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Journal of Medicine and Pharmacy","Tạp chí Y Dược học Cần Thơ",{"EN":487,"VI":488},"\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":490},"wcQ1uqwAAAAJ","2023-05-30T08:17:21.868+00:00",[],[494],{"id":495,"createTime":28,"updateTime":28,"relativeEntities":496,"slug":28,"properties":497,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":507,"parentIds":508,"statistic":28},"6413896b-eca9-442b-a73f-182a58a0ce40",[],{"title":498,"address":501,"country":504,"abbreviation":505},{"EN":499,"VI":500},"Can Tho University of Medicine and Pharmacy","Trường Đại học Y Dược Cần Thơ",{"EN":502,"VI":503},"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":15},{"VOID":506},"ctump","http:\u002F\u002Fwww.ctump.edu.vn\u002F",[],[],"https:\u002F\u002Ftapchi.ctump.edu.vn\u002Findex.php\u002Fctump",{"impactFactor":32,"impactFactorByYear":512,"i10Index":32,"i10IndexLast5Year":32,"totalPublication":514,"totalPublicationByYear":515,"totalCitation":520,"totalCitationByYear":521,"totalCitationPerPublication":108,"totalCitationPerPublicationByYear":523,"hindexLast5Year":45,"hindex":45},{"2022":513,"2023":111,"2024":106},0.01,1556,{"2020":47,"2021":516,"2022":517,"2023":518,"2024":519,"2025":122},57,306,801,358,161,{"2021":146,"2022":280,"2023":522},99,{"2021":524,"2022":318,"2023":104},0.23,{"impactFactor":28,"impactFactorByYear":28,"i10Index":123,"i10IndexLast5Year":123,"totalPublication":526,"totalPublicationByYear":527,"totalCitation":526,"totalCitationByYear":528,"totalCitationPerPublication":40,"totalCitationPerPublicationByYear":531,"hindexLast5Year":49,"hindex":49},476,{"0":205,"2019":123,"2021":139,"2022":459,"2023":451,"2024":357,"2025":49,"2026":48},{"2021":42,"2022":123,"2023":161,"2024":529,"2025":360,"2026":530},136,83,{"2021":105,"2022":513,"2023":532,"2024":127,"2025":533,"2026":534},0.62,25.43,13.83,{"id":536,"createTime":537,"updateTime":382,"relativeEntities":538,"slug":539,"properties":540,"entityType":25,"verifyStatus":26,"verifyTime":28,"verifyNote":28,"languages":552,"translateLanguages":28,"viewCount":133,"subjectFields":553,"manageAffiliations":554,"indexDatabases":555,"url":556,"thumbnailPath":557,"statistic":558,"gsStatistic":594,"type":55,"analyzePriority":28},"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":541,"issn":542,"title":544,"introduce":547,"gsId":550},{"VOID":15},{"VOID":543},"25252445",{"EN":545,"VI":546},"VNU Journal of Foreign Studies","Tạp chí Nghiên cứu nước ngoài",{"EN":548,"VI":549},"{\"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. 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Landslides are a ubiquitous hazard in terrestrial environments with slopes, incurring human fatalities in urban settlements, along transport corridors and at sites of rural industry. Assessment of landslide risk requires high-quality landslide databases. Recently, global landslide databases have shown the extent to which landslides impact on society and identified areas most at risk. Previous global analysis has focused on rainfall-triggered landslides over short ∼ 5-year observation periods. This paper presents spatiotemporal analysis of a global dataset of fatal non-seismic landslides, covering the period from January 2004 to December 2016. The data show that in total 55 997 people were killed in 4862 distinct landslide events. The spatial distribution of landslides is heterogeneous, with Asia representing the dominant geographical area. There are high levels of interannual variation in the occurrence of landslides. Although more active years coincide with recognised patterns of regional rainfall driven by climate anomalies, climate modes (such as El Niño–Southern Oscillation) cannot yet be related to landsliding, requiring a landslide dataset of 30+ years. Our analysis demonstrates that landslide occurrence triggered by human activity is increasing, in particular in relation to construction, illegal mining and hill cutting. This supports notions that human disturbance may be more detrimental to future landslide incidence than climate.\u003C\u002Fjats:p>","\u003Cjats:p>Tóm tắt. Lở đất là một mối nguy hiểm phổ biến trong các môi trường trên cạn có độ dốc, gây ra cái chết cho con người tại các khu định cư đô thị, trên các hành lang giao thông và tại các địa điểm công nghiệp nông thôn. Đánh giá rủi ro lở đất cần có cơ sở dữ liệu lở đất chất lượng cao. Gần đây, các cơ sở dữ liệu lở đất toàn cầu đã chỉ ra mức độ mà lở đất ảnh hưởng đến xã hội và xác định những khu vực có nguy cơ cao nhất. Phân tích toàn cầu trước đây chủ yếu tập trung vào các lở đất do mưa gây ra trong các khoảng thời gian quan sát ngắn khoảng 5 năm. Bài báo này trình bày phân tích không gian-thời gian của một tập dữ liệu toàn cầu về các lở đất không do động đất có gây chết người, bao gồm khoảng thời gian từ tháng 1 năm 2004 đến tháng 12 năm 2016. Dữ liệu cho thấy tổng cộng 55.997 người đã thiệt mạng trong 4.862 sự kiện lở đất khác nhau. Sự phân bố không gian của các lở đất là không đồng nhất, với châu Á là khu vực địa lý chiếm ưu thế. Có sự biến động giữa các năm cao trong việc xảy ra lở đất. Mặc dù những năm hoạt động cao hơn trùng khớp với các kiểu mưa khu vực do các bất thường khí hậu, nhưng các chế độ khí hậu (như Dao động Nam phương El Niño) chưa thể liên kết được với việc lở đất, yêu cầu một tập dữ liệu về lở đất trong thời gian 30 năm trở lên. Phân tích của chúng tôi cho thấy rằng sự xảy ra của lở đất được kích hoạt bởi hoạt động của con người đang gia tăng, đặc biệt liên quan đến xây dựng, khai thác trái phép và cắt đất đồi. Điều này hỗ trợ cho quan điểm rằng sự can thiệp của con người có thể gây hại nhiều hơn cho sự phát sinh lở đất trong tương lai so với khí hậu.\u003C\u002Fjats:p>",{"EN":956,"VI":957},"Global fatal landslide occurrence from 2004 to 2016","Sự xảy ra của lở đất gây chết người trên toàn cầu từ năm 2004 đến 2016",{"VI":959},"",{"VOID":961},"10.5194\u002Fnhess-18-2161-2018","PUBLICATION","Auto Verify",[31],[30],"https:\u002F\u002Fnhess.copernicus.org\u002Farticles\u002F18\u002F2161\u002F2018\u002F",[968,987],{"id":969,"sortIndex":32,"researcher":28,"roles":970,"affiliations":971,"properties":980,"displayName":984,"givenName":28,"familyName":28},"0709f338-4880-42f8-8e90-0b6f3f4ef8af",[],[972],{"id":973,"sortIndex":32,"affiliation":974,"properties":28},"0ca34e73-0137-49da-9be6-7bf18239e62e",{"id":973,"createTime":28,"updateTime":28,"relativeEntities":975,"slug":28,"properties":976,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":979,"statistic":28},[],{"title":977},{"VI":978},"Department of Geography, University of Sheffield, Sheffield S10 2TN, UK",[],{"orcid":981,"title":983,"openalex":985},{"VOID":982},"https:\u002F\u002Forcid.org\u002F0000-0002-5611-1768",{"EN":984},"Melanie Froude",{"VOID":986},"A5022982987",{"id":988,"sortIndex":40,"researcher":28,"roles":989,"affiliations":990,"properties":997,"displayName":1001,"givenName":28,"familyName":28},"41602509-26eb-41f8-93b0-ef4c0b27eccc",[],[991],{"id":973,"sortIndex":32,"affiliation":992,"properties":28},{"id":973,"createTime":28,"updateTime":28,"relativeEntities":993,"slug":28,"properties":994,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":996,"statistic":28},[],{"title":995},{"VI":978},[],{"orcid":998,"title":1000,"openalex":1002},{"VOID":999},"https:\u002F\u002Forcid.org\u002F0000-0002-3061-6282",{"EN":1001},"David N. 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J. Disaster Risk Sci., 8, 498–502, https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs13753-017-0139-4, 2017.",{"doi":1068},"10.1007\u002Fs13753-017-0139-4",{"id":28,"text":1070,"url":28,"identifiers":1071},"Alexander, D.: Urban landslides, Prog. Phys. Geog.-Earth and Environment, 13, 157–189, https:\u002F\u002Fdoi.org\u002F10.1177\u002F030913338901300201, 1989.",{"doi":1072},"10.1177\u002F030913338901300201",{"id":28,"text":1074,"url":28,"identifiers":1075},"Allen, S. K., Rastner, P., Arora, M., Huggel, C., and Stoffel, M.: Lake outburst and debris flow disaster at Kedarnath, June 2013: hydrometeorological triggering and topographic predisposition, Landslides, 13, 1479–1491, https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs10346-015-0584-3, 2016.",{"doi":1076},"10.1007\u002Fs10346-015-0584-3",{"id":28,"text":1078,"url":28,"identifiers":1079},"Anderson, M. B.: Metropolitan areas and disaster vulnerability: a consideration for developing countries, in: Environmental Management and Urban Vulnerability, edited by: Kreimer, A. and Munasinghe, M., World Bank discussion paper #18, World Bank, Washington DC, 1992.",{},{"id":28,"text":1081,"url":28,"identifiers":1082},"Anderson, M. G. and Holcombe, E.: Community-Based Landslide Risk Reduction: Managing Disasters in Small Steps, World Bank Publications, 2013.",{"doi":1083},"10.1596\u002F978-0-8213-9456-4",{"id":28,"text":1085,"url":28,"identifiers":1086},"Anderson, M. G. and Holcombe, E. A.: Sustainable Landslide Risk Reduction in Poorer Countries, Proceedings of the Institution of Civil Engineers-Engineering Sustainability, 159, 23–30, 2006.",{"doi":1087},"10.1680\u002Fensu.2006.159.1.23",{"id":28,"text":1089,"url":28,"identifiers":1090},"Anderson, G. and Ge, Y.: Do Economic Reforms Accelerate Urban Growth? The Case of China, Urban Stud., 41, 2197–2210, https:\u002F\u002Fdoi.org\u002F10.1080\u002F0042098042000268410, 2004.",{"doi":1091},"10.1080\u002F0042098042000268410",{"id":28,"text":1093,"url":28,"identifiers":1094},"Anhorn, J., Lennartz, T., and Nüsser, M., Rapid urban growth and earthquake risk in Musikot, mid-western hills, Nepal, Erdkunde, 69, 307–325, 2015.",{"doi":1095},"10.3112\u002Ferdkunde.2015.04.02",{"id":28,"text":1097,"url":28,"identifiers":1098},"Ashok, K. and Saji, N. H.: On the impacts of ENSO and Indian Ocean dipole events on sub-regional Indian summer monsoon rainfall, Nat. Hazards, 42, 273–285, https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs11069-006-9091-0, 2007.",{"doi":1099},"10.1007\u002Fs11069-006-9091-0",{"id":28,"text":1101,"url":28,"identifiers":1102},"Barnard, P. L., Owen, L. A., Sharma, M. C., and Finkel, R. 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K.: Information retrieval and machine learning: Supporting technologies for web mining research and practice, Webology, 5, available at: http:\u002F\u002Fwww.webology.org\u002F2008\u002Fv5n2\u002Fa55.html (last access: 15 February 2018), 2008.",{},{"id":28,"text":1112,"url":28,"identifiers":1113},"Borgatti, L. and Soldati, M.: Landslides as a geomorphological proxy for climate change: A record from the Dolomites (northern Italy), Geomorphology, 120, 56–64, https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.geomorph.2009.09.015, 2010.",{"doi":1114},"10.1016\u002Fj.geomorph.2009.09.015",{"id":28,"text":1116,"url":28,"identifiers":1117},"Camargo, S. J. and Sobel, A. H.: Western North Pacific Tropical Cyclone Intensity and ENSO, J. 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Bài báo này xem xét sự phát triển qua thời gian lịch sử của ý nghĩa và cách sử dụng thuật ngữ \"khả năng phục hồi\". Mục tiêu là làm sâu sắc thêm sự hiểu biết của chúng ta về cách thuật ngữ này được áp dụng trong giảm thiểu rủi ro thiên tai và giải quyết một số mâu thuẫn và tranh cãi đã phát sinh khi nó được sử dụng. Bài báo lần theo sự phát triển của khả năng phục hồi qua các lĩnh vực khoa học, nhân văn và pháp lý, chính trị. Nó xem xét cách mà cơ học đã chuyển giao thuật ngữ này sang sinh thái học và tâm lý học, và từ đó được các nghiên cứu xã hội và khoa học bền vững tiếp nhận. Như một số tác giả đã lưu ý, với tư cách là một khái niệm, khả năng phục hồi liên quan đến một số mâu thuẫn hoặc mâu thuẫn nghiêm trọng, chẳng hạn như giữa sự ổn định và động lực, hoặc giữa trạng thái cân bằng động (nội môi) và sự tiến hóa. Hơn nữa, mặc dù khái niệm khả năng phục hồi hoạt động khá tốt trong khuôn khổ của lý thuyết hệ thống tổng quát, nhưng trong những tình huống mà việc hình thành hệ thống ngăn cản thay vì thúc đẩy sự giải thích, một sự diễn giải khác về thuật ngữ là cần thiết. Điều này có thể xảy ra trong giảm thiểu rủi ro thiên tai, điều này liên quan đến việc chuyển hóa thay vì bảo tồn \"trạng thái của hệ thống\". Bài viết kết luận rằng sự quan niệm hiện đại về khả năng phục hồi có lợi từ một lịch sử phong phú về các ý nghĩa và ứng dụng, nhưng việc đọc quá nhiều vào thuật ngữ như một mô hình và một khuôn khổ thì có thể nguy hiểm - hoặc ít nhất là có thể mang lại sự thất vọng.","\u003Cjats:p>Abstract. This paper examines the development over historical time of the meaning and uses of the term resilience. The objective is to deepen our understanding of how the term came to be adopted in disaster risk reduction and resolve some of the conflicts and controversies that have arisen when it has been used. The paper traces the development of resilience through the sciences, humanities, and legal and political spheres. It considers how mechanics passed the word to ecology and psychology, and how from there it was adopted by social research and sustainability science. As other authors have noted, as a concept, resilience involves some potentially serious conflicts or contradictions, for example between stability and dynamism, or between dynamic equilibrium (homeostasis) and evolution. Moreover, although the resilience concept works quite well within the confines of general systems theory, in situations in which a systems formulation inhibits rather than fosters explanation, a different interpretation of the term is warranted. This may be the case for disaster risk reduction, which involves transformation rather than preservation of the \"state of the system\". The article concludes that the modern conception of resilience derives benefit from a rich history of meanings and applications, but that it is dangerous – or at least potentially disappointing – to read to much into the term as a model and a paradigm.\u003C\u002Fjats:p>",{"EN":1526,"VI":1527},"Resilience and disaster risk reduction: an etymological journey","Khả năng phục hồi và giảm thiểu rủi ro thiên tai: một hành trình ngữ nghĩa",{"VI":959},{"VOID":1530},"10.5194\u002Fnhess-13-2707-2013",[31],[30],"https:\u002F\u002Fnhess.copernicus.org\u002Farticles\u002F13\u002F2707\u002F2013\u002F",[1535],{"id":1536,"sortIndex":32,"researcher":28,"roles":1537,"affiliations":1538,"properties":1547,"displayName":1551,"givenName":28,"familyName":28},"7ada2810-ab6f-443b-a26a-0f8c1ca99937",[],[1539],{"id":1540,"sortIndex":32,"affiliation":1541,"properties":28},"a1540f79-0a30-424a-84a0-72e376e0407a",{"id":1540,"createTime":28,"updateTime":28,"relativeEntities":1542,"slug":28,"properties":1543,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1546,"statistic":28},[],{"title":1544},{"VI":1545},"Institute for Risk and Disaster Reduction, University College London, London, UK",[],{"orcid":1548,"title":1550,"openalex":1552},{"VOID":1549},"https:\u002F\u002Forcid.org\u002F0000-0003-1235-3658",{"EN":1551},"David Alexander",{"VOID":1553},"A5009682617",{"url":28,"publisher":1555,"properties":1593},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1556,"slug":872,"properties":1557,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1562,"manageAffiliations":1567,"indexDatabases":1578,"url":936,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":1558,"eissn":1559,"issn":1560,"title":1561},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[1563],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":1564,"label":1565,"description":1566,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},[1568,1573],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":1569,"slug":28,"properties":1570,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1572,"statistic":28},[],{"title":1571},{"EN":898},[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":1574,"slug":28,"properties":1575,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1577,"statistic":28},[],{"title":1576},{"EN":905},[],[1579,1586],{"id":909,"indexDatabase":1580,"url":921,"indexYears":28,"academicFieldIds":1585,"indexDatabaseRanking":28},{"id":911,"createTime":28,"updateTime":28,"relativeEntities":1581,"label":1582,"description":1583,"key":918,"publicationTags":1584,"standard":28},[],{"EN":914,"VI":914},{"EN":916,"VI":917},[920,813],[816,923,924],{"id":926,"indexDatabase":1587,"url":932,"indexYears":933,"academicFieldIds":1592,"indexDatabaseRanking":935},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1588,"label":1589,"description":1590,"key":781,"publicationTags":1591,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[787],{"issue":1594,"pages":1596,"volume":1598},{"VOID":1595},"11",{"VOID":1597},"2707-2716",{"VOID":1599},"13",948,{"total":1600,"publishYear":28,"statisticByYear":1602},{"2013":42,"2014":278,"2015":279,"2016":281,"2017":155,"2018":333,"2019":1603,"2020":1604,"2021":153,"2022":354,"2023":1605,"2024":564},121,113,103,[],[1608,1612,1615,1618,1622,1625,1629,1633,1636,1640,1644,1648,1651,1655,1658,1661,1664,1668,1672,1675,1679,1683,1687,1690,1693,1696,1700,1704,1707,1711,1714,1717,1721,1725,1729,1733,1737,1741,1745,1748,1752,1756,1760,1764,1767,1770,1774,1778,1782,1786,1789,1793,1796,1799,1803,1806,1809,1813,1817,1821,1825,1828,1831,1834,1837,1840,1844,1848,1851,1854],{"id":28,"text":1609,"url":28,"identifiers":1610},"Adger, W. 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Hazards, 53, 21–41, 2008.",{"doi":1857},"10.1007\u002Fs11069-009-9407-y",{"id":1859,"createTime":1860,"updateTime":1861,"relativeEntities":1862,"slug":1863,"properties":1864,"entityType":962,"verifyStatus":26,"verifyTime":1878,"verifyNote":963,"languages":1879,"translateLanguages":1880,"viewCount":32,"primaryUrl":1881,"fullTextUrl":28,"authors":1882,"publicationType":1004,"publisherRelationship":1955,"citationCount":2001,"citationInfo":2002,"publishDate":28,"publishYear":28,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":2004,"openAccess":28,"references":2005,"isForceReanalyzing":1510},"f8610902-4eb3-4ab8-b281-311f0a640fbe","2024-09-28T15:25:28.999+00:00","2025-02-21T07:41:21.548+00:00",[],"Flood-risk-assessment-and-associated-uncertainty",{"openalex":1865,"mag":1867,"abstract":1869,"title":1872,"keywords":1875,"doi":1876},{"VOID":1866},"W2171174555",{"VOID":1868},"2171174555",{"EN":1870,"VI":1871},"\u003Cjats:p>Abstract. Flood disaster mitigation strategies should be based on a comprehensive assessment of the flood risk combined with a thorough investigation of the uncertainties associated with the risk assessment procedure. Within the \"German Research Network of Natural Disasters\" (DFNK) the working group \"Flood Risk Analysis\" investigated the flood process chain from precipitation, runoff generation and concentration in the catchment, flood routing in the river network, possible failure of flood protection measures, inundation to economic damage. The working group represented each of these processes by deterministic, spatially distributed models at different scales. While these models provide the necessary understanding of the flood process chain, they are not suitable for risk and uncertainty analyses due to their complex nature and high CPU-time demand. We have therefore developed a stochastic flood risk model consisting of simplified model components associated with the components of the process chain. We parameterised these model components based on the results of the complex deterministic models and used them for the risk and uncertainty analysis in a Monte Carlo framework. The Monte Carlo framework is hierarchically structured in two layers representing two different sources of uncertainty, aleatory uncertainty (due to natural and anthropogenic variability) and epistemic uncertainty (due to incomplete knowledge of the system). The model allows us to calculate probabilities of occurrence for events of different magnitudes along with the expected economic damage in a target area in the first layer of the Monte Carlo framework, i.e. to assess the economic risks, and to derive uncertainty bounds associated with these risks in the second layer. It is also possible to identify the contributions of individual sources of uncertainty to the overall uncertainty. It could be shown that the uncertainty caused by epistemic sources significantly alters the results obtained with aleatory uncertainty alone. The model was applied to reaches of the river Rhine downstream of Cologne.\n                    \u003C\u002Fjats:p>","\u003Cjats:p>Tóm tắt. Các chiến lược giảm thiểu thiên tai lũ nên dựa trên một đánh giá toàn diện về rủi ro lũ kết hợp với một cuộc điều tra kỹ lưỡng về các bất định liên quan đến quy trình đánh giá rủi ro. Trong \"Mạng Nghiên cứu Thảm họa Thiên nhiên Đức\" (DFNK), nhóm công tác \"Phân tích Rủi ro Lũ\" đã nghiên cứu chuỗi quy trình lũ từ lượng mưa, việc phát sinh và tập trung dòng chảy trong lưu vực, định hướng lũ trong mạng lưới sông, khả năng thất bại của các biện pháp bảo vệ lũ, ngập lụt cho đến thiệt hại kinh tế. Nhóm công tác đại diện cho từng quy trình này bằng các mô hình xác định, phân bố không gian ở các quy mô khác nhau. Mặc dù các mô hình này cung cấp hiểu biết cần thiết về chuỗi quy trình lũ, nhưng chúng không phù hợp cho các phân tích rủi ro và bất định do bản chất phức tạp và yêu cầu thời gian CPU cao của chúng. Do đó, chúng tôi đã phát triển một mô hình rủi ro lũ ngẫu nhiên bao gồm các thành phần mô hình đơn giản hóa liên quan đến các thành phần của chuỗi quy trình. Chúng tôi đã định tham số cho các thành phần mô hình này dựa trên kết quả của các mô hình xác định phức tạp và sử dụng chúng cho phân tích rủi ro và bất định trong khuôn khổ Monte Carlo. Khuôn khổ Monte Carlo được cấu trúc theo cách phân cấp thành hai lớp đại diện cho hai nguồn bất định khác nhau, bất định ngẫu nhiên (do biến đổi tự nhiên và nhân tạo) và bất định tri thức (do hiểu biết không đầy đủ về hệ thống). Mô hình cho phép chúng tôi tính toán xác suất xảy ra cho các sự kiện với độ lớn khác nhau cùng với thiệt hại kinh tế dự kiến trong một khu vực mục tiêu ở lớp đầu tiên của khuôn khổ Monte Carlo, tức là đánh giá các rủi ro kinh tế, và đưa ra các giới hạn bất định liên quan đến những rủi ro này ở lớp thứ hai. Cũng có thể xác định các đóng góp của các nguồn bất định riêng lẻ vào bất định tổng thể. Có thể thấy rằng bất định do các nguồn tri thức gây ra làm thay đổi đáng kể kết quả thu được chỉ với bất định ngẫu nhiên. Mô hình đã được áp dụng cho những đoạn sông Rhine hạ lưu Cologne.\u003C\u002Fjats:p>",{"EN":1873,"VI":1874},"Flood risk assessment and associated uncertainty","Đánh giá rủi ro lũ và các bất định liên quan",{"VI":959},{"VOID":1877},"10.5194\u002Fnhess-4-295-2004","2024-09-28T15:25:28.998+00:00",[31],[30],"https:\u002F\u002Fnhess.copernicus.org\u002Farticles\u002F4\u002F295\u002F2004\u002F",[1883,1902,1919,1936],{"id":1884,"sortIndex":32,"researcher":28,"roles":1885,"affiliations":1886,"properties":1895,"displayName":1899,"givenName":28,"familyName":28},"f84eed7f-aebc-4a7c-ae0b-b8ffd490d3ea",[],[1887],{"id":1888,"sortIndex":32,"affiliation":1889,"properties":28},"61fa551f-1be1-45f3-9302-a9a22f1f2a52",{"id":1888,"createTime":28,"updateTime":28,"relativeEntities":1890,"slug":28,"properties":1891,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1894,"statistic":28},[],{"title":1892},{"EN":1893},"GeoForschungsZentrum Potsdam (GFZ), Section 5.4 Engineering Hydrology, Telegrafenberg, 14473 Potsdam, Germany",[],{"orcid":1896,"title":1898,"openalex":1900},{"VOID":1897},"https:\u002F\u002Forcid.org\u002F0000-0002-8852-652X",{"EN":1899},"Heiko Apel",{"VOID":1901},"A5068085970",{"id":1903,"sortIndex":40,"researcher":28,"roles":1904,"affiliations":1905,"properties":1912,"displayName":1916,"givenName":28,"familyName":28},"320ebe88-d5e5-462e-b3fe-8e4fa43d0d17",[],[1906],{"id":1888,"sortIndex":32,"affiliation":1907,"properties":28},{"id":1888,"createTime":28,"updateTime":28,"relativeEntities":1908,"slug":28,"properties":1909,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1911,"statistic":28},[],{"title":1910},{"EN":1893},[],{"orcid":1913,"title":1915,"openalex":1917},{"VOID":1914},"https:\u002F\u002Forcid.org\u002F0000-0001-7068-2615",{"EN":1916},"Annegret H. Thieken",{"VOID":1918},"A5042795778",{"id":1920,"sortIndex":123,"researcher":28,"roles":1921,"affiliations":1922,"properties":1929,"displayName":1933,"givenName":28,"familyName":28},"baccc4c6-ad2f-4656-a850-278bbe808671",[],[1923],{"id":1888,"sortIndex":32,"affiliation":1924,"properties":28},{"id":1888,"createTime":28,"updateTime":28,"relativeEntities":1925,"slug":28,"properties":1926,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1928,"statistic":28},[],{"title":1927},{"EN":1893},[],{"orcid":1930,"title":1932,"openalex":1934},{"VOID":1931},"https:\u002F\u002Forcid.org\u002F0000-0002-5992-1440",{"EN":1933},"Bruno Merz",{"VOID":1935},"A5045067771",{"id":1937,"sortIndex":42,"researcher":28,"roles":1938,"affiliations":1939,"properties":1948,"displayName":1952,"givenName":28,"familyName":28},"0549b20f-ac29-4088-97a4-0e472cb36a5b",[],[1940],{"id":1941,"sortIndex":32,"affiliation":1942,"properties":28},"f3a0be71-b1d4-46b2-8f84-f942d8169757",{"id":1941,"createTime":28,"updateTime":28,"relativeEntities":1943,"slug":28,"properties":1944,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1947,"statistic":28},[],{"title":1945},{"EN":1946},"Institute of Hydraulics, Hydrology and Water Resources Management, Vienna University of Technology, Karlsplatz 13, A–1040 Wien, Austria",[],{"orcid":1949,"title":1951,"openalex":1953},{"VOID":1950},"https:\u002F\u002Forcid.org\u002F0000-0003-2227-8225",{"EN":1952},"Günter Blöschl",{"VOID":1954},"A5015678021",{"url":28,"publisher":1956,"properties":1994},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1957,"slug":872,"properties":1958,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1963,"manageAffiliations":1968,"indexDatabases":1979,"url":936,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":1959,"eissn":1960,"issn":1961,"title":1962},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[1964],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":1965,"label":1966,"description":1967,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},[1969,1974],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":1970,"slug":28,"properties":1971,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1973,"statistic":28},[],{"title":1972},{"EN":898},[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":1975,"slug":28,"properties":1976,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1978,"statistic":28},[],{"title":1977},{"EN":905},[],[1980,1987],{"id":909,"indexDatabase":1981,"url":921,"indexYears":28,"academicFieldIds":1986,"indexDatabaseRanking":28},{"id":911,"createTime":28,"updateTime":28,"relativeEntities":1982,"label":1983,"description":1984,"key":918,"publicationTags":1985,"standard":28},[],{"EN":914,"VI":914},{"EN":916,"VI":917},[920,813],[816,923,924],{"id":926,"indexDatabase":1988,"url":932,"indexYears":933,"academicFieldIds":1993,"indexDatabaseRanking":935},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1989,"label":1990,"description":1991,"key":781,"publicationTags":1992,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[787],{"issue":1995,"pages":1997,"volume":1999},{"VOID":1996},"2",{"VOID":1998},"295-308",{"VOID":2000},"4",478,{"total":2001,"publishYear":28,"statisticByYear":2003},{"2012":131,"2013":148,"2014":133,"2015":141,"2016":352,"2017":140,"2018":278,"2019":201,"2020":140,"2021":133,"2022":150,"2023":139,"2024":146},[],[],{"id":2007,"createTime":2008,"updateTime":2009,"relativeEntities":2010,"slug":2011,"properties":2012,"entityType":962,"verifyStatus":26,"verifyTime":2008,"verifyNote":963,"languages":2026,"translateLanguages":2027,"viewCount":32,"primaryUrl":2028,"fullTextUrl":28,"authors":2029,"publicationType":1004,"publisherRelationship":2049,"citationCount":2094,"citationInfo":2095,"publishDate":28,"publishYear":28,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":2097,"openAccess":28,"references":2098,"isForceReanalyzing":1510},"7fa32b0a-186c-4f3d-90e2-c7841f83c3cd","2024-09-05T23:16:04.081+00:00","2025-02-21T07:42:19.366+00:00",[],"Validation-of-a-social-vulnerability-index-in-context-to-river-floods-in-Germany",{"openalex":2013,"mag":2015,"abstract":2017,"title":2020,"keywords":2023,"doi":2024},{"VOID":2014},"W2117150513",{"VOID":2016},"2117150513",{"EN":2018,"VI":2019},"\u003Cjats:p>Abstract. Social vulnerability indices are a means for generating information about people potentially affected by disasters that are e.g. triggered by river-floods. The purpose behind such an index is in this study the development and the validation of a social vulnerability map of population characteristics towards river-floods covering all counties in Germany. This map is based on a composite index of three main indicators for social vulnerability in Germany – fragility, socio-economic conditions and region. These indicators have been identified by a factor analysis of selected demographic variables obtained from federal statistical offices. Therefore, these indicators can be updated annually based on a reliable data source. The vulnerability patterns detected by the factor analysis are verified by using an independent second data set. The interpretation of the second data set shows that vulnerability is revealed by a real extreme flood event and demonstrates that the patterns of the presumed vulnerability match the observations of a real event. It comprises a survey of flood-affected households in three federal states. By using logistic regression, it is demonstrated that the theoretically presumed indications of vulnerability are correct and that the indicators are valid. It is shown that indeed certain social groups like the elderly, the financially weak or the urban residents are higher risk groups.\n                    \u003C\u002Fjats:p>","\u003Cjats:p>Tóm tắt. Các chỉ số dễ tổn thương xã hội là một phương tiện để tạo ra thông tin về những người có khả năng bị ảnh hưởng bởi các thảm họa do lũ lụt từ sông gây ra. Mục đích của chỉ số này trong nghiên cứu này là phát triển và xác thực bản đồ dễ tổn thương xã hội về các đặc điểm của dân số đối với lũ lụt từ sông, bao gồm tất cả các huyện ở Đức. Bản đồ này dựa trên một chỉ số tổng hợp của ba chỉ số chính cho dễ tổn thương xã hội ở Đức – sự dễ bị tổn thương, tình trạng kinh tế xã hội và khu vực. Các chỉ số này đã được xác định thông qua phân tích nhân tố các biến nhân khẩu học được chọn từ các cơ quan thống kê liên bang. Do đó, các chỉ số này có thể được cập nhật hàng năm dựa trên một nguồn dữ liệu đáng tin cậy. Các mẫu dễ tổn thương được phát hiện qua phân tích nhân tố được xác nhận thông qua việc sử dụng một tập dữ liệu thứ hai độc lập. Việc diễn giải tập dữ liệu thứ hai cho thấy rằng dễ tổn thương được thể hiện qua một sự kiện lũ lụt cực đoan thực tế và chứng minh rằng các mẫu của dễ tổn thương giả định khớp với những quan sát của một sự kiện thực tế. Nó bao gồm một cuộc khảo sát các hộ gia đình bị ảnh hưởng bởi lũ lụt ở ba bang liên bang. Bằng cách sử dụng hồi quy logistic, nghiên cứu đã chứng minh rằng các chỉ số dễ tổn thương lý thuyết được giả định là đúng và các chỉ số là hợp lệ. Đúng là một số nhóm xã hội nhất định như người cao tuổi, những người có thu nhập thấp hoặc cư dân thành phố là những nhóm có nguy cơ cao hơn.\n                    \u003C\u002Fjats:p>",{"EN":2021,"VI":2022},"Validation of a social vulnerability index in context to river-floods in Germany","Xác thực chỉ số dễ tổn thương xã hội trong bối cảnh lũ lụt ở Đức",{"VI":959},{"VOID":2025},"10.5194\u002Fnhess-9-393-2009",[31],[30],"https:\u002F\u002Fnhess.copernicus.org\u002Farticles\u002F9\u002F393\u002F2009\u002F",[2030],{"id":2031,"sortIndex":32,"researcher":28,"roles":2032,"affiliations":2033,"properties":2042,"displayName":2046,"givenName":28,"familyName":28},"d76d52b0-f7af-4bab-85ff-e9c2d34644e1",[],[2034],{"id":2035,"sortIndex":32,"affiliation":2036,"properties":28},"b739fcda-8849-4bf5-9f20-42bc92862dd8",{"id":2035,"createTime":28,"updateTime":28,"relativeEntities":2037,"slug":28,"properties":2038,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2041,"statistic":28},[],{"title":2039},{"VI":2040},"United Nations University, Institute for Environment and Human Security (UNU-EHS), UN Campus, Hermann-Ehlers-Str. 10, 53113 Bonn, Germany",[],{"orcid":2043,"title":2045,"openalex":2047},{"VOID":2044},"https:\u002F\u002Forcid.org\u002F0000-0002-8029-6774",{"EN":2046},"Alexander Fekete",{"VOID":2048},"A5064696750",{"url":28,"publisher":2050,"properties":2088},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":2051,"slug":872,"properties":2052,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":2057,"manageAffiliations":2062,"indexDatabases":2073,"url":936,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":2053,"eissn":2054,"issn":2055,"title":2056},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[2058],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":2059,"label":2060,"description":2061,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},[2063,2068],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":2064,"slug":28,"properties":2065,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2067,"statistic":28},[],{"title":2066},{"EN":898},[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":2069,"slug":28,"properties":2070,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2072,"statistic":28},[],{"title":2071},{"EN":905},[],[2074,2081],{"id":909,"indexDatabase":2075,"url":921,"indexYears":28,"academicFieldIds":2080,"indexDatabaseRanking":28},{"id":911,"createTime":28,"updateTime":28,"relativeEntities":2076,"label":2077,"description":2078,"key":918,"publicationTags":2079,"standard":28},[],{"EN":914,"VI":914},{"EN":916,"VI":917},[920,813],[816,923,924],{"id":926,"indexDatabase":2082,"url":932,"indexYears":933,"academicFieldIds":2087,"indexDatabaseRanking":935},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":2083,"label":2084,"description":2085,"key":781,"publicationTags":2086,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[787],{"issue":2089,"pages":2090,"volume":2092},{"VOID":1996},{"VOID":2091},"393-403",{"VOID":2093},"9",466,{"total":2094,"publishYear":28,"statisticByYear":2096},{"2012":128,"2013":127,"2014":128,"2015":134,"2016":202,"2017":140,"2018":201,"2019":201,"2020":353,"2021":328,"2022":436,"2023":328,"2024":202},[],[2099,2101,2103,2105,2107,2109,2111,2113,2115,2117,2119,2121,2123,2125,2127,2129,2131,2133,2135,2137,2139,2141,2143,2145,2147,2149,2151,2153,2155,2157,2159,2161,2163,2165,2167,2169,2171,2173,2175,2177],{"id":28,"text":959,"url":28,"identifiers":2100},{},{"id":28,"text":959,"url":28,"identifiers":2102},{},{"id":28,"text":959,"url":28,"identifiers":2104},{},{"id":28,"text":959,"url":28,"identifiers":2106},{},{"id":28,"text":959,"url":28,"identifiers":2108},{},{"id":28,"text":959,"url":28,"identifiers":2110},{},{"id":28,"text":959,"url":28,"identifiers":2112},{},{"id":28,"text":959,"url":28,"identifiers":2114},{},{"id":28,"text":959,"url":28,"identifiers":2116},{},{"id":28,"text":959,"url":28,"identifiers":2118},{},{"id":28,"text":959,"url":28,"identifiers":2120},{},{"id":28,"text":959,"url":28,"identifiers":2122},{},{"id":28,"text":959,"url":28,"identifiers":2124},{},{"id":28,"text":959,"url":28,"identifiers":2126},{},{"id":28,"text":959,"url":28,"identifiers":2128},{},{"id":28,"text":959,"url":28,"identifiers":2130},{},{"id":28,"text":959,"url":28,"identifiers":2132},{},{"id":28,"text":959,"url":28,"identifiers":2134},{},{"id":28,"text":959,"url":28,"identifiers":2136},{},{"id":28,"text":959,"url":28,"identifiers":2138},{},{"id":28,"text":959,"url":28,"identifiers":2140},{},{"id":28,"text":959,"url":28,"identifiers":2142},{},{"id":28,"text":959,"url":28,"identifiers":2144},{},{"id":28,"text":959,"url":28,"identifiers":2146},{},{"id":28,"text":959,"url":28,"identifiers":2148},{},{"id":28,"text":959,"url":28,"identifiers":2150},{},{"id":28,"text":959,"url":28,"identifiers":2152},{},{"id":28,"text":959,"url":28,"identifiers":2154},{},{"id":28,"text":959,"url":28,"identifiers":2156},{},{"id":28,"text":959,"url":28,"identifiers":2158},{},{"id":28,"text":959,"url":28,"identifiers":2160},{},{"id":28,"text":959,"url":28,"identifiers":2162},{},{"id":28,"text":959,"url":28,"identifiers":2164},{},{"id":28,"text":959,"url":28,"identifiers":2166},{},{"id":28,"text":959,"url":28,"identifiers":2168},{},{"id":28,"text":959,"url":28,"identifiers":2170},{},{"id":28,"text":959,"url":28,"identifiers":2172},{},{"id":28,"text":959,"url":28,"identifiers":2174},{},{"id":28,"text":959,"url":28,"identifiers":2176},{},{"id":28,"text":959,"url":28,"identifiers":2178},{},{"id":2180,"createTime":2181,"updateTime":2182,"relativeEntities":2183,"slug":2184,"properties":2185,"entityType":962,"verifyStatus":26,"verifyTime":2199,"verifyNote":963,"languages":2200,"translateLanguages":2201,"viewCount":32,"primaryUrl":2202,"fullTextUrl":28,"authors":2203,"publicationType":1004,"publisherRelationship":2268,"citationCount":2313,"citationInfo":2314,"publishDate":28,"publishYear":28,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":2316,"openAccess":28,"references":2317,"isForceReanalyzing":1510},"194b6007-6095-4190-9acc-652c510a9267","2024-09-04T23:36:27.133+00:00","2025-02-21T07:43:18.823+00:00",[],"Estimation-uncertainty-of-direct-monetary-flood-damage-to-buildings",{"openalex":2186,"mag":2188,"abstract":2190,"title":2193,"keywords":2196,"doi":2197},{"VOID":2187},"W2132967462",{"VOID":2189},"2132967462",{"EN":2191,"VI":2192},"\u003Cjats:p>Abstract. Traditional flood design methods are increasingly supplemented or replaced by risk-oriented methods which are based on comprehensive risk analyses. Besides meteorological, hydrological and hydraulic investigations such analyses require the estimation of flood impacts. Flood impact assessments mainly focus on direct economic losses using damage functions which relate property damage to damage-causing factors. Although the flood damage of a building is influenced by many factors, usually only inundation depth and building use are considered as damage-causing factors. In this paper a data set of approximately 4000 damage records is analysed. Each record represents the direct monetary damage to an inundated building. The data set covers nine flood events in Germany from 1978 to 1994. It is shown that the damage data follow a Lognormal distribution with a large variability, even when stratified according to the building use and to water depth categories. Absolute depth-damage functions which relate the total damage to the water depth are not very helpful in explaining the variability of the damage data, because damage is determined by various parameters besides the water depth. Because of this limitation it has to be expected that flood damage assessments are associated with large uncertainties. It is shown that the uncertainty of damage estimates depends on the number of flooded buildings and on the distribution of building use within the flooded area. The results are exemplified by a damage assessment for a rural area in southwest Germany, for which damage estimates and uncertainty bounds are quantified for a 100-year flood event. The estimates are compared to reported flood damages of a severe flood in 1993. Given the enormous uncertainty of flood damage estimates the refinement of flood damage data collection and modelling are major issues for further empirical and methodological improvements.\n                    \u003C\u002Fjats:p>","\u003Cjats:p>Tóm tắt. Các phương pháp thiết kế lũ lụt truyền thống đang ngày càng được bổ sung hoặc thay thế bằng các phương pháp dựa trên rủi ro, vốn dựa trên các phân tích rủi ro toàn diện. Ngoài các cuộc điều tra khí tượng, thủy văn và thủy lực, các phân tích như vậy yêu cầu ước lượng thiệt hại do lũ lụt. Đánh giá thiệt hại do lũ lụt chủ yếu tập trung vào những tổn thất kinh tế trực tiếp bằng cách sử dụng các hàm thiệt hại liên kết thiệt hại tài sản với các yếu tố gây thiệt hại. Mặc dù thiệt hại do lũ lụt của một tòa nhà chịu ảnh hưởng bởi nhiều yếu tố, thông thường chỉ có độ sâu ngập lụt và mục đích sử dụng tòa nhà được coi là các yếu tố gây thiệt hại. Trong bài báo này, một tập dữ liệu gồm khoảng 4000 hồ sơ thiệt hại được phân tích. Mỗi hồ sơ đại diện cho thiệt hại tài chính trực tiếp của một tòa nhà bị ngập. Tập dữ liệu bao gồm chín sự kiện lũ lụt tại Đức từ năm 1978 đến 1994. Kết quả cho thấy dữ liệu thiệt hại tuân theo phân phối Lognormal với sự biến động lớn, ngay cả khi được phân tầng theo mục đích sử dụng tòa nhà và các loại độ sâu nước. Các hàm độ sâu-thiệt hại tuyệt đối liên kết tổng thiệt hại với độ sâu nước không hữu ích trong việc giải thích sự biến động của dữ liệu thiệt hại, vì thiệt hại được xác định bởi nhiều tham số khác bên cạnh độ sâu nước. Do hạn chế này, phải dự đoán rằng việc đánh giá thiệt hại do lũ lụt liên quan đến sự không chắc chắn lớn. Kết quả cho thấy sự không chắc chắn của ước lượng thiệt hại phụ thuộc vào số lượng tòa nhà bị ngập và vào sự phân bố mục đích sử dụng tòa nhà trong khu vực bị ngập. Các kết quả được minh họa bằng một đánh giá thiệt hại cho một khu vực nông thôn ở phía tây nam nước Đức, trong đó ước lượng thiệt hại và phạm vi không chắc chắn được định lượng cho một sự kiện lũ lụt diễn ra trong 100 năm. Các ước lượng này được so sánh với các thiệt hại do lũ lụt được báo cáo trong một trận lũ nghiêm trọng vào năm 1993. Với sự không chắc chắn khổng lồ của các ước lượng về thiệt hại do lũ lụt, việc cải thiện thu thập và mô hình hóa dữ liệu thiệt hại do lũ lụt là những vấn đề chính để cải thiện thêm về thực nghiệm và phương pháp luận.\u003C\u002Fjats:p>",{"EN":2194,"VI":2195},"Estimation uncertainty of direct monetary flood damage to buildings","Sự không chắc chắn trong ước lượng thiệt hại tài chính do lũ lụt trực tiếp đến các công trình xây dựng",{"VI":959},{"VOID":2198},"10.5194\u002Fnhess-4-153-2004","2024-09-04T23:36:27.132+00:00",[31],[30],"https:\u002F\u002Fnhess.copernicus.org\u002Farticles\u002F4\u002F153\u002F2004\u002F",[2204,2220,2237,2251],{"id":2205,"sortIndex":32,"researcher":28,"roles":2206,"affiliations":2207,"properties":2216,"displayName":1933,"givenName":28,"familyName":28},"89dc5c88-c15a-4e7f-b0c8-2a296e33c64c",[],[2208],{"id":2209,"sortIndex":32,"affiliation":2210,"properties":28},"2f517ec5-7a41-496f-9ead-334f2ad3e076",{"id":2209,"createTime":28,"updateTime":28,"relativeEntities":2211,"slug":28,"properties":2212,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2215,"statistic":28},[],{"title":2213},{"EN":2214},"GFZ - German Research Centre for Geosciences - Helmholtz-Centre Potsdam (Telegrafenberg, 14473 Potsdam - Germany)",[],{"orcid":2217,"title":2218,"openalex":2219},{"VOID":1931},{"EN":1933},{"VOID":1935},{"id":2221,"sortIndex":40,"researcher":28,"roles":2222,"affiliations":2223,"properties":2230,"displayName":2234,"givenName":28,"familyName":28},"750fec3d-d864-4d0b-8cac-0a9216632390",[],[2224],{"id":2209,"sortIndex":32,"affiliation":2225,"properties":28},{"id":2209,"createTime":28,"updateTime":28,"relativeEntities":2226,"slug":28,"properties":2227,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2229,"statistic":28},[],{"title":2228},{"EN":2214},[],{"orcid":2231,"title":2233,"openalex":2235},{"VOID":2232},"https:\u002F\u002Forcid.org\u002F0000-0001-6274-3625",{"EN":2234},"Heidi Kreibich",{"VOID":2236},"A5006100138",{"id":2238,"sortIndex":123,"researcher":28,"roles":2239,"affiliations":2240,"properties":2247,"displayName":1916,"givenName":28,"familyName":28},"f7c2f158-31be-413a-9731-46241edecfc5",[],[2241],{"id":2209,"sortIndex":32,"affiliation":2242,"properties":28},{"id":2209,"createTime":28,"updateTime":28,"relativeEntities":2243,"slug":28,"properties":2244,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2246,"statistic":28},[],{"title":2245},{"EN":2214},[],{"orcid":2248,"title":2249,"openalex":2250},{"VOID":1914},{"EN":1916},{"VOID":1918},{"id":2252,"sortIndex":42,"researcher":28,"roles":2253,"affiliations":2254,"properties":2263,"displayName":2265,"givenName":28,"familyName":28},"f2677a17-0bf9-48ab-a685-ede30400558e",[],[2255],{"id":2256,"sortIndex":32,"affiliation":2257,"properties":28},"b8197895-ae36-4d73-9f6a-17ee0ae43485",{"id":2256,"createTime":28,"updateTime":28,"relativeEntities":2258,"slug":28,"properties":2259,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2262,"statistic":28},[],{"title":2260},{"EN":2261},"Bayerisches Landesamt für Wasserwirtschaft (Germany)",[],{"title":2264,"openalex":2266},{"EN":2265},"R. 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In light of the recent enhanced activity in the study of tsunami waves and their source mechanisms, we consider tsunami-like waves that are induced by atmospheric processes rather than by seismic sources. These waves are mainly associated with atmospheric gravity waves, pressure jumps, frontal passages, squalls and other types of atmospheric disturbances, which normally generate barotropic ocean waves in the open ocean and amplify them near the coast through specific resonance mechanisms (Proudman, Greenspan, shelf, harbour). The main purpose of the present study is to describe this hazardous phenomenon, to show similarities and differences between seismic and meteorological tsunamis and to provide an overview of meteorological tsunamis in the World Ocean. It is shown that tsunamis and meteotsunamis have the same periods, same spatial scales, similar physical properties and affect the coast in a comparably destructive way. Some specific features of meteotsunamis make them akin to landslide-generated tsunamis. The generation efficiency of both phenomena depend on the Froude number (Fr), with resonance taking place when Fr~1.0. Meteotsunamis are much less energetic than seismic tsunamis and that is why they are always local, while seismic tsunamis can have globally destructive effects. Destructive meteotsunamis are always the result of a combination of several resonant factors; the low probability of such a combination is the main reason why major meteotsunamis are infrequent and observed only at some specific locations in the ocean.\n                    \u003C\u002Fjats:p>","\u003Cjats:p>Tóm tắt. Trong bối cảnh hoạt động nghiên cứu sóng thần và cơ chế nguồn của chúng gần đây được tăng cường, chúng tôi xem xét các sóng giống như sóng thần được kích thích bởi các quá trình khí quyển thay vì các nguồn phát sinh động đất. Những sóng này chủ yếu liên quan đến các sóng trọng lực khí quyển, những bước nhảy áp suất, sự qua mặt của mặt trận, cơn bão và các loại rối loạn khí quyển khác, thường tạo ra sóng đại dương barotropic ở đại dương mở và khuếch đại chúng gần bờ thông qua các cơ chế cộng hưởng đặc biệt (Proudman, Greenspan, kệ, cảng). Mục tiêu chính của nghiên cứu hiện tại là mô tả hiện tượng nguy hiểm này, chỉ ra sự tương đồng và khác biệt giữa sóng thần do động đất và sóng thần khí tượng, đồng thời cung cấp cái nhìn tổng quan về sóng thần khí tượng trong đại dương thế giới. Đã chỉ ra rằng sóng thần và sóng thần khí tượng có cùng chu kỳ, cùng quy mô không gian, các tính chất vật lý tương tự và ảnh hưởng tới bờ biển theo cách tàn phá tương tự. Một số đặc điểm cụ thể của sóng thần khí tượng làm cho chúng tương tự như sóng thần do sạt lở tạo ra. Hiệu suất tạo ra của cả hai hiện tượng phụ thuộc vào số Froude (Fr), với cộng hưởng xảy ra khi Fr~1.0. Sóng thần khí tượng ít năng lượng hơn nhiều so với sóng thần do động đất và đó là lý do tại sao chúng thường chỉ xảy ra tại địa phương, trong khi sóng thần do động đất có thể có tác động tàn phá toàn cầu. Sóng thần khí tượng tàn phá luôn là kết quả của sự kết hợp của nhiều yếu tố cộng hưởng; xác suất thấp của sự kết hợp như vậy là lý do chính khiến sóng thần khí tượng lớn hiếm khi xảy ra và chỉ được quan sát tại một số vị trí cụ thể trong đại dương.\n                    \u003C\u002Fjats:p>",{"EN":2331,"VI":2332},"Meteotsunamis: atmospherically induced destructive ocean waves in the tsunami frequency band","Meteotsunamis: Sóng đại dương gây ra bởi khí quyển có tính phá hoại trong dải tần số sóng thần",{"VI":959},{"VOID":2335},"10.5194\u002Fnhess-6-1035-2006",[31],[30],"https:\u002F\u002Fnhess.copernicus.org\u002Farticles\u002F6\u002F1035\u002F2006\u002F",[2340,2367,2386],{"id":2341,"sortIndex":32,"researcher":28,"roles":2342,"affiliations":2343,"properties":2360,"displayName":2364,"givenName":28,"familyName":28},"79e87299-907d-413e-a53b-a292d7737529",[],[2344,2352],{"id":2345,"sortIndex":32,"affiliation":2346,"properties":28},"8e76a115-4881-4e05-86e4-45e167d9c603",{"id":2345,"createTime":28,"updateTime":28,"relativeEntities":2347,"slug":28,"properties":2348,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2351,"statistic":28},[],{"title":2349},{"EN":2350},"Departament de Física, Universitat de les Illes Balears, Palma de Mallorca, Spain",[],{"id":2353,"sortIndex":40,"affiliation":2354,"properties":28},"026e7090-9d91-4e90-bc0f-5eaa74ac848e",{"id":2353,"createTime":28,"updateTime":28,"relativeEntities":2355,"slug":28,"properties":2356,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2359,"statistic":28},[],{"title":2357},{"EN":2358},"IMEDEA, UIB-CSIC, Palma de Mallorca, Spain",[],{"orcid":2361,"title":2363,"openalex":2365},{"VOID":2362},"https:\u002F\u002Forcid.org\u002F0000-0002-5965-4872",{"EN":2364},"S. 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Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia",[],{"orcid":2407,"title":2409,"openalex":2411},{"VOID":2408},"https:\u002F\u002Forcid.org\u002F0000-0001-9328-0272",{"EN":2410},"Alexander B. 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Drought is a natural hazard that can cause a wide range of impacts affecting the environment, society, and the economy. Providing an impact assessment and reducing vulnerability to these impacts for regions beyond the local scale, spanning political and sectoral boundaries, requires systematic and detailed data regarding impacts. This study presents an assessment of the diversity of drought impacts across Europe based on the European Drought Impact report Inventory (EDII), a unique research database that has collected close to 5000 impact reports from 33 European countries. The reported drought impacts were classified into major impact categories, each of which had a number of subtypes. The distribution of these categories and types was then analyzed over time, by country, across Europe and for particular drought events. The results show that impacts on agriculture and public water supply dominate the collection of drought impact reports for most countries and for all major drought events since the 1970s, while the number and relative fractions of reported impacts in other sectors can vary regionally and from event to event. The analysis also shows that reported impacts have increased over time as more media and website information has become available and environmental awareness has increased. Even though the distribution of impact categories is relatively consistent across Europe, the details of the reports show some differences. They confirm severe impacts in southern regions (particularly on agriculture and public water supply) and sector-specific impacts in central and northern regions (e.g., on forestry or energy production). The protocol developed thus enabled a new and more comprehensive view on drought impacts across Europe. Related studies have already developed statistical techniques to evaluate the link between drought indices and the categorized impacts using EDII data. The EDII is a living database and is a promising source for further research on drought impacts, vulnerabilities, and risks across Europe. A key result is the extensive variety of impacts found across Europe and its documentation. This insight can therefore inform drought policy planning at national to international levels.\n                    \u003C\u002Fjats:p>","\u003Cjats:p>Tóm tắt. Hạn hán là một mối nguy tự nhiên có thể gây ra nhiều tác động khác nhau ảnh hưởng đến môi trường, xã hội và kinh tế. Việc cung cấp đánh giá tác động và giảm thiểu tổn thương đối với những tác động này cho các khu vực vượt ra ngoài quy mô địa phương, trải qua các ranh giới chính trị và ngành nghề, cần có dữ liệu hệ thống và chi tiết về tác động. Nghiên cứu này trình bày đánh giá về sự đa dạng của các tác động hạn hán trên toàn châu Âu dựa trên báo cáo tác động hạn hán châu Âu (EDII), một cơ sở dữ liệu nghiên cứu độc nhất có gần 5000 báo cáo tác động từ 33 quốc gia châu Âu. Các tác động do hạn hán được phân loại thành các loại tác động chính, mỗi loại bao gồm một số phân loại phụ. Sự phân bố của các loại và phân loại này sau đó đã được phân tích theo thời gian, theo quốc gia, trên toàn châu Âu và cho các sự kiện hạn hán cụ thể. Kết quả cho thấy tác động lên nông nghiệp và cung cấp nước công cộng chiếm ưu thế trong bộ sưu tập báo cáo tác động hạn hán cho hầu hết các quốc gia và cho tất cả các sự kiện hạn hán lớn kể từ những năm 1970, trong khi số lượng và tỷ lệ các tác động được báo cáo ở các ngành khác có thể thay đổi theo khu vực và theo từng sự kiện. Phân tích cũng cho thấy các tác động được báo cáo đã tăng lên theo thời gian khi thông tin từ phương tiện truyền thông và website trở nên phong phú hơn và nhận thức về môi trường gia tăng. Mặc dù sự phân bố của các loại tác động là tương đối đồng nhất trên toàn châu Âu, nhưng chi tiết của các báo cáo cho thấy một số khác biệt. Chúng xác nhận những tác động nghiêm trọng tại các vùng phía nam (đặc biệt là đối với nông nghiệp và cung cấp nước công cộng) và các tác động đặc thù theo ngành tại các vùng trung tâm và phía bắc (ví dụ, đối với lâm nghiệp hoặc sản xuất năng lượng). Quy trình được phát triển do đó đã đem lại cái nhìn mới và toàn diện hơn về tác động của hạn hán trên toàn châu Âu. Các nghiên cứu liên quan đã phát triển các kỹ thuật thống kê để đánh giá mối liên hệ giữa các chỉ số hạn hán và các tác động đã được phân loại sử dụng dữ liệu EDII. EDII là một cơ sở dữ liệu đang sống và là một nguồn hứa hẹn cho các nghiên cứu tiếp theo về tác động, tổn thương và rủi ro của hạn hán trên khắp châu Âu. Một kết quả quan trọng là sự đa dạng phong phú của các tác động được tìm thấy trên toàn châu Âu và sự ghi chép của nó. 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Hazards Earth Syst. Sci., 15, 1381–1397,\nhttps:\u002F\u002Fdoi.org\u002F10.5194\u002Fnhess-15-1381-2015, 2015.",{"doi":3062},"10.5194\u002Fnhess-15-1381-2015",{"id":28,"text":3064,"url":28,"identifiers":3065},"Blauhut V., Gudmundsson, L., and Stahl, K.: Towards pan-European drought risk\nmaps: quantifying the link between drought indices and reported drought\nimpacts, Environ. Res. Lett., 10, 014008, https:\u002F\u002Fdoi.org\u002F10.1088\u002F1748-9326\u002F10\u002F1\u002F014008, 2015a.",{"doi":3066},"10.1088\u002F1748-9326\u002F10\u002F1\u002F014008",{"id":28,"text":3068,"url":28,"identifiers":3069},"Blauhut, V., Stahl, K., and Kohn, I.: The dynamics of vulnerability to\ndrought from an impact perspective, in: Drought: Research and Science-Policy\nInterfacing, edited by: Andreu, J., Solera, A., Paredes-Arquiola, J.,\nHaro-Monteagudo, D., and van Lanen, H. A. J., CRC Press, London, 349–354,\nhttps:\u002F\u002Fdoi.org\u002F10.1201\u002Fb18077-56, 2015b.",{"doi":3070},"10.1201\u002Fb18077-56",{"id":28,"text":3072,"url":28,"identifiers":3073},"Bouma, E.: Development of comparable agro-climatic zones for the\ninternational exchange of data on the efficacy and crop safety of plant\nprotection products, Bulletin OEPP\u002FEPPO, 35, 233–238, 2005.",{"doi":3074},"10.1111\u002Fj.1365-2338.2005.00830.x",{"id":28,"text":3076,"url":28,"identifiers":3077},"Ceglar, A., Medved-Cvikl, B., Morán-Tejeda, E., Vicente Serrano, S. M.,\nand Kajfež-Bogataj, L.: Assessment of multi-scale drought datasets to\nquantify drought severity and impacts in agriculture: a case study for\nSlovenia, Int. J. Spat. Data Infrastruct. 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A. J., Tallaksen, L. M., Stahl, K., Assimacopoulos, D.,\nWolters, W., Andreu, J., Rego, F., Seneviratne, S. I., De Stefano, L.,\nMassarutto, A., Garnier, E., and Seidl, I.: Fostering Drought Research and\nScience-Policy Interfacing: Achievements of the DROUGHT-R&SPI project,\nin: Drought: Research and Science-Policy Interfacing, edited by: Andreu, J.,\nSolera, A., Paredes-Arquiola, J., Haro-Monteagudo, D., and van Lanen, H. A.\nJ., CRC Press, London, 3–12, https:\u002F\u002Fdoi.org\u002F10.1201\u002Fb18077-56, 2015.",{"doi":3070},{"id":28,"text":3192,"url":28,"identifiers":3193},"Van Loon, A. F. and Van Lanen, H. A. J.: A process-based typology of hydrological\ndrought, Hydrol. Earth Syst. Sci., 16, 1915–1946, https:\u002F\u002Fdoi.org\u002F10.5194\u002Fhess-16-1915-2012, 2012.",{"doi":3194},"10.5194\u002Fhess-16-1915-2012",{"id":28,"text":3196,"url":28,"identifiers":3197},"Van Loon, A. F., Ploum, S. W., Parajka, J., Fleig, A. K., Garnier, E.,\nLaaha, G. and Van Lanen, H. A. 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A.,\nRoutledge, New York, London, 245–255, 2000.",{},{"id":28,"text":3210,"url":28,"identifiers":3211},"Wilhite, D. A., Svoboda, M. D., and Hayes, M. J.: Understanding the complex\nimpacts of drought: A key to enhancing drought mitigation and preparedness,\nWater Resour. Manage., 21, 763–774, https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs11269-006-9076-5, 2007.",{"doi":3212},"10.1007\u002Fs11269-006-9076-5",{"id":3214,"createTime":3215,"updateTime":3216,"relativeEntities":3217,"slug":3218,"properties":3219,"entityType":962,"verifyStatus":26,"verifyTime":3215,"verifyNote":963,"languages":3233,"translateLanguages":3234,"viewCount":32,"primaryUrl":3235,"fullTextUrl":28,"authors":3236,"publicationType":1004,"publisherRelationship":3322,"citationCount":3366,"citationInfo":3367,"publishDate":28,"publishYear":28,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":3369,"openAccess":28,"references":3370,"isForceReanalyzing":1510},"d794e9f0-348e-43b3-a6dc-72242a1dfc92","2024-09-28T09:43:31.946+00:00","2025-02-21T07:46:13.474+00:00",[],"The-European-storm-Kyrill-in-January-2007-synoptic-evolution-meteorological-impacts-and-some-considerations-with-respect-to-climate-change",{"openalex":3220,"mag":3222,"abstract":3224,"title":3227,"keywords":3230,"doi":3231},{"VOID":3221},"W2082323488",{"VOID":3223},"2082323488",{"EN":3225,"VI":3226},"\u003Cjats:p>Abstract. The synoptic evolution and some meteorological impacts of the European winter storm Kyrill that swept across Western, Central, and Eastern Europe between 17 and 19 January 2007 are investigated. The intensity and large storm damage associated with Kyrill is explained based on synoptic and mesoscale environmental storm features, as well as on comparisons to previous storms. Kyrill appeared on weather maps over the US state of Arkansas about four days before it hit Europe. It underwent an explosive intensification over the Western North Atlantic Ocean while crossing a very intense zonal polar jet stream. A superposition of several favourable meteorological conditions west of the British Isles caused a further deepening of the storm when it started to affect Western Europe. Evidence is provided that a favourable alignment of three polar jet streaks and a dry air intrusion over the occlusion and cold fronts were causal factors in maintaining Kyrill's low pressure very far into Eastern Europe.  Kyrill, like many other strong European winter storms, was embedded in a pre-existing, anomalously wide, north-south mean sea-level pressure (MSLP) gradient field. In addition to the range of gusts that might be expected from the synoptic-scale pressure field, mesoscale features associated with convective overturning at the cold front are suggested as the likely causes for the extremely damaging peak gusts observed at many lowland stations during the passage of Kyrill's cold front. Compared to other storms, Kyrill was by far not the most intense system in terms of core pressure and circulation anomaly. However, the system moved into a pre-existing strong MSLP gradient located over Central Europe which extended into Eastern Europe. This fact is considered determinant for the anomalously large area affected by Kyrill.  Additionally, considerations of windiness in climate change simulations using two state-of-the-art regional climate models driven by ECHAM5 indicate that not only Central, but also Eastern Central Europe may be affected by higher surface wind speeds at the end of the 21st century. These changes are partially associated with the increased pressure gradient over Europe which is identified in the ECHAM5 simulations. Thus, with respect to the area affected, as well as to the synoptic and mesoscale storm features, it is proposed that Kyrill may serve as an interesting study case to assess future storm impacts.\n                    \u003C\u002Fjats:p>","\u003Cjats:p>Trích dẫn. Sự phát triển đồng bộ và một số tác động khí tượng của cơn bão mùa đông Kyrill châu Âu đã xảy ra trên Tây Âu, Trung Âu và Đông Âu từ ngày 17 đến ngày 19 tháng 1 năm 2007 được nghiên cứu. Cường độ và thiệt hại lớn về bão liên quan đến Kyrill được giải thích dựa trên các đặc điểm môi trường bão đồng bộ và mesoscale, cũng như qua việc so sánh với các cơn bão trước đó. Kyrill xuất hiện trên bản đồ thời tiết ở bang Arkansas của Mỹ khoảng bốn ngày trước khi nó đổ bộ vào châu Âu. Nó đã trải qua một sự gia tăng cường độ đột ngột khi vượt qua Bắc Đại Tây Dương trong khi băng qua một dòng jet cực kỳ mạnh trên trục phương. Sự chồng chéo của một số điều kiện khí tượng thuận lợi phía tây quần đảo Anh đã gây ra sự sâu thêm của bão khi nó bắt đầu ảnh hưởng đến Tây Âu. Có bằng chứng cho thấy sự căn chỉnh thuận lợi của ba vệt jet cực và một làn không khí khô xâm nhập qua các mặt tiền lạnh và mặt tiền chắn là những yếu tố gây ra trong việc duy trì áp suất thấp của Kyrill rất xa vào Đông Âu. Kyrill, giống như nhiều cơn bão mùa đông mạnh khác ở châu Âu, được nhúng trong một trường gradient áp suất trung bình ở mực nước biển (MSLP) Bắc-Nam có độ rộng bất thường trước đó. Ngoài khoảng gió có thể được mong đợi từ trường áp suất đồng bộ, các đặc điểm mesoscale liên quan đến sự lật ngược đối lưu ở mặt trước lạnh được đưa ra như là những nguyên nhân có khả năng cho các đợt gió cực kỳ thiệt hại đã được quan sát tại nhiều trạm vùng trũng trong suốt quá trình cơn bão Kyrill đi qua. So với các cơn bão khác, Kyrill không phải là hệ thống mạnh nhất về áp suất lõi và dị thường dòng chảy. Tuy nhiên, hệ thống đã di chuyển vào một gradient áp suất MSLP mạnh có sẵn nằm trên Trung Âu kéo dài vào Đông Âu. Thực tế này được coi là quyết định cho khu vực bất thường lớn bị ảnh hưởng bởi Kyrill. Ngoài ra, việc xem xét sự gió mạnh trong các mô phỏng biến đổi khí hậu sử dụng hai mô hình khí hậu khu vực tiên tiến do ECHAM5 điều khiển cho thấy rằng không chỉ Trung Âu, mà cả Đông Trung Âu cũng có thể bị ảnh hưởng bởi tốc độ gió bề mặt cao hơn vào cuối thế kỷ 21. Những thay đổi này một phần liên quan đến gradient áp suất tăng lên trên châu Âu mà được xác định trong các mô phỏng ECHAM5. Do đó, với sự liên quan đến khu vực bị ảnh hưởng, cũng như các đặc điểm bão đồng bộ và mesoscale, Kyrill có thể được đề xuất như là một trường hợp nghiên cứu thú vị để đánh giá các tác động của cơn bão trong tương lai.\u003C\u002Fjats:p>",{"EN":3228,"VI":3229},"The European storm Kyrill in January 2007: synoptic evolution, meteorological impacts and some considerations with respect to climate change","Cơn bão châu Âu Kyrill vào tháng 1 năm 2007: sự phát triển đồng bộ, những tác động khí tượng và một số xem xét liên quan đến biến đổi khí hậu",{"VI":959},{"VOID":3232},"10.5194\u002Fnhess-9-405-2009",[31],[30],"https:\u002F\u002Fnhess.copernicus.org\u002Farticles\u002F9\u002F405\u002F2009\u002F",[3237,3256,3273,3288,3305],{"id":3238,"sortIndex":32,"researcher":28,"roles":3239,"affiliations":3240,"properties":3249,"displayName":3253,"givenName":28,"familyName":28},"2d797024-5017-49f6-8d14-b1fde603f458",[],[3241],{"id":3242,"sortIndex":32,"affiliation":3243,"properties":28},"544b3983-adf0-44b6-b7a3-11cc7b6ba688",{"id":3242,"createTime":28,"updateTime":28,"relativeEntities":3244,"slug":28,"properties":3245,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":3248,"statistic":28},[],{"title":3246},{"EN":3247},"Institute for Geophysics and Meteorology, Univ. of Cologne, Germany",[],{"orcid":3250,"title":3252,"openalex":3254},{"VOID":3251},"https:\u002F\u002Forcid.org\u002F0000-0002-5840-2120",{"EN":3253},"Andreas H. 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An algorithm developed to map flooded areas from synthetic aperture radar imagery is presented in this paper. It is conceived to be inserted in the operational flood management system of the Italian Civil Protection and can be used in an almost automatic mode or in an interactive mode, depending on the user's needs. The approach is based on the fuzzy logic that is used to integrate theoretical knowledge about the radar return from inundated areas taken into account by means of three electromagnetic scattering models, with simple hydraulic considerations and contextual information. This integration aims at allowing a user to cope with situations, such as the presence of vegetation in the flooded area, in which inundation mapping from satellite radars represents a difficult task. The algorithm is designed to work with radar data at L, C, and X frequency bands and employs also ancillary data, such as a land cover map and a digital elevation model. The flood mapping procedure is tested on an inundation that occurred in Albania on January 2010 using COSMO-SkyMed very high resolution X-band SAR data.\n                    \u003C\u002Fjats:p>","\u003Cjats:p>Tóm tắt. Bài báo này trình bày một thuật toán được phát triển để lập bản đồ các khu vực ngập lụt từ hình ảnh radar tổng hợp. Thuật toán này được thiết kế để được đưa vào hệ thống quản lý lũ lụt hoạt động của Cơ quan Bảo vệ Dân sự Ý và có thể được sử dụng ở chế độ gần như tự động hoặc ở chế độ tương tác, tùy thuộc vào nhu cầu của người dùng. Phương pháp này dựa trên logic mờ, được sử dụng để tích hợp kiến thức lý thuyết về phản xạ radar từ các khu vực bị ngập nước, dựa trên ba mô hình tán xạ điện từ, cùng với các cân nhắc thủy lực đơn giản và thông tin ngữ cảnh. Sự tích hợp này nhằm giúp người dùng có thể xử lý các tình huống, chẳng hạn như sự hiện diện của thực vật trong khu vực ngập lụt, trong đó việc lập bản đồ ngập lụt từ radar vệ tinh là một nhiệm vụ khó khăn. Thuật toán này được thiết kế để hoạt động với dữ liệu radar ở các băng tần tần số L, C và X, và cũng sử dụng dữ liệu bổ sung, chẳng hạn như bản đồ che phủ đất và mô hình độ cao số. Quy trình lập bản đồ lũ lụt đã được thử nghiệm trên một đợt ngập xảy ra ở Albania vào tháng 1 năm 2010, sử dụng dữ liệu SAR băng X độ phân giải cao rất lớn từ COSMO-SkyMed.\n                    \u003C\u002Fjats:p>",{"EN":3514,"VI":3515},"An algorithm for operational flood mapping from Synthetic Aperture Radar (SAR) data using fuzzy logic","Thuật toán cho việc lập bản đồ lũ lụt trong hoạt động từ dữ liệu Radar tổng hợp (SAR) sử dụng logic mờ",{"VI":959},{"VOID":3518},"10.5194\u002Fnhess-11-529-2011",[31],[30],"https:\u002F\u002Fnhess.copernicus.org\u002Farticles\u002F11\u002F529\u002F2011\u002F",[3523,3542,3559,3578],{"id":3524,"sortIndex":32,"researcher":28,"roles":3525,"affiliations":3526,"properties":3535,"displayName":3539,"givenName":28,"familyName":28},"ebd43e25-ce71-41b5-8cd3-596ce2d5a884",[],[3527],{"id":3528,"sortIndex":32,"affiliation":3529,"properties":28},"3db66000-a1b8-4b04-8985-2e174fba0a72",{"id":3528,"createTime":28,"updateTime":28,"relativeEntities":3530,"slug":28,"properties":3531,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":3534,"statistic":28},[],{"title":3532},{"VI":3533},"Department of Information Engineering, Electronics, and Telecommunications, SAPIENZA University of Rome, Via Eudossiana 18, 00184 Rome, 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Ma trận biến đổi affine giữa hai lần thu thập TLS miêu tả chính xác các dịch chuyển của vụ lở đất và cho phép tách biệt chúng thành các thành phần dịch chuyển dịch chuyển, chẳng hạn như tốc độ và hướng dịch chuyển, và các thành phần quay giống như lật ngược. Nghiên cứu này cho thấy khả năng của TLS trong việc thu được thông tin dịch chuyển 3-D đáng tin cậy trên một khu vực lớn không ổn định. Cuối cùng, một mô hình không ổn định khả thi cho phần trên của vụ lở đất Åknes giải thích các dịch chuyển dịch chuyển và quay đã đo được bằng sự kết hợp của trượt phẳng về phía nam dọc theo lớp gneiss, sự lún trọng lực theo chiều dọc dọc theo bề mặt trượt đáy phức tạp, bước và sự lật ngược về phía bắc theo cấu trúc graben đã mở. \u003C\u002Fjats:p>","\u003Cjats:p>Abstract. Terrestrial laser scanning (TLS) provides high-resolution point clouds of the topography and new TLS instruments with ranges exceeding 300 m or even 1000 m are powerful tools for characterizing and monitoring slope movements. 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