI":634},"VNU Journal of Foreign Studies","Tạp chí Nghiên cứu nước ngoài",{"EN":636,"VI":637},"{\"ops\":[{\"insert\":\"\\n\\nThe \\n\"},{\"attributes\":{\"italic\":true},\"insert\":\"VNU Journal of Science\"},{\"insert\":\"\\n was established in 1985 for the publication of national and international research papers in all fields of natural sciences and technology, social sciences and humanities. Since then, the journal has grown in quality, size and scope and now comprises a dozen of serials spanning academic research. 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Although, the main text structure may vary based on the review subtopics, the articles should be formatted according to suitable Templates as research articles.\"},{\"attributes\":{\"align\":\"justify\"},\"insert\":\"\\n\"},{\"insert\":\"\\n\"}]}","{\"ops\":[{\"insert\":\"Tạp chí Khoa học Trường ĐHSP Hà Nội 2 nhằm mục đích cung cấp một nền tảng liên ngành của sự phổ biến những tiến bộ của khoa học và công nghệ. Tạp chí xuất bản các bài báo gốc có giá trị khoa học hoặc công nghệ trong tất cả các lĩnh vực khoa học tự nhiên, xã hội hoặc giáo dục.\\n\"},{\"attributes\":{\"bold\":true},\"insert\":\"Chuyên san Khoa học tự nhiên và công nghệ:\"},{\"insert\":\" Là các bài báo mô tả những phát hiện có giá trị trong vật lý, toán học, hóa học, sinh học; giải quyết các vấn đề kỹ thuật hoặc công nghệ.\"},{\"attributes\":{\"list\":\"bullet\"},\"insert\":\"\\n\"},{\"attributes\":{\"bold\":true},\"insert\":\"Chuyên san Khoa học Xã hội và Nhân văn:\"},{\"insert\":\" là các bài báo xuất bản chất lượng cao trong các lĩnh vực khác nhau của khoa học xã hội và nghiên cứu phát triển con người.\"},{\"attributes\":{\"list\":\"bullet\"},\"insert\":\"\\n\"},{\"attributes\":{\"bold\":true},\"insert\":\"Chuyên san Khoa học giáo dục:\"},{\"insert\":\" là các bài báo xuất bản trong lĩnh vực khoa học giáo dục và các ứng dụng của tiến bộ vào giáo dục để cải thiện và nâng cao giáo dục khoa học ở tất cả các cấp.\"},{\"attributes\":{\"list\":\"bullet\"},\"insert\":\"\\n\"},{\"insert\":\"Tạp chí trường ĐHSP Hà Nội 2 xuất bản được phản biện kín, xét duyệt bởi ít nhất 02 chuyên gia, và được đánh giá, chọn lựa từ ban biên tập và Tổng biên tập.\\n\"},{\"attributes\":{\"bold\":true},\"insert\":\"Các loại bài báo\"},{\"insert\":\":\\nBài báo nghiên cứu:\"},{\"attributes\":{\"list\":\"ordered\"},\"insert\":\"\\n\"},{\"insert\":\"Báo cáo học thuật về nghiên cứu ban đầu chưa từng được xuất bản ở bất kỳ nơi nào, hay bằng bất kỳ ngôn ngữ nào khác. Bản thảo thích hợp, nên chứa các phần sau theo thứ tự: Tiêu đề, Tác giả, Liên kết tác giả, Địa chỉ email của tác giả tương ứng, Tóm tắt, Từ khóa, Danh pháp (nếu có), Giới thiệu, Thử nghiệm, Lý thuyết, Kết quả và thảo luận, Kết luận, Xung đột quan tâm, Lời cảm ơn (nếu có), Tài liệu tham khảo, Phụ lục (nếu có). Bản xuất bản trước phải được định dạng theo Mẫu (phiên bản MS-Word).\\n2. Bài báo tổng quan:\\nNgoài các bài phê bình được mời, các bài phê bình tài liệu, bài phê bình có hệ thống và bài phê bình sẽ được chấp nhận để xem xét. Bản thảo cần được soạn thảo và sắp xếp theo trình tự yêu cầu: Tên sách, Tên tác giả, Liên kết, Địa chỉ email, Tóm tắt, Từ khóa, Nội dung chính, Kết luận, Xung đột lợi ích, Lời cảm ơn (nếu có), Tài liệu tham khảo. Mặc dù, cấu trúc văn bản chính có thể thay đổi dựa trên các chủ đề phụ của bài đánh giá, các bài báo nên được định dạng theo các Mẫu phù hợp như các bài báo nghiên cứu.\\n\"}]}",{"VOID":814},"YPoBvsIAAAAJ",[],[],[],"https:\u002F\u002Fsj.hpu2.edu.vn\u002Findex.php\u002Fjournal","\u002Fapi\u002Fpublic\u002Ffile\u002Fpublisher\u002F954132b5-ca74-461c-b819-45ad6e49a404\u002F2790ef1d0a7d7a40a504c2fc1647f670.jpg",{"impactFactor":23,"impactFactorByYear":821,"i10Index":23,"i10IndexLast5Year":23,"totalPublication":417,"totalPublicationByYear":823,"totalCitation":222,"totalCitationByYear":824,"totalCitationPerPublication":612,"totalCitationPerPublicationByYear":825,"hindexLast5Year":91,"hindex":91},{"2024":822},0.17,{"2022":224,"2023":366,"2024":230},{"2022":445,"2023":214,"2024":91},{"2022":257,"2023":312,"2024":253},{"impactFactor":22,"impactFactorByYear":22,"i10Index":135,"i10IndexLast5Year":135,"totalPublication":418,"totalPublicationByYear":827,"totalCitation":242,"totalCitationByYear":828,"totalCitationPerPublication":829,"totalCitationPerPublicationByYear":830,"hindexLast5Year":136,"hindex":136},{"0":91,"2022":222,"2023":224,"2024":158,"2025":233},{"2023":136,"2024":224,"2025":289,"2026":366},1.22,{"2023":202,"2024":428,"2025":831},4.56,{"id":833,"createTime":834,"updateTime":835,"relativeEntities":836,"slug":837,"properties":838,"entityType":20,"verifyStatus":119,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":158,"subjectFields":850,"manageAffiliations":851,"indexDatabases":859,"url":899,"thumbnailPath":22,"statistic":900,"gsStatistic":932,"type":96,"analyzePriority":22},"21ccdb34-414d-420f-8a60-a592a2fa848e","2023-05-29T10:42:53.358+00:00","2026-08-27T01:57:29.560+00:00",[],"Vietnam-Journal-of-Earth-Sciences",{"country":839,"eissn":840,"issn":842,"title":844,"introduce":846,"gsId":848},{"VOID":109},{"VOID":841},"26159783",{"VOID":843},"08667187",{"EN":845},"Vietnam Journal of Earth Sciences",{"EN":847},"Science of the Earth, formerly Vietnam Journal of Earth Sciences, is a peer-reviewed journal to publish high-quality articles on the entire range of earth sciences and the environment, focused on the Asia Pacific region and their correlations and connections to the globe. The journal publishes fundamental and applied research in earth sciences and the environment, including geology, geophysics, geography, soil science, hydrology, meteorology, oceanography, petroleum, geohazards, environmental sciences, environmental engineering, sustainable development, geoinformatics, geodesy, GIS, and remote sensing.",{"VOID":849},"5htfr3YAAAAJ",[],[852],{"id":162,"createTime":22,"updateTime":22,"relativeEntities":853,"slug":22,"properties":854,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":171,"parentIds":858,"statistic":22},[],{"title":855,"country":856,"abbreviation":857},{"EN":166,"VI":167},{"VOID":109},{"VOID":170},[],[860,872,883],{"id":861,"indexDatabase":862,"url":867,"indexYears":868,"academicFieldIds":869,"indexDatabaseRanking":871},"6ace2085-a177-4a27-b309-8813b832111e",{"id":74,"createTime":22,"updateTime":22,"relativeEntities":863,"label":864,"description":865,"key":80,"publicationTags":866,"standard":22},[],{"EN":77,"VI":77},{"EN":77,"VI":79},[82],"https:\u002F\u002Fwww.scopus.com\u002Fsourceid\u002F21101039869","2018-2024",[870],"1689391c-5702-4349-aaa7-d720ee4321fc","NONE",{"id":873,"indexDatabase":874,"url":879,"indexYears":880,"academicFieldIds":881,"indexDatabaseRanking":22},"dadb15a8-ee22-41c2-a287-49e969d9a998",{"id":177,"createTime":22,"updateTime":22,"relativeEntities":875,"label":876,"description":877,"key":183,"publicationTags":878,"standard":22},[],{"EN":180,"VI":180},{"EN":182,"VI":182},[185],"https:\u002F\u002Fasean-cites.org\u002Fjournal_info?jid=10629","2016-2022",[882],"e04f14cf-280b-4aa8-b711-b77ddd79cbaf",{"id":884,"indexDatabase":885,"url":896,"indexYears":22,"academicFieldIds":897,"indexDatabaseRanking":22},"06f278ee-37b9-41eb-a9b0-3d2d77fa502b",{"id":886,"createTime":22,"updateTime":22,"relativeEntities":887,"label":888,"description":890,"key":893,"publicationTags":894,"standard":22},"88bab0f7-443b-476c-a72a-7fa5222da393",[],{"EN":889,"VI":889},"ISI\u002FESCI  - 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Gravity data (from 381 ground gravity stations) were collected, processed, and analyzed together with the available aeromagnetic (800 line-km) data to investigate the hydrogeologic and structural settings, areal distribution, geometry, and water storage of the aquifers in El Qaa coastal plain in the southwest Sinai Peninsula, and to assess their longevity given projected extraction rates. Findings include (1) complete Bouguer anomaly and total magnetic intensity maps show two connected sub-basins separated by a narrow saddle with an average basin length of 43 km and an average width of 12 km; (2) two-dimensional modeling of both gravity and magnetic data indicates basin fill with a maximum thickness of 3.5 km; (3) using anomalous residual gravity, the volume of water in storage was estimated at 40–56 km3; and (4) progressive increases in extraction rates over time will deplete up to 40 % of the aquifers’ volume in 200–230 years and will cause the water quality to deteriorate due to seawater intrusion in 45 years. Similar geophysical exploration campaigns, if conducted over the entire coastal plains of the Red Sea and the Gulfs of Suez and Aqaba, could assist in the development of sound and sustainable management schemes for the freshwater resources in these areas. The adopted techniques could pave the way toward the establishment of sustainable utilization schemes for a much larger suite of similar aquifers worldwide.",{"EN":959},"Geophysical Constraints on the Hydrogeologic and Structural Settings of the Gulf of Suez Rift-Related Basins: Case Study from the El Qaa Plain, Sinai, Egypt",{"VOID":961},"Allam A, Khalil H (1989) Geology and stratigraphy of Gebel Qabeliat area, Southwestern Sinai, Egypt. J Afr Earth Sci 9:59–67\nAlsharhan AS (2003) Petroleum geology and potential hydrocarbon plays in the Gulf of Suez rift basin, Egypt. AAPG Bull 87:143–180\nAttia MA (1930) Report on fresh water of El-Tor Quarry. Geological Survey of Egypt, Cairo\nBosworth W (1985) Geometry of propagating continental rifts. Nature 316:625–627\nBosworth W, Crevello P, Winn RD, Steinmetz J (1998) Structure, sedimentation, and basin dynamics during rifting of the Gulf of Suez and north-western Red Sea. 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Geol Surv Israel Bull 71:1–44\nGhorab MA (1961) Abnormal stratigraphic features in Ras Gharib oil field. Third Arab Petroleum Congress. Alexandria\nGilboa Y (1972) Survey of water resources at A-Tor. Tahal, Water Planning for Israel Ltd., Tel Aviv\nGorski J, Ghodeif K (2000) Salinization of shallow water aquifer in El-Qaa coastal plain, Sinai, Egypt. In: Sadurski A (ed) The 16th salt water intrusion meeting (SWIM), Międzyzdroje–Wolin Island. Nicholas Copernicus University, Poland, pp 63–72\nIsmail AM (1998) Geophysical studies in Northern Part of Egypt. Cairo University, Cairo\nKlitzsch E, List FK, Pohlmann G (1987) Geological map of Egypt, South Sinai sheet, Scale 1:500,000. Cario, Egypt, The Egyptian General Petroleum Corporation\u002FConoco; Berlin Institut für Angewandte Geodasie\nLambiase JJ, Bosworth W (1995) Structural controls on sedimentation in continental rifts. In: Lambiase JJ (ed) Hydrocarbon habitat in rift basins. Geological Society Special Publication 80, pp 117–144\nLandon SM (1994) Interior rift basins. In: Landon SM (ed) Interior rift basins. A.APG Memoir 59, pp 1–4\nMacLeod IN, Jones K, Dai TF (1993) 3D analytic signal in the interpretation of total magnetic field data at low magnetic latitudes. Explor Geophys 24:679–688\nMcClay KR, Nichols GJ, Khalil SM, Darwish M, Bosworth W (1998) Extensional tectonics and sedimentation, eastern Gulf of Suez, Egypt. In: Purser B, Bosence DW (eds) Sedimentation and tectonics of the Gulf of Aden-Red Sea rift system. Chapman and Hall, London, pp 223–228\nMcGuire VL, Johnson MR, Schieffer RL, Stanton JS, Sebree SK, Verstraeten IM (2000) Water in storage and approaches to ground-water management, high plains Aquifer, vol 1243. US Geologic Survey Circular Reston, Virginia\nMorley CK, Nelson RA, Patton TL, Munn SG (1990) Transfer zones in the East African rift system and their relevance to hydrocarbon exploration in rifts. AAPG Bull 74:1234–1253\nMoustafa AR (1993) Organic geochemistry of source rocks and related crude oils in the Gulf of Suez, Egypt, vol 147. Berlin Geowissenschaften Abbandlungen. Selbstverlag Fachbereich Geowissenschaften, Berlin\nMoustafa AR (1997) Controls on the development and evolution of transfer zones: the influence of basement structure and sedimentary thickness in the Suez rift and Red Sea. J Struct Geol 19:755–768\nMoustafa AR (2002) Controls on the geometry of transfer zones in the Suez rift and northwest Red Sea: implications for the structural geometry of rift systems. AAPG Bull 86:979–1002\nMoustafa AR (2004) Geologic maps of the Eastern Side of the Suez Rift (Western Sinai Peninsula), Egypt. AAPG\u002FDatapages, CD-ROm, Tulsa\nNabighian MN (1972) The analytic signal of two-dimensional magnetic bodies with polygonal cross-section: its properties and use for automated anomaly interpretation. Geophysics 37:507–517\nOmran M (1982) Combined gravity and seismic study on the Nile Delta Region. Mansoura University, Mansoura\nPatton TL, Moustafa AR, Nelson RA, Abdine SA (1994) Tectonic evolution and structural setting of the Suez rift. In: Landon SM (ed) Interior rift basins. AAPG Memoir 59, pp 9–56\nPivnik DA, Ramzy M, Steer BL, Thorseth J, El Sisi Z, Gaafar I, Garing JD, Tucker RS (2003) Episodic growth of normal faults as recorded by syntectonic sediments, July oil field, Suez rift, Egypt. AAPG Bull 87:1015–1030\nRabeh T, Miranda JM (2008) A tectonic model of the Sinai Peninsula based on magnetic data. J Geophys Eng 5:69–479\nRabeh T, Miranda JM, Carvalho J, Bocin A (2009) Interpretation case study of the Sahl El Qaa area, southern Sinai Peninsula, Egypt. Geophys Prospect 57:447–459\nRamsey AS (1949) An introduction to the theory of Newtonian attraction. The University Press, Cambridge\nRoest WR, Verhoef J, Pilkington M (1992) Magnetic interpretation using the 3-D analytic signal. Geophysics 57:116–125\nRosendahl BR, Reynolds DJ, Lorber PM, Burgess CF, McGill J, Scott D, Lambiase JJ, Derksen SJ (1986) Structural expression of rifting: lessons from Lake Tanganyika, Africa. In: Frostick LE, Renaut RW, Reid I, Tiercelin JJ (eds) Sedimentation in the African rifts. Geological Society Special Publication 25, pp 29–43\nSaibi H, Nishijima J, Ehara S, Aboud E (2006) Integrated gradient interpretation techniques for 2D and 3D gravity data interpretation. Earth Planets Space 58:815–821\nSaid R (1962) The geology of Egypt. Elsevier, New York\nSaid R (1990) Cenozoic. In: Said R (ed) The geology of Egypt. A. A. Balkema, Rotterdam, pp 451–486\nSchutz KI (1994) Structure and stratigraphy of the Gulf of Suez, Egypt. In: Landon SM (ed) Interior rift basins. AAPG Memoir 59, pp 57–96\nSelim EI (2002) The use of the geophysical methods to study the subsurface structure in the Southeastern Mediterranean and North Sinai region. Mansoura University, Mansoura\nSetto I (1991) A crustal modeling for the Nile Delta, Egypt. J Geol 34:279–292\nSharp IR, Gawthorpe RL, Underhill JR, Gupta S (2000) Fault-propagation folding in extensional settings: examples of structural style and synrift sedimentary response from the Suez rift, Sinai, Egypt. GSA Bull 112:1877–1899\nSturchio NC, Arehart GB, Sultan M, Sano Y, AboKamar Y, Sayed M (1996) Composition and origin of thermal waters in the Gulf of Suez area, Egypt. Appl Geochem 11:471–479\nSturchio NC, Du X, Purtschert R, Lehmann BE, Sultan M, Patterson LJ, Lu ZT, Muller P, Bigler T, Bailey K, O’Connor TP, Young L, Lorenzo R, Becker R, El Alfy Z, El Kaliouby B, Dawood Y, Abdallah AMA (2004) One million year old groundwater in the Sahara revealed by krypton-81 and chlorine-36. Geophys Res Lett 31:L05503\nSultan M, Yan E, Sturchio N, Wagdy A, Milewski A, Abdel Gelil K, Manocha N, Becker R (2007) Natural discharge: a key to sustainable utilization of fossil groundwater: Amsterdam. J Hydrol 335:25–36\nSultan SA, Mohameden MI, Santos FM (2009) Hydrogeophysical study of the El Qaa Plain, Sinai, Egypt. Bull Eng Geol Environ 68:525–537\nSultan M, Metwally S, Milewski A, Becker D, Ahmed M, Sauck W, Soliman F, Sturchio N, Yan E, Rashed M, Wagdy A, Becker R, Welton B (2011) Modern recharge to the Nubian Aquifer, Sinai Peninsula: geochemical, geophysical, and modeling constraints. J Hydrol 403:14–24\nTelford WM, Geldart LP, Sheriff RE (1990) Applied geophysics. Cambridge University Press, Cambridge\nVersfelt J, Rosendahl BR (1989) Relationship between prerift structure and rift architecture in Lakes Tanganyika and Malawi, East Africa. Nature 337:257–354",{"VOID":963},"10.1007\u002Fs10712-013-9259-6","PUBLICATION","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs10712-013-9259-6",[967,992,1005,1018,1036,1049],{"id":968,"sortIndex":23,"researcher":22,"roles":969,"affiliations":971,"properties":989,"displayName":991,"givenName":22,"familyName":22},"c5fb046c-8907-4fe0-a596-882374986845",[970],"AUTHOR",[972,980],{"id":973,"sortIndex":23,"affiliation":974,"properties":22},"66a99271-5002-4e45-bfc8-7360d3dfd523",{"id":973,"createTime":22,"updateTime":22,"relativeEntities":975,"slug":22,"properties":976,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":979,"statistic":22},[],{"title":977},{"VI":978},"Geosciences Department, Western Michigan University, Kalamazoo, 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King Abdulaziz University, Jeddah, Saudi Arabia",[],{},{"title":1069},{"VI":1070},"Mohamed Rashed","ARTICLE",{"url":965,"publisher":1073,"properties":1119},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":1074,"slug":10,"properties":1075,"entityType":20,"verifyStatus":21,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":23,"subjectFields":1079,"manageAffiliations":1088,"indexDatabases":1099,"url":22,"thumbnailPath":22,"statistic":1114,"gsStatistic":22,"type":96,"analyzePriority":22},[],{"issn":1076,"title":1077,"eissn":1078},{"VOID":15},{"EN":17},{"VOID":13},[1080,1084],{"id":26,"createTime":22,"updateTime":22,"relativeEntities":1081,"label":1082,"description":1083,"parentId":22,"standard":22,"scholarHubFieldId":22},[],{"EN":29},{},{"id":32,"createTime":22,"updateTime":22,"relativeEntities":1085,"label":1086,"description":1087,"parentId":22,"standard":22,"scholarHubFieldId":22},[],{"EN":35},{},[1089,1094],{"id":39,"createTime":22,"updateTime":22,"relativeEntities":1090,"slug":22,"properties":1091,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1093,"statistic":22},[],{"title":1092},{"EN":43},[],{"id":46,"createTime":22,"updateTime":22,"relativeEntities":1095,"slug":22,"properties":1096,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1098,"statistic":22},[],{"title":1097},{"EN":50},[52],[1100,1107],{"id":55,"indexDatabase":1101,"url":68,"indexYears":22,"academicFieldIds":1106,"indexDatabaseRanking":22},{"id":57,"createTime":22,"updateTime":22,"relativeEntities":1102,"label":1103,"description":1104,"key":64,"publicationTags":1105,"standard":22},[],{"EN":60,"VI":60},{"EN":62,"VI":63},[66,67],[70],{"id":72,"indexDatabase":1108,"url":83,"indexYears":84,"academicFieldIds":1113,"indexDatabaseRanking":88},{"id":74,"createTime":22,"updateTime":22,"relativeEntities":1109,"label":1110,"description":1111,"key":80,"publicationTags":1112,"standard":22},[],{"EN":77,"VI":77},{"EN":77,"VI":79},[82],[86,87],{"impactFactor":23,"impactFactorByYear":1115,"i10Index":23,"i10IndexLast5Year":23,"totalPublication":91,"totalPublicationByYear":1116,"totalCitation":23,"totalCitationByYear":1117,"totalCitationPerPublication":23,"totalCitationPerPublicationByYear":1118,"hindexLast5Year":23,"hindex":23},{},{"1976":93,"1980":93},{},{},{"pages":1120,"volume":1122},{"VOID":1121},"415-430",{"VOID":1123},"35","2013-11-09",2013,[66,88],false,{"id":1129,"createTime":1130,"updateTime":1131,"relativeEntities":1132,"slug":1133,"properties":1134,"entityType":964,"verifyStatus":119,"verifyTime":1131,"verifyNote":1143,"languages":22,"translateLanguages":22,"viewCount":23,"primaryUrl":1144,"fullTextUrl":22,"authors":1145,"publicationType":1071,"publisherRelationship":1288,"citationCount":22,"citationInfo":22,"publishDate":1340,"publishYear":1341,"citationAnalyzeStatus":21,"lastCitationAnalyze":22,"indexDatabases":1342,"openAccess":22,"references":22,"isForceReanalyzing":1127},"008e6204-b04f-4d4a-9aed-eba9d823684e","2024-01-10T19:37:51.660+00:00","2025-01-14T01:08:38.468+00:00",[],"Soil-Moisture-and-Sea-Surface-Salinity-Derived-from-Satellite-Borne-Sensors",{"abstract":1135,"title":1137,"references":1139,"doi":1141},{"EN":1136},"The monitoring of soil moisture and sea surface salinity over the Earth has been profoundly enhanced during the last thirteen years due to a new generation of satellite sensors. L-band radiometry is currently the only technology providing direct measurements of soil moisture, insensitive to surface roughness and distribution of elements in the soil, and the only technology the only technology for measuring that allows us to measure sea surface salinity from space. The Soil Moisture and Ocean Salinity (SMOS) and Soil Moisture Active Passive (SMAP) satellite missions resolve global and local variability with a spatial resolution of approximately 43 km, a swath width close to 1000 km, and a sampling time, for each mission, of at least twice every 3 days. These resolutions and samplings can be increased by either merging data from the two sensors, and with complementary information gathered from other passive or active sensors, or with in situ information at higher spatial resolution. Numerous scientific studies based on the use of this new type of measurement have led to a better understanding and constraint of the processes governing the variability of the water cycle, ocean circulation and the Earth's climate. The continuity of measurements, and the increased spatial and radiometric resolution is critical for fulfilling scientific needs. Future L-band radiometry missions currently being planned in Europe (the Copernicus Imaging Microwave Radiometer), and in China (the Ocean Salinity mission) should provide better constraints on auxiliary parameters by combining multiple frequencies, but they will not have improved spatial resolution beyond SMOS and SMAP. The temporal continuity with SMOS and SMAP will likely not be ensured. In parallel, new concepts are being developed to increase spatial resolution of both land and ocean parameters.",{"EN":1138},"Soil Moisture and Sea Surface Salinity Derived from Satellite-Borne Sensors",{"VOID":1140},"Akbar R, Short Gianotti D, McColl KA, Haghighi E, Salvucci GD, Entekhabi D (2018) Hydrological storage length scales represented by remote sensing estimates of soil moisture and precipitation. Water Resour Res 54(3):1476–1492. https:\u002F\u002Fdoi.org\u002F10.1002\u002F2017WR021508\nAkhil VP, Vialard J, Lengaigne M, Keerthi MG, Boutin J, Vergely JL, Papa F (2020) Bay of Bengal Sea surface salinity variability using a decade of improved SMOS re-processing. Remote Sens Environ 248:111964. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.rse.2020.111964\nAl-Khaldi MM, Johnson JT, O’Brien AJ, Balenzano A, Mattia F (2019) Time-series retrieval of soil moisture using CYGNSS. 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Proc Natl Acad Sci 109(36):14343–14347. https:\u002F\u002Fdoi.org\u002F10.1073\u002Fpnas.1201364109\nBalaguru K, Foltz GR, Leung LR, Asaro ED, Emanuel KA, Liu H, Zedler SE (2015) Dynamic Potential Intensity: an improved representation of the ocean’s impact on tropical cyclones. Geophys Res Lett 42(16):6739–6746. https:\u002F\u002Fdoi.org\u002F10.1002\u002F2015GL064822\nBalaguru K, Foltz GR, Leung LR, Kaplan J, Xu W, Reul N, Chapron B (2020) Pronounced impact of salinity on rapidly intensifying tropical cyclones. Bull Am Meteorol Soc 101(9):E1497–E1511. https:\u002F\u002Fdoi.org\u002F10.1175\u002FBAMS-D-19-0303.1\nBauer-Marschallinger B, Freeman V, Cao S, Paulik C, Schaufler S, Stachl T, Modanesi S, Massari C, Ciabatta L, Brocca L (2018) Toward global soil moisture monitoring with Sentinel-1: harnessing assets and overcoming obstacles. 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IEEE Trans Geosci Remote Sens 50(5):1662–1675. https:\u002F\u002Fdoi.org\u002F10.1109\u002FTGRS.2012.2184546\nBoutin J, Chao Y, Asher WE, Delcroix T, Drucker R, Drushka K, Kolodziejczyk N, Lee T, Reul N, Reverdin G, Schanze J, Soloviev A, Yu L, Anderson J, Brucker L, Dinnat E, Santos-Garcia A, Jones WL, Maes C, Meissner T, Tang W, Vinogradova N, Ward B (2016) Satellite and in situ salinity: understanding near-surface stratification and subfootprint variability. Bull Am Meteorol Soc 97(8):1391–1407. https:\u002F\u002Fdoi.org\u002F10.1175\u002Fbams-d-15-00032.1\nBoutin J, Vergely JL, Marchand S, D’Amico F, Hasson A, Kolodziejczyk N, Reul N, Reverdin G, Vialard J (2018) New SMOS Sea Surface Salinity with reduced systematic errors and improved variability. Remote Sens Environ 214:115–134. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.rse.2018.05.022\nBoutin J, Reul N, Koehler J, Martin A, Catany R, Guimbard S, Rouffi F, Vergely JL, Arias M, Chakroun M, Corato G, Estella-Perez V, Hasson A, Josey S, Khvorostyanov D, Kolodziejczyk N, Mignot J, Olivier L, Reverdin G, Stammer D, Supply A, Thouvenin-Masson C, Turiel A, Vialard J, Cipollini P, Donlon C, Sabia R, Mecklenburg S (2021a) Satellite-based sea surface salinity designed for ocean and climate studies. J Geophys Res Oceans 126(11):e2021JC017676. https:\u002F\u002Fdoi.org\u002F10.1029\u002F2021JC017676\nBoutin J, Vergely J-L, Dinnat EP, Waldteufel P, D’Amico F, Reul N, Supply A, Thouvenin-Masson C (2021b) Correcting sea surface temperature spurious effects in salinity retrieved from spaceborne L-band radiometer measurements. IEEE Trans Geosci Remote Sens 59(9):7256–7269. https:\u002F\u002Fdoi.org\u002F10.1109\u002Ftgrs.2020.3030488\nBrandt M, Wigneron JP, Chave J, Tagesson T, Penuelas J, Ciais P, Rasmussen K, Tian F, Mbow C, Al-Yaari A, Rodriguez-Fernandez N, Schurgers G, Zhang WM, Chang JF, Kerr Y, Verger A, Tucker C, Mialon A, Rasmussen LV, Fan L, Fensholt R (2018a) Satellite passive microwaves reveal recent climate-induced carbon losses in African drylands. Nat Ecol Evol 2(5):827–835. https:\u002F\u002Fdoi.org\u002F10.1038\u002Fs41559-018-0530-6\nBrandt M, Yue YM, Wigneron JP, Tong XW, Tian F, Jepsen MR, Xiao XM, Verger A, Mialon A, Al-Yaari A, Wang KL, Fensholt R (2018b) Satellite-observed major greening and biomass increase in South China Karst during recent decade. Earths Future 6(7):1017–1028. https:\u002F\u002Fdoi.org\u002F10.1029\u002F2018ef000890\nC. 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J Clim 14(7):1479–1498. https:\u002F\u002Fdoi.org\u002F10.1175\u002F1520-0442(2001)014%3c1479:OOCBSW%3e2.0.CO;2\nChew C, Small E (2018) Soil moisture sensing using spaceborne GNSS reflections: comparison of CYGNSS reflectivity to SMAP soil moisture. Geophys Res Lett 45(9):4049–4057. https:\u002F\u002Fdoi.org\u002F10.1029\u002F2018GL077905\nChoudhury BJ, Schmugge TJ, Chang A, Newton RW (1979) Effect of surface roughness on the microwave emission from soils. J Geophys Res Oceans 84(C9):5699–5706. https:\u002F\u002Fdoi.org\u002F10.1029\u002FJC084iC09p05699\nClarizia MP, Pierdicca N, Costantini F, Floury N (2019) Analysis of CYGNSS data for soil moisture retrieval. IEEE J Sel Top Appl Earth Observ Remote Sens 12(7):2227–2235. https:\u002F\u002Fdoi.org\u002F10.1109\u002FJSTARS.2019.2895510\nColliander A, Ruokokoski L, Suomela J, Veijola K, Kettunen J, Kangas V, Aalto A, Levander M, Greus H, Hallikainen MT, Lahtinen J (2007) Development and calibration of SMOS reference radiometer. IEEE Trans Geosci Remote Sens 45(7):1967–1977. https:\u002F\u002Fdoi.org\u002F10.1109\u002FTGRS.2007.894055\nColliander A, Reichle R, Crow W, Cosh M, Chen F, Chan S, Das N, Bindlish R, Chaubell J, Kim S, Liu Q, O’Neill P, Dunbar S, Dang L, Kimball J, Jackson T, AlJassar H, Asanuma J, Bhattacharya B, Berg A, Bosch D, Bourgeau-Chavez L, Caldwell T, Calvet J-C, Collins CH, Jensen K, Livingston S, López-Baeza E, Martínez-Fernández J, McNairn H, Moghaddam M, Montzka C, Notarnicola C, Pellarin T, Pfeil I, Pulliainen J, Ramos J, Seyfrie M, Starks P, Su Z, Thibeault M, van der Velde R, Vreugdenhil M, Walker J, Zeng Y, Zribi M, Entekhabi D, Yueh S (2021) Validation of soil moisture data products from the NASA SMAP mission. IEEE J Sel Top Appl Earth Observ Remote Sens 15:364–392. https:\u002F\u002Fdoi.org\u002F10.1109\u002FJSTARS.2021.3124743\nCrow WT, Gomez CA, Sabater JM, Holmes T, Hain CR, Lei FN, Dong JZ, Alfieri JG, Anderson MC (2020) Soil moisture-evapotranspiration overcoupling and L-band brightness temperature assimilation: sources and forecast implications. J Hydrometeorol 21(10):2359–2374. https:\u002F\u002Fdoi.org\u002F10.1175\u002Fjhm-d-20-0088.1\nD'Addezio JM, Bingham FM, Jacobs GA. (2019) Sea surface salinity subfootprint variability estimates from regional high-resolution model simulations. Remote Sens Environ. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.rse.2019.111365\nDaganzo-Eusebio E, Oliva R, Kerr YH, Nieto S, Richaume P, Mecklenburg SM (2013) SMOS Radiometer in the 1400–1427-MHz passive band: impact of the RFI environment and approach to its mitigation and cancellation. 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Front Mar Sci 6:243. https:\u002F\u002Fdoi.org\u002F10.3389\u002Ffmars.2019.00243\nWagner W, Lindorfer R, Melzer T, Hahn S, Bauer-Marschallinger B, Morrison K, Calvet J-C, Hobbs S, Quast R, Greimeister-Pfeil I, Vreugdenhil M (2022) (2022) Widespread occurrence of anomalous C-band backscatter signals in arid environments caused by subsurface scattering. Remote Sens Environ 276:113025. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.rse.2022.113025\nWaldteufel P, Vergely J, Cot C (2004) A modified cardioid model for processing multiangular radiometric observations. IEEE Trans Geosci Remote Sens 42(5):1059–1063. https:\u002F\u002Fdoi.org\u002F10.1109\u002FTGRS.2003.821698\nWang H, Magagi R, Goita K, Jagdhuber T (2019) Refining a polarimetric decomposition of multi-angular UAVSAR time series for soil moisture retrieval over low and high vegetated agricultural fields. IEEE J Sel Top Appl Earth Observ Remote Sens 12(5):1431–1450. https:\u002F\u002Fdoi.org\u002F10.1109\u002FJSTARS.2019.2909984\nWigneron J-P, Chanzy A, Calvet J-C, Bruguier N (1995) A simple algorithm to retrieve soil moisture and vegetation biomass using passive microwave measurements over crop fields. Remote Sens Environ 51(3):331–341. https:\u002F\u002Fdoi.org\u002F10.1016\u002F0034-4257(94)00081-W\nWigneron JP, Waldteufel P, Chanzy A, Calvet JC, Kerr Y (2000) Two-dimensional microwave interferometer retrieval capabilities over land surfaces (SMOS mission). Remote Sens Environ 73(3):270–282. https:\u002F\u002Fdoi.org\u002F10.1016\u002FS0034-4257(00)00103-6\nWigneron JP, Jackson TJ, O’Neill P, De Lannoy G, de Rosnay P, Walker JP, Ferrazzoli P, Mironov V, Bircher S, Grant JP, Kurum M, Schwank M, Munoz-Sabater J, Das N, Royer A, Al-Yaari A, Al Bitar A, Fernandez-Moran R, Lawrence H, Mialon A, Parrens M, Richaume P, Delwart S, Kerr Y (2017) Modelling the passive microwave signature from land surfaces: A review of recent results and application to the L-band SMOS & SMAP soil moisture retrieval algorithms. Remote Sens Environ 192(April 2017):238–262. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.rse.2017.01.024\nWu H, Kimball JS, Zhou N, Alfieri L, Luo L, Du J, Huang Z (2019) (2019) Evaluation of real-time global flood modeling with satellite surface inundation observations from SMAP. 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IEEE Geosci Remote Sens Lett 17(2):207–211. https:\u002F\u002Fdoi.org\u002F10.1109\u002FLGRS.2019.2918764\nYueh SH, Shah R, Chaubell MJ, Hayashi A, Xu X, Colliander A (2020b) A semiempirical modeling of soil moisture, vegetation, and surface roughness impact on CYGNSS reflectometry data. IEEE Trans Geosci Remote Sens 60:1–17. https:\u002F\u002Fdoi.org\u002F10.1109\u002FTGRS.2020.3035989\nYueh SH, Shah R, Xu X, Stiles B, Bosch-Lluis X (2021) A satellite synthetic aperture radar concept using P-band signals of opportunity. IEEE J Sel Top Appl Earth Observ Remote Sens 14:2796–2816. https:\u002F\u002Fdoi.org\u002F10.1109\u002FJSTARS.2021.3059242\nZavorotny VU, Larson KM, Braun JJ, Small EE, Gutmann ED, Bilich AL (2010) A physical model for GPS multipath caused by land reflections: toward bare soil moisture retrievals. IEEE J Sel Top Appl Earth Observ Remote Sens 3(1):100–110. https:\u002F\u002Fdoi.org\u002F10.1109\u002FJSTARS.2009.2033608\nZhu JS, Huang BH, Zhang RH, Hu ZZ, Kumar A, Balmaseda MA, Marx L, Kinter JL (2014) Salinity anomaly as a trigger for ENSO events. Sci Rep 4:6821. https:\u002F\u002Fdoi.org\u002F10.1038\u002Fsrep06821\nZhu J, Kumar A, Wang W (2020) Intraseasonal surface salinity variability and the MJO in a climate model. Geophys Res Lett 47(17):997. https:\u002F\u002Fdoi.org\u002F10.1029\u002F2020GL088997\nZribi M, Dechambre M (2003) A new empirical model to retrieve soil moisture and roughness from C-band radar data. Remote Sens Environ 84(1):42–52. https:\u002F\u002Fdoi.org\u002F10.1016\u002FS0034-4257(02)00069-X",{"VOID":1142},"10.1007\u002Fs10712-023-09798-5","Auto Verify","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs10712-023-09798-5",[1146,1161,1176,1191,1204,1219,1234,1249,1262,1275],{"id":1147,"sortIndex":23,"researcher":22,"roles":1148,"affiliations":1149,"properties":1158,"displayName":1160,"givenName":22,"familyName":22},"91093a5f-e567-4ad4-bcac-9d6d362372ab",[970],[1150],{"id":1151,"sortIndex":23,"affiliation":1152,"properties":22},"c8a7f1b5-b1b9-4fdf-9dc5-7131fcc7ebc0",{"id":1151,"createTime":22,"updateTime":22,"relativeEntities":1153,"slug":22,"properties":1154,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1157,"statistic":22},[],{"title":1155},{"VI":1156},"Sorbonne University, LOCEAN\u002FIPSL laboratory, CNRS, IRD, MNHN, Paris, France",[],{"title":1159},{"VI":1160},"J. 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The Central Pontides, where the Eastern and Western Pontides met and formed a tectonic knot, represent an amalgamated tectonic mosaic consisting of remnants of oceanic, continental, and island arc segments. Subduction polarity, which is responsible for the formation of the Pontides, is still under debate because of limited geological, geophysical, and geochemical data. Two-dimensional (2-D) thermal modelling studies along the Central Pontides magmatic arc (Northern Turkey), Sakarya and Kırşehir continents are investigated in order to delineate the crustal thermal structure and subduction polarity. The obtained numerical results indicate that arc and back-arc regions are hot because of the cooling effects of a subducting plate. Moho temperatures in the investigated region are found between 992°C in the south (back-arc) and 415°C in the north (arc). Moreover, mantle heat flow values vary from 57.2 mWm−2 in the south (back-arc) to 34.7 mWm−2 in the north (arc). It is shown from this study that the Eurasia plate had moved from north to south under the Anatolia plate along the south Black Sea coast.",{"EN":1353},"Two-Dimensional Geothermal Modelling Along the Central Pontides Magmatic Arc: Implications for the Geodynamic Evolution of Northern Turkey",{"VOID":1355},"Adamia S, Lordkipanidze MB, Zakariadze GS (1977) Evolution of an active continental margin as exemplified by the Alpine history of the Caucasus. Tectonophysics 40:183–189\nAdamia SA, Chkhotua T, Kekelia M, Lordkipanidze M, Shavisvili I, Zahariadze F (1981) Tectonics of the caucasus and adjoining regions: implications for the evolution of the Tethys Ocean. J Struct Geol 3:437–447\nAteş A, Bilim F, Büyüksaraç A (2005) Curie point depth investigation of Central Anatolian Turkey. Pure Appl Geophys 162:357–371\nAydın I, Karat HI, Koçak A (2005) Curie-point depth map of Turkey. Geophys J Int 162:633–640\nBansal AR, Dimri VP (2001) Depth estimation from the scaling power spectral density of nonstationary gravity profile. Pure Appl Geophys 158:799–812\nBansal AR, Dimri VP, Sagar GV (2006) Depth estimation from gravity data using the maximum entropy method (MEM) and the multi taper method (MTM). Pure Appl Geophys 163:1417–1434\nBektaş Ö (1986) Paleostress trajectories and polyphase rifting in arc-back arc of Eastern Pontides, vol 103\u002F104. Mineral Research and Exploration Institute (MTA) Bulletin, Ankara, pp 1–15\nBektaş Ö, Van A, Boynukalın S (1987) Jurassic volcanism and its geotectonics in the eastern Pontides (NE Turkey). Geol Bull Turk 30:9–18\nBektaş Ö, Pelin S, Korkmaz S (1984) Mantle uprising and polygenetic ophiolite fact in the back-arc basin of the Eastern Pontides. In: TJK Ketin symposium, Ankara, Turkey, pp 175–188\nBektaş Ö, Şen C, Atıcı Y, Köprübaşı N (1999) Migration of the upper cretaceous subduction-related volcanism towards the back-arc basin of the Eastern Pontide magmatic arc (NE Turkey). Geol J 34:95–106\nBektaş Ö, Ravat D, Büyüksaraç A, Bilim F, Ateş A (2007) Regional geothermal characterization of East Anatolia from aeromagnetic, heat flow and gravity data. Pure Appl Geophys 164:975–998\nBhattacharyya BK (1966) Continuous spectrum of the total magnetic data due to a rectangular prismatic body. Geophysics 31:97–121\nBhattacharyya BK, Leu LK (1975) Spectral analysis of gravity and magnetic anomalies due to two-dimensional structures. Geophysics 40:993–1013\nBhattacharyya BK, Leu LK (1977) Spectral analysis of gravity and magnetic anomalies due to rectangular prismatic bodies. Geophysics 42:41–50\nBilim F (2007) Investigations into the tectonic lineaments and thermal structure of Kutahya–Denizli region, western Anatolia, from using aeromagnetic, gravity and seismological data. Phys Earth Planet Interiors 165:135–146\nBirch F, Roy RF, Decker ER (1968) Heat flow and thermal history in New England and New York. In: Zen E, White WS, Hadley JB, Thompson JB Jr (eds) Studies of appalachian geology: northern and maritime. Interscience, New York, pp 437–451\nBozkurt E (2001) Neotectonics of Turkey–a synthesis. Geodinamica Acta 14:3–30\nCermak V, Bodri L (1986) Tow-dimensional temperature modeling along five east-European geotraverses. J Geodyn 5:133–163\nCermak V, Rybach L (1989) Vertical distribution of heat production in the continental crust. Tectonophysics 159:217–230\nCermak V, Bodri L, Rybach L (1991) Radioactive heat production in the continental crust and its depth dependence. In: Cermak V, Rybach L (eds) Terrestrial heat flow and the lithosphere structure. 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Tectonophysics 6:251–269\nYılmaz Y, Tüysüz O, Yığıtbaş E, Can Genç Ş, Şengör AMC (1997) Geology and tectonic evolution of the Pontides, In: Robinson AG (ed) Regional and petroleum geology of the Black Sea and surrounding region: AAPG Memoir, vol 68, pp 183–226",{"VOID":1357},"10.1007\u002Fs10712-011-9158-7","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs10712-011-9158-7",[1360],{"id":1361,"sortIndex":23,"researcher":22,"roles":1362,"affiliations":1363,"properties":1372,"displayName":1374,"givenName":22,"familyName":22},"284a9c40-af53-480a-9981-447eec8fbd7b",[970],[1364],{"id":1365,"sortIndex":23,"affiliation":1366,"properties":22},"edf9fa04-bb08-4462-a085-893ed3fb9e4d",{"id":1365,"createTime":22,"updateTime":22,"relativeEntities":1367,"slug":22,"properties":1368,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1371,"statistic":22},[],{"title":1369},{"VI":1370},"Department of Geophysics, Gümüşhane University, Gümüşhane, Turkey",[],{"title":1373},{"VI":1374},"Nafiz Maden",{"url":1358,"publisher":1376,"properties":1422},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":1377,"slug":10,"properties":1378,"entityType":20,"verifyStatus":21,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":23,"subjectFields":1382,"manageAffiliations":1391,"indexDatabases":1402,"url":22,"thumbnailPath":22,"statistic":1417,"gsStatistic":22,"type":96,"analyzePriority":22},[],{"issn":1379,"title":1380,"eissn":1381},{"VOID":15},{"EN":17},{"VOID":13},[1383,1387],{"id":26,"createTime":22,"updateTime":22,"relativeEntities":1384,"label":1385,"description":1386,"parentId":22,"standard":22,"scholarHubFieldId":22},[],{"EN":29},{},{"id":32,"createTime":22,"updateTime":22,"relativeEntities":1388,"label":1389,"description":1390,"parentId":22,"standard":22,"scholarHubFieldId":22},[],{"EN":35},{},[1392,1397],{"id":39,"createTime":22,"updateTime":22,"relativeEntities":1393,"slug":22,"properties":1394,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1396,"statistic":22},[],{"title":1395},{"EN":43},[],{"id":46,"createTime":22,"updateTime":22,"relativeEntities":1398,"slug":22,"properties":1399,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1401,"statistic":22},[],{"title":1400},{"EN":50},[52],[1403,1410],{"id":55,"indexDatabase":1404,"url":68,"indexYears":22,"academicFieldIds":1409,"indexDatabaseRanking":22},{"id":57,"createTime":22,"updateTime":22,"relativeEntities":1405,"label":1406,"description":1407,"key":64,"publicationTags":1408,"standard":22},[],{"EN":60,"VI":60},{"EN":62,"VI":63},[66,67],[70],{"id":72,"indexDatabase":1411,"url":83,"indexYears":84,"academicFieldIds":1416,"indexDatabaseRanking":88},{"id":74,"createTime":22,"updateTime":22,"relativeEntities":1412,"label":1413,"description":1414,"key":80,"publicationTags":1415,"standard":22},[],{"EN":77,"VI":77},{"EN":77,"VI":79},[82],[86,87],{"impactFactor":23,"impactFactorByYear":1418,"i10Index":23,"i10IndexLast5Year":23,"totalPublication":91,"totalPublicationByYear":1419,"totalCitation":23,"totalCitationByYear":1420,"totalCitationPerPublication":23,"totalCitationPerPublicationByYear":1421,"hindexLast5Year":23,"hindex":23},{},{"1976":93,"1980":93},{},{},{"pages":1423,"volume":1425},{"VOID":1424},"275-292",{"VOID":1426},"33","2011-11-30",2011,[66,88],{"id":1431,"createTime":1432,"updateTime":1433,"relativeEntities":1434,"slug":1435,"properties":1436,"entityType":964,"verifyStatus":119,"verifyTime":1433,"verifyNote":1143,"languages":22,"translateLanguages":22,"viewCount":23,"primaryUrl":1445,"fullTextUrl":22,"authors":1446,"publicationType":1071,"publisherRelationship":1488,"citationCount":22,"citationInfo":22,"publishDate":1540,"publishYear":1541,"citationAnalyzeStatus":21,"lastCitationAnalyze":22,"indexDatabases":1542,"openAccess":22,"references":22,"isForceReanalyzing":1127},"01678093-ff27-4f65-90b0-77baf251fe20","2024-01-11T01:41:13.970+00:00","2024-12-27T18:39:41.353+00:00",[],"Array-Triplication-Data-Constraining-Seismic-Structure-and-Composition-in-the-Mantle",{"abstract":1437,"title":1439,"references":1441,"doi":1443},{"EN":1438},"Seismic data recorded in the upper mantle triplication distance range between 10° and 30° are generated by wave propagation through complex upper mantle structure. They can be used to place constraints on seismic velocity structures in the upper mantle, key seismic features near the major discontinuities, and anisotropic structure varying with depth. In this paper, we review wave propagation of the upper mantle triplicated phases, how different key seismic features can be studied using upper mantle triplicated data, and the importance of those seismic features to the understanding of mantle temperature and composition. We present two examples of using array triplicated phases to constrain upper mantle velocity structures and detailed features of a certain discontinuity, with one for a shallow event and the other for deep events. For the shallow event, we present examples of how the array triplication data can be used to constrain several key properties of the upper mantle: existence of a lithospheric lid, existence of a low velocity zone beneath the lithospheric lid, and P\u002FS velocity ratio as a function of depth. For deep events, we show examples of how array triplication data can be used to constrain the detailed structures of a certain discontinuity: velocity gradients above and below the discontinuity, velocity jumps across the discontinuity and depth extents of different velocity gradients. We discuss challenges of the upper mantle triplication study, its connection to other approaches, and its potential for further studying some other important features of the mantle: the existence of double 660-km discontinuities, existence of low-velocity channels near major discontinuities and anisotropy varying with depth.",{"EN":1440},"Array Triplication Data Constraining Seismic Structure and Composition in the Mantle",{"VOID":1442},"An Y, Gu YJ, Sacchi M (2007) Imaging mantle discontinuities using least-squares radon transform. J Geophys Res 112. doi:10.1029\u002F2007JB005009\nBercovici D, Karato S (2003) Whole-mantle convection and the transition-zone water filter. 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J Geophys Res 104:47830–47894",{"VOID":1444},"10.1007\u002Fs10712-009-9073-3","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs10712-009-9073-3",[1447,1462,1475],{"id":1448,"sortIndex":23,"researcher":22,"roles":1449,"affiliations":1450,"properties":1459,"displayName":1461,"givenName":22,"familyName":22},"43081007-c468-4e6b-b58d-8ad75bdab629",[970],[1451],{"id":1452,"sortIndex":23,"affiliation":1453,"properties":22},"da43d6b9-add1-415b-b5cc-d3dd4bb8c109",{"id":1452,"createTime":22,"updateTime":22,"relativeEntities":1454,"slug":22,"properties":1455,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1458,"statistic":22},[],{"title":1456},{"VI":1457},"Department of Geosciences, State University of New York at Stony Brook, Stony Brook, USA",[],{"title":1460},{"VI":1461},"Yi 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probabilistic seismic hazard analysis, assessment of the three recurrence parameters, namely the mean activity rate \n                  \n                    \n                  \n                  $$\\lambda$$\n                  \n                , Gutenberg–Richter \n                  \n                    \n                  \n                  $$b$$\n                  \n                -value, and maximum possible seismic event magnitude \n                  \n                    \n                  \n                  $$m_{\\max }$$\n                  \n                , is paramount. Over the years, several assessment procedures have been developed, each with its advantages and disadvantages. Typically, estimation techniques for the mean activity rate \n                  \n                    \n                  \n                  $$\\lambda$$\n                  \n                 and the Gutenberg–Richter \n                  \n                    \n                  \n                  $$b$$\n                  \n                -value are discussed and evaluated separately from those designed for the maximum possible event magnitude \n                  \n                    \n                  \n                  $$m_{\\max }$$\n                  \n                . Yet, the three parameters are typically defined in terms of joint distributions for \n                  \n                    \n                  \n                  $$\\lambda$$\n                  \n                , \n                  \n                    \n                  \n                  $$b$$\n                  \n                , and \n                  \n                    \n                  \n                  $$m_{\\max }$$\n                  \n                . In this study, we focused on systematically constructing joint distributions for the three recurrence parameters for considering complete and incomplete seismic event catalogues. The Bayesian formalism is introduced to constrain the parameter estimates with independent a priori information. Further, we discuss an iterative technique to solve the systems of equations sequentially. The procedures are compared and illustrated using Monte Carlo simulation and a seismic event catalogue for Cape Town, South Africa.\n \n                  \n                    \n                      \n                    \n                    \n                      \n                    \n                    \n                      \n                    \n                  \n                ",{"EN":1551},"Estimation Techniques for Seismic Recurrence Parameters for Incomplete Catalogues",{"VOID":1553},"Aki K (1965) Maximum likelihood estimate of b in the formula log N=a-bM and its confidence limits. Bull Earthq Res Inst Univ Tokyo 43:237–239\nAlamilla JL, Rodriguez JA, Vai R (2020) Unification of different approaches to probabilistic seismic hazard analysis. Bull Seismol Soc Am. https:\u002F\u002Fdoi.org\u002F10.1785\u002F0120200148\nAtkinson GM (2004) An overview of developments in seismic hazard analysis. Paper No. 5001. 13th World Conference on Earthquake Engineering Vancouver, B.C., Canada, August 1–6, 2004\nAXCO Insurance Market Report on South Africa – Non-Life, AXCO\nBeirlant J, Kijko A, Reynkens T, Einmahl JH (2019) Estimating the maximum possible earthquake magnitude using extreme value methodology: the Groningen case. Nat Hazards 98(3):1091–1113\nBender B (1988) Reliability of estimates of maximum earthquake magnitudes based on observed maxima. Seismol Res Lett 59(1):1–15\nBenjamin JR, Cornell CA (2014) Probability, statistics, and decision for civil engineers. Courier Corporation\nBommer JJ, Abrahamson NA (2006) Why do modern probabilistic seismic-hazard analyses often lead to increased hazard estimates? Bull Seismol Soc Am 96:1967–1977\nCalais E, Camelbeeck T, Stein S, Liu M, Craig TJ (2016) A new paradigm for large earthquakes in stable continental plate interiors. Geophys Res Lett. https:\u002F\u002Fdoi.org\u002F10.1002\u002F2016GL070815\nCheng RH, Traylor L (1995) Non-regular maximum likelihood problems. J R Stat Soc Series B Stat Methodol 57:3–44\nChinnery MA (1979) Investigations of the seismological input to the safety design of nuclear power reactors in New England. US Nuclear Regulatory Commission Report NUREG\u002FCR-0563, 72 pp\nCooke P (1979) Statistical inference for bounds of random variables. Biometrika 66:367–374\nCoppersmith KJ (1994) Conclusions regarding maximum earthquake assessment. In: Report: Johnston AC, Kanter LR, Coppersmith KJ Cornell CA (1994) The earthquakes of stable continental regions. vol 1: Assessment of large earthquake potential, Final Report, EPRI TR-102261-V1\nCornell CA (1968) Engineering seismic risk analysis. Bull Seismol Soc Am 58:1583–1606\nCornell CA (1994) Statistical analysis of maximum magnitudes in the earthquakes of stable continental regions. In: Report: Johnston AC, Kanter LR, Coppersmith KJ, Cornell CA (1994) The earthquakes of stable continental regions. vol. 1: Assessment of large earthquake potential, Final Report, EPRI TR-102261-V1\nCosentino P, Ficara V, Luzio D (1977) Truncated exponential frequency-magnitude relationship in the earthquake statistics. Bull Seismol Soc Am 67:1615–1623\nDavies N, Kijko A (2003) Seismic risk assessment: with an application to the South African insurance industry. S Afr Actuar J 3:1–28\nDavison AC (2003) Statistical models. Cambridge. Series in Statistical and Probabilistic Mathematics. Cambridge University Press, Cambridge.\nDeichmann N (2006) Local magnitude, a moment revisited. Bull Seism Soc Am 96:1267–1277\nEadie WT, Drijard D, James FE (1971) Statistical methods in experimental physics. North-Holland, Amsterdam\nEsteva L (1969) Seismicity prediction: A Bayesian approach. 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Bull Seismol Soc Am 46:105–145\nHamilton RM (1967) Mean magnitude of an earthquake sequence. Bull Seismol Soc Am 57:1115–1126\nHeaton T, Tajima F, Mori A (1986) Estimating ground motions using recorded accelerograms. Surv Geophys 8:25–83\nHolschneider M, Zöller G, Hainzl S (2011) Estimation of the maximum possible magnitude in the framework of a doubly truncated Gutenberg-Richter model. Bull Seismol Soc Am 101:1649–1659\nIsacks B, Oliver J (1964) Seismic waves with frequencies from 1 to 100 cycles per second recorded in a deep mine in northern New Jersey. Bull Seismol Soc Am 54:1941–1979\nIshimoto M, Iida K (1939) Observations of earthquakes registered with the micro seismograph constructed recently. Bull Earthq Res Inst Univ Tokyo 17:443–478\nIervolino, I, Giorgio M (2015) Stochastic modeling of recovery from seismic shocks. 12th International Conference on Applications of Statistics and Probability in Civil Engineering, ICASP12, Vancouver, Canada, July 12–15, 2015\nJohnson NL, Kotz S, Balakrishnan N (1994) Continuous univariate distributions. vol. 1, 2nd ed. John Willey & Sons, New York\nJohnston AC (1994) Seismotectonic interpretations and conclusions from the Stable Continental Region Seismicity Database. In: Report: Johnston AC, Kanter LR, Coppersmith KJ, Cornell CA (1994) The earthquakes of stable continental regions. vol 1: Assessment of large earthquake potential, Final Report, EPRI TR-102261-V1\nKagan YY (2002a) Seismic moment distribution revisited: I. Statistical Results Geophys J Int 148(3):520–541. https:\u002F\u002Fdoi.org\u002F10.1046\u002Fj.1365-246x.2002.01594.x\nKagan YY (2002b) Seismic moment distribution revisited: II. Moment Conserv Principle Geophys J Int 149:731–754. https:\u002F\u002Fdoi.org\u002F10.1046\u002Fj.1365-246X.2002.01671.x\nKendall M, Stuart A (1967) The advanced theory of statistics in inference and relationship, vol 2. Griffin, London\nKijko A (2004) Estimation of the maximum earthquake magnitude, mmax. Pure Appl Geophys 161:1655–1681\nKijko A (2012) On Bayesian procedure for maximum earthquake magnitude estimation. Res Geophys 2(1):7. https:\u002F\u002Fdoi.org\u002F10.4081\u002Frg.2012.e7\nKijko A, Graham G (1998) “Parametric-Historic” procedure for probabilistic seismic hazard analysis. Part I Assess Maximum Regional Magnitude mMax 152:413–442\nKijko A, Sellevoll MA (1989) Estimation of earthquake hazard parameters from incomplete data files. Part I. Utilization of extreme and complete catalogs with different threshold magnitudes. Bull Seismol Soc Am 79:645–654\nKijko A, Sellevoll MA (1992) Estimation of earthquake hazard parameters from incomplete data files. Part II. Incorporation of magnitude heterogeneity. Bull Seismol Soc Am 82:120–134\nKijko A, Singh M (2011) Statistical tools for maximum possible earthquake magnitude estimation. Acta Geophys 59(4):674–700\nKijko A, Smit A (2012) Extension of the Aki-Utsu b-value estimator for incomplete catalogs. Bull Seismol Soc Am 102:1283–1287\nKijko A, Smit A, Sellevoll MA (2016) Estimation of earthquake hazard parameters from incomplete data files. Part III. Incorporation of uncertainty of earthquake-occurrence model. Bull Seismol Soc Am 106:1210–1222\nLeCam L (1970) On the assumptions used to prove asymptotic normality of maximum likelihood estimates. Ann Statist 41:802–828\nManzunzu B, Brandt MBC, Midzi V, Durrheim RJ, Saunders I, Mulabisana TF (2021) Towards a homogeneous moment magnitude determination for earthquakes in South Africa: Reduction of associated uncertainties. J Afr Earth Sci 173:1–11\nMarzocchi W, Sandri L (2003) A review and new insights on the estimation of the b-value and its uncertainty. Ann Geophys 46:1271–1282\nMcGuire RK (1976) FORTRAN computer program for seismic risk analysis, U.S. Geol Surv Open-File Report 76:1–67\nMcGuire R (2008) Probabilistic seismic hazard analysis: early history. Earthq Eng Struct Dyn 37:329–338\nMolchan GM, Keilis-Borok VL, Vilkovich V (1970) Seismicity and principal seismic effects. Geophys J Int 21:323–335. https:\u002F\u002Fdoi.org\u002F10.1111\u002Fj.1365-246X.1970.tb01795.x\nMood AM, Graybill F, Boes DC (1974) Introduction to the theory of statistics. McGraw-Hill, Auckland\nNewmark NM, Rosenblueth E (1971) Fundamentals of earthquake engineering. Prentice-Hall, Englewood Cliffs\nPagani MM, Monelli D, Weatherill G, Danciu L, Crowley H, Silva V, Henshaw P, Butler L, Nastasi M, Panzeri L, Simionato M, Vigano D (2014) OpenQuake engine: an open hazard (and risk) software for the global earthquake model. 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In: Proceedings of the 1st International Conference on Microzonation, Seattle\nStevens VL, Avouac J-P (2017) Determination of Mmax from background seismicity and moment conservation. Bull Seismol Soc Am 107:2578–2596\nTate RF (1959) Unbiased estimation: Function of location and scale parameters. Ann Math Statist 30:331–366\nUtsu T (1965) A method for determining the value of b in the formula log(n) = a–bM showing the magnitude-frequency relation for earthquakes (with English summary). Geophys Bull Hokkaido Univ 13:99–103\nVermeulen PJ (2020) Problems in parameter estimation in probabilistic seismic hazard analysis and some solutions, PhD Thesis, Faculty of Natural and Agricultural Sciences, University of Pretoria, Pretoria, February 2020, pp 139\nVermeulen PJ, Kijko A (2017) More statistical tools for maximum possible earthquake magnitude estimation. Acta Geophys 65:579–587. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs11600-017-0048-3\nVermeulen PJ, Kijko A (2019) Joint maximum likelihood estimators for Gutenberg-Richter parameters λ0 and β using subcatalogs. Earthq Spectra 35:1053–1058\nWeichert DH (1980) Estimation of the earthquake recurrence parameters for unequal observation periods for different magnitudes. Bull Seismol Soc Am 70:1337–1346\nWeichert DH, Kijko A (1989) Estimation of earthquake recurrence parameters from incomplete and variably complete catalogue. Seismol Res Lett 60:28\nWheeler RL (2009) Methods of Mmax estimation east of Rocky Mountains. USGS, Open-File Report 2009–1018",{"VOID":1555},"10.1007\u002Fs10712-021-09672-2","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs10712-021-09672-2",[1558,1573,1588],{"id":1559,"sortIndex":23,"researcher":22,"roles":1560,"affiliations":1561,"properties":1570,"displayName":1572,"givenName":22,"familyName":22},"38ef643e-023c-4f21-a729-913845e67192",[970],[1562],{"id":1563,"sortIndex":23,"affiliation":1564,"properties":22},"ccc984f7-70a5-413e-89c7-4dfa3fc8c649",{"id":1563,"createTime":22,"updateTime":22,"relativeEntities":1565,"slug":22,"properties":1566,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1569,"statistic":22},[],{"title":1567},{"VI":1568},"University of Pretoria Natural Hazard Centre, University of Pretoria, Pretoria, South Africa",[],{"title":1571},{"VI":1572},"Andrzej Kijko",{"id":1574,"sortIndex":93,"researcher":22,"roles":1575,"affiliations":1576,"properties":1585,"displayName":1587,"givenName":22,"familyName":22},"78573e44-66c7-40e9-aeb5-941c66a8cce1",[970],[1577],{"id":1578,"sortIndex":23,"affiliation":1579,"properties":22},"49e983d6-b6ab-46d6-91ec-2c4504277057",{"id":1578,"createTime":22,"updateTime":22,"relativeEntities":1580,"slug":22,"properties":1581,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1584,"statistic":22},[],{"title":1582},{"VI":1583},"Cullinan, South Africa",[],{"title":1586},{"VI":1587},"Petrus Johannes Vermeulen",{"id":1589,"sortIndex":91,"researcher":22,"roles":1590,"affiliations":1591,"properties":1600,"displayName":1602,"givenName":22,"familyName":22},"ff56da92-dfd3-413e-b78d-684d0407453f",[970],[1592],{"id":1593,"sortIndex":23,"affiliation":1594,"properties":22},"17a5ca94-9a0e-4f0c-bd08-64021908b246",{"id":1593,"createTime":22,"updateTime":22,"relativeEntities":1595,"slug":22,"properties":1596,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1599,"statistic":22},[],{"title":1597},{"VI":1598},"Department of Geology, University of Pretoria Natural Hazard Centre, University of Pretoria, Pretoria, South Africa",[],{"title":1601},{"VI":1602},"Ansie Smit",{"url":1556,"publisher":1604,"properties":1650},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":1605,"slug":10,"properties":1606,"entityType":20,"verifyStatus":21,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":23,"subjectFields":1610,"manageAffiliations":1619,"indexDatabases":1630,"url":22,"thumbnailPath":22,"statistic":1645,"gsStatistic":22,"type":96,"analyzePriority":22},[],{"issn":1607,"title":1608,"eissn":1609},{"VOID":15},{"EN":17},{"VOID":13},[1611,1615],{"id":26,"createTime":22,"updateTime":22,"relativeEntities":1612,"label":1613,"description":1614,"parentId":22,"standard":22,"scholarHubFieldId":22},[],{"EN":29},{},{"id":32,"createTime":22,"updateTime":22,"relativeEntities":1616,"label":1617,"description":1618,"parentId":22,"standard":22,"scholarHubFieldId":22},[],{"EN":35},{},[1620,1625],{"id":39,"createTime":22,"updateTime":22,"relativeEntities":1621,"slug":22,"properties":1622,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1624,"statistic":22},[],{"title":1623},{"EN":43},[],{"id":46,"createTime":22,"updateTime":22,"relativeEntities":1626,"slug":22,"properties":1627,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1629,"statistic":22},[],{"title":1628},{"EN":50},[52],[1631,1638],{"id":55,"indexDatabase":1632,"url":68,"indexYears":22,"academicFieldIds":1637,"indexDatabaseRanking":22},{"id":57,"createTime":22,"updateTime":22,"relativeEntities":1633,"label":1634,"description":1635,"key":64,"publicationTags":1636,"standard":22},[],{"EN":60,"VI":60},{"EN":62,"VI":63},[66,67],[70],{"id":72,"indexDatabase":1639,"url":83,"indexYears":84,"academicFieldIds":1644,"indexDatabaseRanking":88},{"id":74,"createTime":22,"updateTime":22,"relativeEntities":1640,"label":1641,"description":1642,"key":80,"publicationTags":1643,"standard":22},[],{"EN":77,"VI":77},{"EN":77,"VI":79},[82],[86,87],{"impactFactor":23,"impactFactorByYear":1646,"i10Index":23,"i10IndexLast5Year":23,"totalPublication":91,"totalPublicationByYear":1647,"totalCitation":23,"totalCitationByYear":1648,"totalCitationPerPublication":23,"totalCitationPerPublicationByYear":1649,"hindexLast5Year":23,"hindex":23},{},{"1976":93,"1980":93},{},{},{"pages":1651,"volume":1653},{"VOID":1652},"597-617",{"VOID":1654},"43","2021-11-20",2021,[66,88],{"id":1659,"createTime":1660,"updateTime":1661,"relativeEntities":1662,"slug":1663,"properties":1664,"entityType":964,"verifyStatus":119,"verifyTime":1661,"verifyNote":1143,"languages":22,"translateLanguages":22,"viewCount":23,"primaryUrl":1673,"fullTextUrl":22,"authors":1674,"publicationType":1071,"publisherRelationship":1818,"citationCount":22,"citationInfo":22,"publishDate":1870,"publishYear":1871,"citationAnalyzeStatus":21,"lastCitationAnalyze":22,"indexDatabases":1872,"openAccess":22,"references":22,"isForceReanalyzing":1127},"025d7ab5-1177-4156-8f50-7f60ffa65c95","2023-12-07T10:42:40.526+00:00","2024-12-25T13:52:55.404+00:00",[],"Early-Lessons-on-Combining-Lidar-and-Multi-baseline-SAR-Measurements-for-Forest-Structure-Characterization",{"abstract":1665,"title":1667,"references":1669,"doi":1671},{"EN":1666},"The estimation and monitoring of 3D forest structure at large scales strongly rely on the use of remote sensing techniques. Today, two of them are able to provide 3D forest structure estimates: lidar and synthetic aperture radar (SAR) configurations. The differences in wavelength, imaging geometry, and technical implementation make the measurements provided by the two configurations different and, when it comes to the sensitivity to individual 3D forest structure components, complementary. Accordingly, the potential of combining lidar and SAR measurements toward an improved 3D forest structure estimation has been recognised from the very beginning. However, until today there is no established framework for this combination. This paper attempts to review differences, commonalities, and complementarities of lidar and SAR measurements. First, vertical lidar reflectance and SAR reflectivity profiles at different wavelengths are compared in different forest types. Then, current perspectives on their combination for the generation of enhanced structure products are discussed. Two promising frameworks for combining lidar and SAR measurements are reviewed. The first one is a model-based framework where lidar-derived parameters are used to initialize SAR scattering models, and relies on both the validity of the models and on the physical equivalence of the used lidar and SAR parameters. The second one is a structure-based framework based on the ability of lidar and SAR measurements to express physical forest structure by means of appropriate indices. These indices can then be used to establish a link between the two kind of measurements. The review is supported by experimental results achieved using space- and airborne data acquired in recent relevant mission and campaigns.",{"EN":1668},"Early Lessons on Combining Lidar and Multi-baseline SAR Measurements for Forest Structure Characterization",{"VOID":1670},"Aguilera E, Nannini M, Reigber A (2013) Wavelet-based compressed sensing for SAR tomography of forested areas. 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Papathanassiou",{"id":1793,"sortIndex":445,"researcher":22,"roles":1794,"affiliations":1795,"properties":1802,"displayName":1804,"givenName":22,"familyName":22},"df30163d-36c9-4d1e-affd-ac3acf5745d2",[970],[1796],{"id":1695,"sortIndex":23,"affiliation":1797,"properties":22},{"id":1695,"createTime":22,"updateTime":22,"relativeEntities":1798,"slug":22,"properties":1799,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1801,"statistic":22},[],{"title":1800},{"VI":1700},[],{"title":1803},{"VI":1804},"Ralph O. Dubayah",{"id":1806,"sortIndex":233,"researcher":22,"roles":1807,"affiliations":1808,"properties":1815,"displayName":1817,"givenName":22,"familyName":22},"1cb3cb3d-dd72-431c-bd07-3a35ce8c5bf6",[970],[1809],{"id":1729,"sortIndex":23,"affiliation":1810,"properties":22},{"id":1729,"createTime":22,"updateTime":22,"relativeEntities":1811,"slug":22,"properties":1812,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1814,"statistic":22},[],{"title":1813},{"VI":1734},[],{"title":1816},{"VI":1817},"Lola E. Fatoyinbo",{"url":1673,"publisher":1819,"properties":1865},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":1820,"slug":10,"properties":1821,"entityType":20,"verifyStatus":21,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":23,"subjectFields":1825,"manageAffiliations":1834,"indexDatabases":1845,"url":22,"thumbnailPath":22,"statistic":1860,"gsStatistic":22,"type":96,"analyzePriority":22},[],{"issn":1822,"title":1823,"eissn":1824},{"VOID":15},{"EN":17},{"VOID":13},[1826,1830],{"id":26,"createTime":22,"updateTime":22,"relativeEntities":1827,"label":1828,"description":1829,"parentId":22,"standard":22,"scholarHubFieldId":22},[],{"EN":29},{},{"id":32,"createTime":22,"updateTime":22,"relativeEntities":1831,"label":1832,"description":1833,"parentId":22,"standard":22,"scholarHubFieldId":22},[],{"EN":35},{},[1835,1840],{"id":39,"createTime":22,"updateTime":22,"relativeEntities":1836,"slug":22,"properties":1837,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1839,"statistic":22},[],{"title":1838},{"EN":43},[],{"id":46,"createTime":22,"updateTime":22,"relativeEntities":1841,"slug":22,"properties":1842,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1844,"statistic":22},[],{"title":1843},{"EN":50},[52],[1846,1853],{"id":55,"indexDatabase":1847,"url":68,"indexYears":22,"academicFieldIds":1852,"indexDatabaseRanking":22},{"id":57,"createTime":22,"updateTime":22,"relativeEntities":1848,"label":1849,"description":1850,"key":64,"publicationTags":1851,"standard":22},[],{"EN":60,"VI":60},{"EN":62,"VI":63},[66,67],[70],{"id":72,"indexDatabase":1854,"url":83,"indexYears":84,"academicFieldIds":1859,"indexDatabaseRanking":88},{"id":74,"createTime":22,"updateTime":22,"relativeEntities":1855,"label":1856,"description":1857,"key":80,"publicationTags":1858,"standard":22},[],{"EN":77,"VI":77},{"EN":77,"VI":79},[82],[86,87],{"impactFactor":23,"impactFactorByYear":1861,"i10Index":23,"i10IndexLast5Year":23,"totalPublication":91,"totalPublicationByYear":1862,"totalCitation":23,"totalCitationByYear":1863,"totalCitationPerPublication":23,"totalCitationPerPublicationByYear":1864,"hindexLast5Year":23,"hindex":23},{},{"1976":93,"1980":93},{},{},{"pages":1866,"volume":1868},{"VOID":1867},"803-837",{"VOID":1869},"40","2019-07-09",2019,[66,88],{"id":1874,"createTime":1875,"updateTime":1875,"relativeEntities":1876,"slug":1877,"properties":1878,"entityType":964,"verifyStatus":21,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":23,"primaryUrl":1887,"fullTextUrl":22,"authors":1888,"publicationType":1071,"publisherRelationship":1939,"citationCount":22,"citationInfo":22,"publishDate":1991,"publishYear":1992,"citationAnalyzeStatus":21,"lastCitationAnalyze":22,"indexDatabases":1993,"openAccess":22,"references":22,"isForceReanalyzing":1127},"02ae7f83-082d-489f-bd45-aefd5d4a6aba","2023-11-27T04:51:48.233+00:00",[],"Diurnal-Periodicity-of-Weak-Earthquakes-in-the-Zhongar-North-Tian-Shan-Region",{"abstract":1879,"title":1881,"references":1883,"doi":1885},{"EN":1880},"A targeted exploration of the dependence of seismic activity on the time of day continues for about a century and a half. During this time, numerous scientific studies have been done on the diurnal periodicity in the occurrence of earthquakes. In this work, we present the first results of a study of diurnal periodicity in the occurrence of weak earthquakes by the example of individual seismically active zones of the Zhongar North Tian Shan region. The research was performed on the data on number of earthquakes with energy classes (K = logE, J) equal to 5, 6, 7 and 8, which arose within the North Tian Shan (1), Zhongar (2), Halyktau (3) and Ketmen (4) zones. To do this, by counting the number of earthquakes of corresponding energy that occurred during each hour, a time series of hourly values of number of shocks for the entire time period was compiled. Then, using the method of superposition of periods, the number of seismic events for each hour over the entire time interval is summed up, and a graph of the average daily course of the number of earthquakes was compiled. Studies have established the existence of diurnal periodicity in the realization of weak earthquakes and microquakes. It was most clearly observed for seismic events with K ≤ 6 for the North Tien Shan, Zhongar, Ketmen, and K ≤ 7 for Halyktau zones. With an increase in energy class (magnitude) of earthquakes, the observed pattern weakens and practically disappears for shocks with K ≥ 7 for the earthquakes, Zhongar, Ketmen and with K ≥ 8 for the Halyktau zones. The obtained graphs of the diurnal sequence of seismicity are identical to the analogous curves of diurnal variation in the numbers of weak earthquakes allocated for other regions (areas) of the globe.",{"EN":1882},"Diurnal Periodicity of Weak Earthquakes in the Zhongar North Tian Shan Region",{"VOID":1884},"Adushkin VV, Kocharyan GG (eds) (2010) Trigger effects in geosystems. Materials of the all-Russian seminar-meeting. GEOS, Moscow\nAtef A, Liu K, Gao S (2009) Apparent weekly and daily earthquake periodicities in the Western United States. Bull Seismol Soc Am 99(4):2273–2279\nBelyakov AS, Zhuravlev VI, Lucc AA (2011) The daily frequency of weak earthquakes and high-frequency underground noise in Kamchatka. Phys Earth 3:34–54\nBogomolov LM, Sychev VN, Sycheva NA (2012) On the diurnal periodicity of the random component in the stream of seismic events. Pac Geol 31(6):68–78\nBogomolov LM, Sychev VN, Sycheva NA (2013) Seismological applications of non-standard seismic analysis. Bull Far East Branch Russ Acad Sci 3:19–25\nDescherovskaya EV, Sidorin AYa (2004) The reason for the seasonal periodicity of earthquakes according to observations at the Garm test site. OIFZ RAS, Moscow\nDescherovskaya EV, Sidorin AYa (2005) The daily frequency of earthquakes of the Garm landfill. RAS Rep 402(3):383–387\nDescherovskaya EV, Sidorin AYa (2012) Daily frequency of Greek earthquakes. Seism Instrum 48(3):5–31\nDescherovskaya EV, Sidorin AYa (2014) Daily frequency of Southern California earthquakes. Seism Instrum 50(1):27–50\nGavrilov VA, Morozova YuV, Storcheus AV (2006) Variations in the level of geoacoustic emission in the deep well G-1 (Kamchatka) and their relationship with seismic activity. Volcanol Seism 1:52–67\nHao J, Zhang J, Yao Z (2019) Evidence for diurnal periodicity of earthquakes from midnight to daybreak. Natl Sci Rev 6(5):1016–1023\nKolosova EA, Lucc AA, Serova AYa, Sidorin AYa (2015) Natural and technogenic sources of trigger activity of seismicity and seismic noise. NTR 94(4):30–43\nMikhailova NN, Komarov II (2009) Glacial earthquakes of the Central Tien Shan. Bull NNC RK 3:120–126\nNanjo KZ, Tsuruoka H, Ishibe T, Hirata N, Ishigaki Y, Schorlemmer D (2010) Analysis of the completeness magnitude and seismic network coverage of Japan. Bull Seismol Soc Am 100(6):3261–3268\nNurmagambetov A (1999) Seismic history of Almaty. LEM, Almaty\nReznik N (2006) Hour of earthquakes. https:\u002F\u002Fwww.ng.ru\u002Fscience\u002F2006-06-14\u002F15_earthquake.html. Accessed 14 June 2006\nSadykova AB (2012) Seismic hazard of the territory of Kazakhstan. High Technology, Almaty\nSchorlemmer D, Mele F, Marzocchi W (2010) A completeness analysis of the National Seismic Network of Italy. J Geophys Res Solid Earth 115(B4). https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002Ffull\u002F10.1029\u002F2008JB006097. Accessed 08 Apr 2010\nShimshoni M (1971) Evidence to higher seismic activity during the night. J Geophys Res Solid Earth 24:97–99\nSidorin AYa (2009) Daily frequency of Greek earthquakes. Seism Instrum 45(3):60–76\nSidorin AYa (2013) Features of the diurnal periodicity of earthquakes in Japan. Seism Instrum 49(3):55–84\nSidorenkov NS (1979) Investigation of the non-tidal irregularity of the Earth's rotation and its connection with processes in the atmosphere. Dissertation, GAISH\nSydykov A (2004) Seismic regime of the territory of Kazakhstan. Gylym, Almaty\nSychev VN, Bogomolov LM, Sycheva NA (2012) On the diurnal periodicity of the random component in the stream of seismic events. Pac Geol 31(6):68–78\nZharov VE (2005) Earth rotation and time scales. Sci Russ 1(145):4–9\nZhuravlev VI, Sidorin AYa (2005) General properties of the diurnal periodicity of an earthquake in some parts of the world. Geophys Res 2:61–70\nZhuravlev VI, Lucc AA (2011) Midday activation of seismicity in Turkey in a number of other regions of the world. Geophys Res 12(4):31–57\nZhuravlev VI, Lucc AA (2012) Features of the diurnal periodicity of weak earthquakes in Iran. Phys Earth 1:63–81\nZhuravlev VI, Lucc AA, Mirzoev KM, Sycheva NA (2006) Daily frequency of weak earthquakes in Central Asia. Phys Earth 11:29–43",{"VOID":1886},"10.1007\u002Fs10712-020-09622-4","http:\u002F\u002Flink.springer.com\u002F10.1007\u002Fs10712-020-09622-4",[1889,1904,1917],{"id":1890,"sortIndex":23,"researcher":22,"roles":1891,"affiliations":1892,"properties":1901,"displayName":1903,"givenName":22,"familyName":22},"e346e922-54da-44dd-8f42-547ec004f42c",[970],[1893],{"id":1894,"sortIndex":23,"affiliation":1895,"properties":22},"19cb55ba-aeda-414c-979d-140b78ee0ce0",{"id":1894,"createTime":22,"updateTime":22,"relativeEntities":1896,"slug":22,"properties":1897,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1900,"statistic":22},[],{"title":1898},{"VI":1899},"Laboratory of Regional Seismicity, Institute of Seismology, Almaty, Republic of Kazakhstan",[],{"title":1902},{"VI":1903},"Aluadin Sydykov",{"id":1905,"sortIndex":93,"researcher":22,"roles":1906,"affiliations":1907,"properties":1914,"displayName":1916,"givenName":22,"familyName":22},"6afa4384-96a6-4566-bdeb-18e82a102fb1",[970],[1908],{"id":1894,"sortIndex":23,"affiliation":1909,"properties":22},{"id":1894,"createTime":22,"updateTime":22,"relativeEntities":1910,"slug":22,"properties":1911,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1913,"statistic":22},[],{"title":1912},{"VI":1899},[],{"title":1915},{"VI":1916},"Alla B. Sadykova",{"id":1918,"sortIndex":91,"researcher":22,"roles":1919,"affiliations":1920,"properties":1936,"displayName":1938,"givenName":22,"familyName":22},"9f451ca2-79d4-4641-bdbe-0efa35765d58",[970],[1921,1927],{"id":1894,"sortIndex":23,"affiliation":1922,"properties":22},{"id":1894,"createTime":22,"updateTime":22,"relativeEntities":1923,"slug":22,"properties":1924,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1926,"statistic":22},[],{"title":1925},{"VI":1899},[],{"id":1928,"sortIndex":93,"affiliation":1929,"properties":1935},"209428cc-32ce-4fc1-9cfc-c4a7043886e5",{"id":1928,"createTime":22,"updateTime":22,"relativeEntities":1930,"slug":22,"properties":1931,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1934,"statistic":22},[],{"title":1932},{"VI":1933},"Department of Geophysics, Satbayev University, Almaty, Republic of Kazakhstan",[],{},{"title":1937},{"VI":1938},"Akgenzhe O. Siylkanova",{"url":1887,"publisher":1940,"properties":1986},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":1941,"slug":10,"properties":1942,"entityType":20,"verifyStatus":21,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":23,"subjectFields":1946,"manageAffiliations":1955,"indexDatabases":1966,"url":22,"thumbnailPath":22,"statistic":1981,"gsStatistic":22,"type":96,"analyzePriority":22},[],{"issn":1943,"title":1944,"eissn":1945},{"VOID":15},{"EN":17},{"VOID":13},[1947,1951],{"id":26,"createTime":22,"updateTime":22,"relativeEntities":1948,"label":1949,"description":1950,"parentId":22,"standard":22,"scholarHubFieldId":22},[],{"EN":29},{},{"id":32,"createTime":22,"updateTime":22,"relativeEntities":1952,"label":1953,"description":1954,"parentId":22,"standard":22,"scholarHubFieldId":22},[],{"EN":35},{},[1956,1961],{"id":39,"createTime":22,"updateTime":22,"relativeEntities":1957,"slug":22,"properties":1958,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1960,"statistic":22},[],{"title":1959},{"EN":43},[],{"id":46,"createTime":22,"updateTime":22,"relativeEntities":1962,"slug":22,"properties":1963,"entityType":22,"verifyStatus":22,"verifyTime":22,"verifyNote":22,"languages":22,"translateLanguages":22,"viewCount":22,"url":22,"parentIds":1965,"statistic":22},[],{"title":1964},{"EN":50},[52],[1967,1974],{"id":55,"indexDatabase":1968,"url":68,"indexYears":22,"academicFieldIds":1973,"indexDatabaseRanking":22},{"id":57,"createTime":22,"updateTime":22,"relativeEntities":1969,"label":1970,"description":1971,"key":64,"publicationTags":1972,"standard":22},[],{"EN":60,"VI":60},{"EN":62,"VI":63},[66,67],[70],{"id":72,"indexDatabase":1975,"url":83,"indexYears":84,"academicFieldIds":1980,"indexDatabaseRanking":88},{"id":74,"createTime":22,"updateTime":22,"relativeEntities":1976,"label":1977,"description":1978,"key":80,"publicationTags":1979,"standard":22},[],{"EN":77,"VI":77},{"EN":77,"VI":79},[82],[86,87],{"impactFactor":23,"impactFactorByYear":1982,"i10Index":23,"i10IndexLast5Year":23,"totalPublication":91,"totalPublicationByYear":1983,"totalCitation":23,"totalCitationByYear":1984,"totalCitationPerPublication":23,"totalCitationPerPublicationByYear":1985,"hindexLast5Year":23,"hindex":23},{},{"1976":93,"1980":93},{},{},{"pages":1987,"volume":1989},{"VOID":1988},"21-41",{"VOID":1990},"42","2020-12-05",2020,[66,88],{"id":1995,"createTime":1996,"updateTime":1997,"relativeEntities":1998,"slug":1999,"properties":2000,"entityType":964,"verifyStatus":119,"verifyTime":1997,"verifyNote":1143,"languages":22,"translateLanguages":22,"viewCount":23,"primaryUrl":2009,"fullTextUrl":22,"authors":2010,"publicationType":1071,"publisherRelationship":2026,"citationCount":22,"citationInfo":22,"publishDate":2078,"publishYear":1125,"citationAnalyzeStatus":21,"lastCitationAnalyze":22,"indexDatabases":2079,"openAccess":22,"references":22,"isForceReanalyzing":1127},"02ce7ad2-cfe1-4727-aa42-21f213156ea3","2023-12-07T06:54:24.238+00:00","2025-02-08T16:59:44.091+00:00",[],"The-Physics-of-Lightning",{"abstract":2001,"title":2003,"references":2005,"doi":2007},{"EN":2002},"An overview of the physics of cloud-to-ground lightning is given, including its initiation, propagation, and attachment to ground. Discharges artificially initiated (triggered) from natural thunderclouds using the rocket-and-wire technique are discussed with a view toward studying properties of natural lightning. Both conventional and runaway breakdown mechanisms of lightning initiation in thunderclouds are reviewed, as is the role of the lower positive charge region in facilitating different types of lightning. New observations of negative-leader stepping and its attachment to ground are compared to similar processes in long laboratory sparks. The mechanism and parameters of compact intracloud lightning discharges that are thought to be the most intense natural producers of HF-VHF (3–300 MHz) radiation on Earth are reviewed. The M-component mode of charge transfer to ground and its difference from the leader\u002Freturn-stroke mode are discussed. Lightning interaction with the ionosphere and the production of energetic radiation (X-rays and gamma radiation) by cloud-to-ground leaders are considered.",{"EN":2004},"The Physics of Lightning",{"VOID":2006},"Bazelyan EM, Raizer YuP (2000) Lightning physics and lightning protection, 325 p. IOP, Bristol\nBazelyan EM, Gorin BN, Levitov VI (1978) Physical and engineering foundations of lightning protection, 223 p. Gidrometeoizdat, Leningrad\nBeasley WH, Uman MA, Rustan PL (1982) Electric fields preceding cloud-to-ground lightning flashes. J Geophys Res 87:4883–4902\nBetz HD, Schumann U, Laroche P (eds) (2009) Lightning: principles, instruments and applications. Springer, 691 p\nBiagi CJ, Jordan DM, Uman MA, Hill JD, Beasley WH, Howard J (2009) High-speed video observations of rocket-and-wire initiated lightning. Geophys Res Lett 36:L15801. doi:10.1029\u002F2009GL038525\nBiagi CJ, Uman MA, Hill JD, Jordan DM, Rakov VA, Dwyer JR (2010) Observations of stepping mechanisms in a rocket-and-wire triggered lightning flash. J Geophys Res 115:D23215. doi:10.1029\u002F2010JD014616\nBrook M, Ogawa T (1977) The cloud discharge. In R. Golde (ed) Lightning, vol. 1, Physics of lightning. Academic Press, London, pp. 191–230\nChen M, Takagi N, Watanabe T, Wang D, Kawasaki Z-I, Liu X (1999) Spatial and temporal properties of optical radiation produced by stepped leaders. J Geophys Res 104:27573–27584\nCooray GV (ed) (2003) The lightning flash, 574 p. The Institution of Electrical Engineers, London\nCooray V, Becerra M, Rakov VA (2009) On the electric field at the tip of dart leaders in lightning flashes. J Atmos Solar-Terr Phys 71(12):1397–1404. doi:10.1016\u002Fj.jastp.2009.06.002\nCooray V, Dwyer JR, Rakov VA, Rahman M (2010) On the mechanism of X-ray production by dart leaders of lightning flashes. J Atmos Solar-Terr Phys 72(11–12):848–855. doi:10.1016\u002Fj.jastp.2010.04.006\nDwyer JR, Babich LP (2011) Low-energy electron production by relativistic runaway electron avalanches in air. J Geophys Res 116:A09301. doi:10.1029\u002F2011JA016494\nDwyer JR, Babich L (2012) Reply to comment by A. V. Gurevich et al. on “Low-energy electron production by relativistic runaway electron avalanches in air”. J Geophys Res 117:A04303. doi:10.1029\u002F2011JA017487\nDwyer JR, Schaal M, Rassoul HK, Uman MA, Jordan DM, Hill D (2011) High-speed X-ray images of triggered lightning dart leaders. J Geophys Res 116:D20208. doi:10.1029\u002F2011JD015973\nEidelman S et al (2004) Review of particle physics. Phys Lett B 592:1–1109. doi:10.1016\u002Fj.physletb.2004.06.001\nGorin BN, Levitov VI, Shkilev AV (1976) Some principles of leader discharge of air gaps with a strong non-uniform field. Gas discharges. IEE Conf Publ 143:274–278\nGriffiths RF, Phelps CT (1976a) The effects of air pressure and water vapour content on the propagation of positive corona streamers, and their implications to lightning initiation. Q J Roy Meteor Soc 102:419–426\nGriffiths RF, Phelps CT (1976b) A model of lightning initiation arising from positive corona streamer development. J Geophys Res 31:3671–3676\nGurevich AV, Zybin KP (2001) Runaway breakdown and electric discharges in thunderstorms. Physics–Uspekhi 44 (11): 1119–1140\nGurevich AV, Milikh GM, Roussel-Dupre R (1992) Runaway electron mechanism of air breakdown and preconditioning during a thunderstorm. Phys Lett A 165:463–468\nGurevich AV, Zybin KP, Roussel-Dupre RA (1999) Lightning initiation by simultaneous effect of runaway breakdown and cosmic ray showers. Phys Lett A 254:79–87\nGurevich AV, Duncan LM, Medvedev YuV, Zybin KP (2002) Radio emission due to simultaneous effect of runaway breakdown and extensive atmospheric showers. Phys Lett A 301:320–326\nGurevich AV, Duncan LM, Karashtin AN, Zybin KP (2003) Radio emission of lightning initiation. Phys Lett A 312:228–237\nGurevich AV, Roussel-Dupre R, Zybin KP, Milikh GM (2012) Comment on “Low-energy electron production by relativistic runway electron avalanches in air” by J. R. Dwyer and L. P. Babich. J Geophys Res 117:A04302. doi:10.1029\u002F2011JA017431\nHaddad MA, Rakov VA, Cummer SA (2012) New measurements of lightning electric fields in Florida: waveform characteristics, interaction with the ionosphere, and peak current estimates. J Geophys Res 117:D10101. doi:10.1029\u002F2011JD017196\nHill JD, Uman MA, Jordan DM (2011) High-speed video observations of a lightning stepped leader. J Geophys Res 116:D16117. doi:10.1029\u002F2011JD015818\nInan US, Cummer SA, Marshall RA (2010) A survey of ELF and VLF research of lightning-ionosphere interactions and causative discharges. J Geophys Res 115:A00E36, doi:10.1029\u002F2009JA014775\nJayakumar V, Rakov VA, Miki M, Uman MA, Schnetzer GH, Rambo KJ (2006) Estimation of input energy in rocket-triggered lightning. Geophys Res Lett 33:L05702. doi:10.1029\u002F2005GL025141\nKrehbiel PR, Riousset JA, Pasko VP, Thomas RJ, Rison W, Stanley MA, Edens HE (2008) Upward electrical discharges from thunderstorms. Nature Geosci 1:233–237. doi:10.1038\u002Fngeo162\nKrider EP, Dawson GA, Uman MA (1968) The peak power and energy dissipation in a single–stroke lightning flash. J Geophys Res 73:3335–3339\nLarigaldie S, Roussaud A, Jecko B (1992) Mechanisms of high-current pulses in lightning and long-spark. J Appl Phys 72(5):1729–1739\nLebedev VB, Feldman GG, Gorin BN, Shcherbakov Yu V, Syssoev VS, Rakov VA, Uman MA, Olsen RC (2007) Test of the image converter camera complex for research of discharges in long air gaps and lightning. In Proceedings of the 13th international conference on atmospheric electricity, Beijing, China, August 13–17, 2007, pp. 509–512\nLoeb LB (1966) The mechanisms of stepped and dart leaders in cloud-to-ground lightning strokes. J Geophys Res 71:4711–4721\nLu G et al (2011) Lightning development associated with two negative gigantic jets. Geophys Res Lett 38:L12801. doi:10.1029\u002F2011GL047662\nMalan DJ, Schonland BFJ (1951) The electrical processes in the intervals between the strokes of a lightning discharge. Proc Roy Soc (Lond) A206:145–163\nMallick S, Rakov VA, Dwyer JR (2012) A study of X-ray emissions from thunderstorms with emphasis on subsequent strokes in natural lightning. J Geophys Res 117:D16107. doi:10.1029\u002F2012JD017555\nMoss G, Pasko VP, Liu N, Veronis G (2006) Monte Carlo model for analysis of thermal runaway electrons in streamer tips in transient luminous events and streamer zones of lightning leaders. J Geophys Res 111:A02307. doi:10.1029\u002F2005JA011350\nNag A, Rakov VA (2008) Pulse trains characteristic of preliminary breakdown in cloud-to-ground lightning that are not followed by return stroke pulses. J Geophys Res 113:D01102. doi:10.1029\u002F2007JD008489\nNag A, Rakov VA (2009) Some inferences on the role of lower positive charge region in facilitating different types of lightning. Geophys Res Lett 36:L05815. doi:10.1029\u002F2008GL036783\nNag A, Rakov VA (2010a) Compact intracloud lightning discharges: 1. Mechanism of electromagnetic radiation and modeling. J Geophys Res 115:D20102. doi:10.1029\u002F2010JD014235\nNag A, Rakov VA (2010b) Compact intracloud lightning discharges: 2. Estimation of electrical parameters. J Geophys Res 115:D20103. doi:10.1029\u002F2010JD014237\nNag A, Rakov VA, Tsalikis D, Cramer JA (2010) On phenomenology of compact intracloud lightning discharges. J Geophys Res 115:D14115. doi:10.1029\u002F2009JD012957\nNguyen MD, Michnowski S (1996) On the initiation of lightning discharge in a cloud 2. The lightning initiation on precipitation particles. J Geophys Res 101:26675–26680\nPaxton AH, Gardner RL, Baker L (1986) Lightning return stroke: a numerical calculation of the optical radiation. Phys Fluids 29:2736–2741\nPaxton AH, Baker L, Gardner RL (1987) Reply to comments of Hill. Phys Fluids 30:2586–2587\nPhelps CT (1974) Positive streamers system intensification and its possible role in lightning initiation. J Atmos Terr Phys 36:103–111\nPierce ET (1958) Some topics in atmospheric electricity. In: Smith LG (ed) Recent advances in atmospheric electricity. Pergamon, New York, pp 5–16\nQie X, Jiang R, Wang C, Yang J, Wang J, Liu D (2011) Simultaneously measured current, luminosity, and electric field pulses in a rocket-triggered lightning flash. J Geophys Res 116:D10102. doi:10.1029\u002F2010JD015331\nRakov VA (1998) Some inferences on the propagation mechanisms of dart leaders and return strokes. J Geophys Res 103:1879–1887\nRakov VA, Uman MA (2003) Lightning: physics and effects. Cambridge University Press, 687 p\nRakov VA (2006) Initiation of lightning in thunderclouds. In Sergeev AM (ed) Topical problems of nonlinear wave physics. Proceedings SPIE, Vol. 5975, pp 362–373\nRakov VA, Uman MA (1990) Waveforms of first and subsequent leaders in negative lightning flashes. J Geophys Res 95(D10):16561–16577. doi:10.1029\u002FJD095iD10p16561\nRakov VA, Uman MA, Jordan DM, Priore CA III (1990) Ratio of leader to return stroke field change for first and subsequent lightning strokes. J Geophys Res 95(16):579–587\nRakov VA, Thottappillil R, Uman MA, Barker PP (1995) Mechanism of the lightning M component. J Geophys Res 100:25701–25710\nRakov VA, Uman MA, Rambo KJ, Fernandez MI, Fisher RJ, Schnetzer GH, Thottappillil R, Eybert-Berard A, Berlandis JP, Lalande P, Bonamy A, Laroche P, Bondiou-Clergerie A (1998) New insights into lightning processes gained from triggered-lightning experiments in Florida and Alabama. J Geophys Res 103:14117–14130\nRao M, Bhattacharya H (1966) Lateral corona currents from the return stroke channel and slow field change after the return stroke in a lightning discharge. J Geophys Res 71:2811–2814\nSaleh Z, Dwyer J, Howard J, Uman M, Bakhtiari M, Concha D, Stapleton M, Hill D, Biagi C, Rassoul H (2009) Properties of the X-ray emission from rocket-triggered lightning as measured by the Thunderstorm Energetic Radiation Array (TERA). J Geophys Res 114:D17210. doi:10.1029\u002F2008JD011618\nSolomon R, Schroeder V, Baker MB (2001) Lightning initiation: conventional and runaway-breakdown hypotheses. 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