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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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Aerosols coming from the Sahara Desert were found to be loaded with particulate matter, especially silicon. The aerosols were shown to have varying geochemical behaviour along the “South-North” displacement of the Saharan plumes, depending on the wind flow characteristics, geomorphologic features and the nature of soils swept by the wind. In the south and the center part of the country, the transfer of aerosol constituents to the soil (by gravity and\u002For impaction) was probably predominated by localized enrichment phenomena. The latter are reinforced by the effect of turbulent winds over bare soils, wind wakes and probably selective disintegration, especially in the vicinity of the geomorphologic features of central Tunisia. These relatively high features, extending over important distances, appear to be of paramount importance for the phenomena of redistribution of aerosol constituents even during periods without Sirocco wind circulations. In the northern section of the country, aerosol constituent concentrations dropped to almost 50%, in spite of the abundance of localized turbulent winds. This may be explained by the effect of forests and the relatively dense vegetation cover, which clearly reinforces the transfer phenomena to the soil and the attenuate of dust entrainment.",{"EN":997},"Geochemical behaviour of the Tunisian background aerosols in Sirocco wind circulations",{"VOID":999},"Aviala, A., and J. Penuelas, 1999: Increasing frequency of Saharan rains over north-eastern Spain and its ecological consequences. The Science of Total Environment, 228(2–3), 153–156.\nAzri, C., A. Maalej, A. Tlili, and K. Medhioub, 2002: Characterization of the pollution level in Sfax City (Tunisia): Influence of sources and meteorological factors. Techniques, Sciences, Méthodes TSM, 97, 78–92.\nBach, W., 1976: Global air pollution and climate change. Rev. Geophys. Space Phys., 14(3), 429–474.\nBelghith, I., 1999: Study of the atmospheric aerosol in the region of Sfax: Influence of local and synoptic meteorological conditions. Ph. D. dissertation, University of Tunis II, 207pp.\nBen Ayed, N., 1993: Tectonic evolution of the alpine range of Tunisia. Annuals of mines and geology, No. 32, Editions of the geologic service of Tunisia, 120pp.\nBlum, M. D., G. Kocurek, M. Deynoux, C. Swezey, N. Lancaster, D. Price, and J. C. Pion, 1998: Quaternary wadi lacustrine Aeolian depositional cycles and sequences, Chott Gharsa Basin. Quanternary Deserts and Climatic Change, Alsharhan et al., Eds., Balkema Press, 552pp.\nBorbely-Kiss, I., A. Z. Kiss, E. Koltay, G. Szabo, and L. Lozo, 2004: Saharan dust episodes in Hungarian aerosol: Elemental signatures and transport trajectories. Journal of Aerosol Sciences, 53(10), 1205–1224.\nBousnina, A., 1990: Climate of Sfax. Report No. 1, Magreb-Editions, INM, 61pp.\nBrewer, P. G., 1975: Minor elements in sea water. Chemical Oceanography, 2nd ed., J.P. Riley, G. Skirrow, Eds., Academic Press, London, 415–496.\nCharlson, R. J., S. E. Schwartz, J. M. Hales, R. D. Cess, J. A. Coakley, J. E. Hansen, and D. J. Hofmann, 1992: Climate forcing by anthropogenic aerosols. Science, 225, 423–430.\nDraxler, R. R., and G. D. Rolph, 2003: HYSPLIT (HYbrid Single-Particle Lagrangian Integrated Trajectory) Model, NOAA Air Resources Laboratory, Silver Spring, MD. [Available online from http:\u002F\u002Fwww.arl.noaa.gov\u002Fready\u002Fhysplit4.html].\nEngelstaedter, S., I. Tegen, and R. Washington, 2006: North African dust emissions and transport. Earth Science Reviews, 79(1–2), 73–100.\nGanor, E., 1994: The frequency of Saharan dust episodes over Tel Aviv, Israel. Atmos. Environ., 28(17), 2867–2871.\nGoudie, A. S., and N. J. Middleton, 2001: Saharan dust storms: Nature and consequences. Earth Science Reviews, 56, 179–204.\nIPCC, 2001: Climate Change 2001: The Scientific Basis. Contribution of Working Group I to the Third Assessment Report of International Panel on Climate Change, Houghton et al., Eds., Cambridge University Press, Cambridge and New York, 572pp.\nIsraelevich, P. L., E. Ganor, Z. Levin, and J. H. Joseph, 2003: Annual variations of physical properties of desert dust over Israel. Geophysical Research, Deposition, John Wiley and Sons, New York, 242pp.\nKubilay, N., S. Nickovic, C. Moulin, and F. Dulac, 2000: An illustration of the transport and deposition of mineral dust onto the eastern Mediterranean. Atmos. Environ., 34(8), 1293–1303.\nLuria, M., and Coauthors, 1996: Atmospheric Sulfur over the east Mediterranean region. J. Geophys. Res., 101(25), 917–930.\nMasmoudi, M., M. Chaabane, D. Tanré, P. Gouloup, L. Blarel, and F. Elleuch, 2003: Spatial and temporal variability of aerosol: Size distribution and optical properties. Atmospheric Research, 66, 1–19.\nMason, B. H., 1966: Principles of Geochemistry. 3rd ed., Wiley and Sons, New York, 329pp.\nMtimet, A. 1999: Atlas des Sols Tunisiens. Ministére de l’Agriculture, Impr, Graphimed, 165pp.\nN’Tchayi, M. G., J. J. Gertrand, and S. E. Nicholson, 1997: The diurnal and seasonal cycles of wind borne dust over Africa north of the equator. J. Appl. Meteor., 36, 868–882.\nOzer, P., 2001: Litho-meteorites in the Sahelian Region. International Journal of Tropical Ecology and Geography, 24, 1–317.\nPerry, K. D., T. A. Cahill, R. A. Eldred, D. D. Dutcher, and T. E. Gill, 1997: Long-range transport of North African dust to the eastern United States. J. Geophys. Res., 102(D10), 11225–11238.\nProspero, J. M., 1980: Aeolian transport to the world ocean. Vol. 7, The Oceanic Lithosphere, The Sea, C. Emiliani, Ed., Wiley-Interscience, New York, 801–874.\nProspero, J. M., and P. J. Lamb, 2003: African droughts and dust transport to the Caribbean: Climate change implications. Science, 302(5647), 1024–1027.\nProspero, J. M., R. A. Glaccum, and R. T. Nees, 1981: Atmospheric transport of soil dust from Africa to South America. Nature, 289, 570–572.\nProspero, J. M., P. Ginoux, O. Torres, S. E. Nicholson, and T. E. Gill, 2002: Environmental characterization of global sources of atmospheric soil dust identified with the Nimbus 7 Total Ozone Mapping Spectrometer (TOMS) absorbing aerosol product. Rev. Geophys., 40(1), 1002.\nPye, K., 1987: Aeolian Dust and Dust Deposits. Academic Press, Inc. (London) Ltd, 177pp.\nReydet, L. G., 1984: Contribution àl’étude des origines de quelques constituants de l’aérosol atmosph_rique en milieu côtier. Thèse de Doctorat, Universitè Paris VII, 124pp. (in French)\nRolph, G. D., 2003: Real-time Environmental Applications and Display sYstem (READY) Website, NOAA Air Resources Laboratory, Silver Spring, MD. http:\u002F\u002Fwww.arl.noaa.gov\u002Fready\u002Fhysplit4.html.\nRyde, H., 1970: L’importance de la météorologie en matière de construction. Genève, Organisation météorologique mondiale Tech. Note No. 109, OMM No. 255.TP.142, 23-36. (in French)\nSehmel, G. A., 1980: Particle and gas dry deposition: A review. Atmos. Environ., 14, 983–1011.\nSeinfeld, J. H., and S. N. Pandis, 1988: Atmospheric chemistry and physics: From air pollution to climate change. John Wiley & Sons, Inc, New York, 1326pp.\nSwap, R., M. Garstang, S. Greco, R. Talbot, and P. Kallberg, 1992: Saharan dust in the Amazon Basin. Tellus B, 44(2), 133–149.\nTwomey, S., 1977: The influence of pollution on the short wave albedo of clouds. J. Atmos. Sci., 34, 1149–1152.\nWashington, R., M. C. Todd, N. J. Middelton, and A. S. Goudie, 2003: Dust-storm source areas determined by the total ozone monitoring spectrometer and surface observations. Annals of the Association of American Geographers, 93(2), 297–313.\nWatson, A., 1985: Structure, chemistry and origins of gypsum crusts in southern Tunisia and the central Namib desert. Sedimentology, 32, 855–875.\nYoboue, V., 1991: Caractéristiques physiques et chimiques des aérosols et des pluies collectés dans la savane humide de Côte d’Ivoire. Thèse de Doctorat, Université Paul Sabatier (Toulouse), 146pp. (in French)\nZender, C. S., R. L. Miller, and I. Tegen, 2004: Quantifying mineral dust mass budgets: Terminology, constraints and current estimates, EOS, Transaction. 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Medhioub","ARTICLE",{"url":1004,"publisher":1052,"properties":1088},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1053,"slug":872,"properties":1054,"entityType":25,"verifyStatus":878,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1057,"manageAffiliations":1062,"indexDatabases":1068,"url":28,"thumbnailPath":28,"statistic":1083,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1055,"title":1056},{"VOID":875},{"EN":877},[1058],{"id":881,"createTime":28,"updateTime":28,"relativeEntities":1059,"label":1060,"description":1061,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":884},{},[1063],{"id":888,"createTime":28,"updateTime":28,"relativeEntities":1064,"slug":28,"properties":1065,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1067,"statistic":28},[],{"title":1066},{"EN":892},[],[1069,1076],{"id":896,"indexDatabase":1070,"url":902,"indexYears":903,"academicFieldIds":1075,"indexDatabaseRanking":906},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1071,"label":1072,"description":1073,"key":781,"publicationTags":1074,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[905],{"id":908,"indexDatabase":1077,"url":920,"indexYears":28,"academicFieldIds":1082,"indexDatabaseRanking":28},{"id":910,"createTime":28,"updateTime":28,"relativeEntities":1078,"label":1079,"description":1080,"key":917,"publicationTags":1081,"standard":28},[],{"EN":913,"VI":913},{"EN":915,"VI":916},[919,813],[922],{"impactFactor":32,"impactFactorByYear":1084,"i10Index":570,"i10IndexLast5Year":140,"totalPublication":927,"totalPublicationByYear":1085,"totalCitation":934,"totalCitationByYear":1086,"totalCitationPerPublication":959,"totalCitationPerPublicationByYear":1087,"hindexLast5Year":141,"hindex":141},{"2012":52,"2013":423,"2014":229,"2015":121,"2016":422,"2017":346,"2018":422,"2019":170,"2020":225,"2021":289,"2022":925,"2023":926},{"1984":127,"1985":137,"1986":140,"1987":138,"1988":134,"1989":133,"1990":134,"1991":202,"1992":142,"1993":137,"1994":139,"1995":69,"1996":135,"1997":69,"1998":139,"1999":352,"2000":142,"2001":158,"2002":325,"2003":162,"2004":151,"2005":208,"2006":208,"2007":567,"2008":157,"2009":354,"2010":929,"2011":358,"2012":930,"2013":354,"2014":211,"2015":931,"2016":530,"2017":566,"2018":932,"2019":157,"2020":330,"2021":154,"2022":933,"2023":574,"2024":142},{"1984":145,"1985":48,"1986":357,"1987":199,"1988":45,"1989":936,"1990":937,"1991":47,"1992":201,"1993":938,"1994":354,"1995":130,"1997":939,"1998":129,"1999":940,"2000":941,"2001":942,"2002":599,"2003":943,"2004":944,"2005":945,"2006":946,"2007":947,"2008":599,"2009":604,"2010":948,"2011":949,"2012":950,"2013":951,"2014":952,"2015":953,"2016":954,"2017":955,"2018":956,"2019":957,"2020":435,"2021":701,"2022":958,"2023":933,"2024":48},{"1984":440,"1985":318,"1986":582,"1987":462,"1988":365,"1989":961,"1990":962,"1991":319,"1992":963,"1993":592,"1994":964,"1995":228,"1997":965,"1998":691,"1999":966,"2000":967,"2001":968,"2002":969,"2003":970,"2004":971,"2005":972,"2006":123,"2007":973,"2008":741,"2009":177,"2010":974,"2011":975,"2012":976,"2013":977,"2014":978,"2015":979,"2016":703,"2017":980,"2018":981,"2019":982,"2020":589,"2021":590,"2022":287,"2023":695,"2024":734},{"pages":1089,"volume":1091},{"VOID":1090},"390-402",{"VOID":1092},"26","2009-05-08",2009,[906,919],false,{"id":1098,"createTime":1099,"updateTime":1099,"relativeEntities":1100,"slug":1101,"properties":1102,"entityType":1002,"verifyStatus":878,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1111,"fullTextUrl":28,"authors":1112,"publicationType":1050,"publisherRelationship":1215,"citationCount":28,"citationInfo":28,"publishDate":1257,"publishYear":1258,"citationAnalyzeStatus":878,"lastCitationAnalyze":28,"indexDatabases":1259,"openAccess":28,"references":28,"isForceReanalyzing":1096},"00d90d4f-481d-44ed-ba10-175f81b06677","2023-12-01T23:52:41.974+00:00",[],"Anthropogenic-Aerosol-Pollution-over-the-Eastern-Slope-of-the-Tibetan-Plateau",{"abstract":1103,"title":1105,"references":1107,"doi":1109},{"EN":1104},"In this study, a combination of satellite observations and reanalysis datasets is used to analyze the spatiotemporal distribution, classification and source of pollutants over the eastern slope of the Tibetan Plateau (ESTP). The aerosol optical depth (AOD) over the ESTP is extremely large and even larger than some important industrialized regions and deserts. The main aerosol component over the ESTP is sulfate, followed by carbonaceous and dust aerosols. Local emissions related to human activity directly contribute to the accumulation of sulfate and carbonaceous aerosols over the Sichuan Basin. In addition, in spring, abundant carbonaceous aerosols emitted from forest, grassland and savanna fires in Southeast Asia can be transported by the prevailing southwesterly wind to southern China and the ESTP. The dust AOD over the ESTP peaks in spring because of the transport from the Taklimakan and Gobi deserts. Additionally, the high aerosol loading over the ESTP is also directly related to the meteorological background. Due to the special topography, the terrain-driven circulation can trap aerosols in the Sichuan Basin and these aerosols can climb along the ESTP due to the perennial updraft. The aerosol loading is lowest in summer because of effective wet deposition induced by the strong precipitation and better dispersion conditions due to the larger vertical temperature gradients and ascending air movement enhanced by the plateau heat pump effect. In contrast, the aerosol loading is greatest in winter. Abundant anthropogenic aerosols over the ESTP may generate some climatic and environmental risks and consequently greatly influence the downstream regions.",{"EN":1106},"Anthropogenic Aerosol Pollution over the Eastern Slope of the Tibetan Plateau",{"VOID":1108},"Abdou, W. A., and Coauthors, 2005: Comparison of coincident multiangle imaging spectroradiometer and moderate resolution imaging spectroradiometer aerosol optical depths over land and ocean scenes containing aerosol robotic network sites. J. Geophys. 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Keller, 2017: Impact of Southeast Asian smoke on aerosol properties in Southwest China: First comparison of model simulations with satellite and ground observations. J. Geophys. Res., 122, 3904–3919, https:\u002F\u002Fdoi.org\u002F10.1002\u002F2016JD025793.\nZhu, Q. Z., Y. Z. Liu, R. Jia, S. Hua, T. B. Shao, and B. Wang, 2018: A numerical simulation study on the impact of smoke aerosols from Russian forest fires on the air pollution over Asia. Atmos. 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global atmospheric general circulation model has been used to perform eleven idealized numerical experiments, i.e., TP00, TP10, ..., TP100, corresponding to different percentages of the Tibetan Plateau altitude. The aim is to explore the sensitivity of East Asian climate to the uplift and expansion of the Tibetan Plateau under the reconstructed boundary conditions for the mid-Pliocene about 3 Ma ago. When the plateau is progressively uplifted, global annual surface temperature is gradually declined and statistically significant cooling signals emerge only in the Northern Hemisphere, especially over and around the Tibetan Plateau, with larger magnitudes over land than over the oceans. On the contrary, annual surface temperature rises notably over Central Asia and most parts of Africa, as well as over northeasternmost Eurasia in the experiments TP60 to TP100. Meanwhile, the plateau uplift also leads to annual precipitation augmentation over the Tibetan Plateau but a reduction in northern Asia, the Indian Peninsula, much of Central Asia, parts of western Asia and the southern portions of northeastern Europe. Additionally, it is found that an East Asian summer monsoon system similar to that of the present initially exists in the TP60 and is gradually intensified with the continued plateau uplift. At 850 hPa the plateau uplift induces an anomalous cyclonic circulation around the Tibetan Plateau in summertime and two anomalous westerly currents respectively located to the south and north of the Tibetan Plateau in wintertime. In the mid-troposphere, similar-to-modern spatial pattern of summertime western North Pacific subtropical high is only exhibited in the experiments TP60 to TP100, and the East Asian trough is steadily deepened in response to the progressive uplift and expansion of the Tibetan Plateau.",{"EN":1270},"Sensitivity of East Asian climate to the progressive uplift and expansion of the Tibetan Plateau under the mid-Pliocene boundary conditions",{"VOID":1272},"Abe, M., A. Kitoh, and T. 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Sci.,27: 1213–1215.",{"doi":1535},"10.1175\u002F1520-0469(1970)027\u003C1213:ANOTVS>2.0.CO;2",{"id":28,"text":1537,"url":28,"identifiers":1538},"Pielke R. A. (1974), A three dimensional numerical model of the sea breeze over South Florida,J. Atmos. Sci.,102: 115–139.",{},{"id":28,"text":1540,"url":28,"identifiers":1541},"Wu Huiding and Zhang Xingwang (1984), A numerical model of atmospheric boundary layer,Acta. Meteor. Sinica,42: 290–300 (in Chinese with English abstract).",{},{"id":28,"text":1543,"url":28,"identifiers":1544},"Yamagishi Y. (1980), Simulation of the air-mass transformation process using a numerical model with the detailed boundary layer parmeterization,J. Meteor. Soc. Japan,58: 357–377.",{"doi":1545},"10.2151\u002Fjmsj1965.58.5_357",{"id":28,"text":1547,"url":28,"identifiers":1548},"Zhang D.-L. (1982), A high-resolution model of the planetary boundary layer-sensitivity tests and comparisons with SESAME-79 data,J. Appl. Meteor.,21: 1594–1609.",{"doi":1549},"10.1175\u002F1520-0450(1982)021\u003C1594:AHRMOT>2.0.CO;2",{"id":28,"text":1551,"url":28,"identifiers":1552},"Zhou Xiaoping (1980), An introduction of a fine-mesh numerical weather model, Institute of Atmospheric Physics, Academia Sinica (in Chinese).",{},{"id":1554,"createTime":1555,"updateTime":1555,"relativeEntities":1556,"slug":28,"properties":1557,"entityType":1002,"verifyStatus":878,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1566,"fullTextUrl":28,"authors":1567,"publicationType":1050,"publisherRelationship":1598,"citationCount":28,"citationInfo":28,"publishDate":1640,"publishYear":1641,"citationAnalyzeStatus":878,"lastCitationAnalyze":28,"indexDatabases":1642,"openAccess":28,"references":28,"isForceReanalyzing":1096},"01ebad8b-b07c-41b0-baa6-ecc49494942c","2024-02-10T11:07:06.698+00:00",[],{"abstract":1558,"title":1560,"references":1562,"doi":1564},{"EN":1559},"By use of the filter analysis technique, the Complex Empirical Othogonal Function (CEOF) method and the ECMWF\u002FWMO 2.5° × 2.5° grid data of the geopotential heights during the summer months in 1988, an interseasonal process that the western Pacific subtropical high (WPSH) was anomalously far to the north in the first and second ten days of July is studied. It has been found that in the western Pacific subtropical region in the first and second ten days of July, it is the continuous assembly of low frequency geopotential waves (LFGWs) that leads to the abnormality of WPSH. This abnormality emerges with the enhancement of wave assembling and ceases while the wave assembling situation disappears. The structure of the low frequency assembling waves corresponds to the structure of subtropical high in its abnormal period. The effect of the assembling waves on the abnormality of subtropical high can be considered as the accumulation of disturbance energy carried by the low frequency waves from different directions in the western Pacific region.",{"EN":1561},"A diagnostic study on the relationship between the assembling of low frequency waves in the pacific ocean and the abnormality of the subtropical high",{"VOID":1563},"Barnet, T. P. (1983), Interaction of the monsoon and Pacific trade wind system at interannual scale, Part 1: The equational zone, Mon. Wea. Rev., 111: 756–773.\nChen Longxun, Xie An (1980), Westward propagating low frequency-Oscillation and its teleconnection in the Eastern Hemisphere, Acta Meteor. Sinica, 2: 300–312.\nDuan Meicheng, Yu Shihua (1997), Diagnostic study and numerical simulation on the intraseasonal anomalous advancement \u002F retreat of the West Pacific Subtropical High, J. Trop. Meteor., 13: 132–139.\nHuang Jiayou (1988), The Complex Empirical Othogonal Function (CEOF) and its application in the diagnostic analysis to weather process, Meteor., 14(5): 3–8.\nKrishnamurti T. N. et. al. (1976), Oscillation of a monsoon system, Part 1: Observational aspect, J. Atmos. Sci., 33: 1937–1954.\nLi Xinglian and Yu Shihua (1996), Distribution of low frequency waves in North Pacific and intraseasonal abnormality of the Western Pacific Subtropical High, J. Trop. Meteor., 2: 172–180.\nLiu Fuming, Lin Hai (1990), Discussions of low-frequency Oscillation features and their relationship with subtropical and typhoon, Acta Me teorologica Sinica, 48: 303–317.\nLuo Jian and Yu Shihua (1995), CEOF analysis of atmospheric low frequency Oscillation in lower latitude region and frequency modulation phenomena of low frequency signals, Acta Meteorologica Sinica, 9(2): 199–206.\nMadden R. D. and P. Julian (1971), Detection of a 40–50 day oscillation in the zonal wind in the tropical Pacific, J. Atmos. Sci., 28: 702–708.\nMadden R. D. and P. Julian (1972), Description of global scale circulation cells in the topic with 40–50 day period, J. Atmos. Sci., 29: 1109–1123.\nWang Pangxing et al. (1994), The direct display of the result of CEOF analysis, Journal of the Nanjing Meteorology Institute, 17(4): 448–454.\nYu Shihua, Yang Weiwu (1995), Diagnostic studies of intraseasonal anomalous advancement \u002F retreat of the subtropical high in Western Pacific, J. Trop. Meteor., 11: 214–222 (in Chinese).",{"VOID":1565},"10.1007\u002Fs00376-998-0043-3","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs00376-998-0043-3",[1568,1583],{"id":1569,"sortIndex":32,"researcher":28,"roles":1570,"affiliations":1571,"properties":1580,"displayName":1582,"givenName":28,"familyName":28},"8ecba01c-5fdb-484d-a903-24cb849fe749",[1009],[1572],{"id":1573,"sortIndex":32,"affiliation":1574,"properties":28},"a518436e-8243-461e-abd8-b9ab98166e83",{"id":1573,"createTime":28,"updateTime":28,"relativeEntities":1575,"slug":28,"properties":1576,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1579,"statistic":28},[],{"title":1577},{"VI":1578},"Meteorological Center, Nanjing Air Force, Nanjing",[],{"title":1581},{"VI":1582},"Zhang Jianwen",{"id":1584,"sortIndex":40,"researcher":28,"roles":1585,"affiliations":1586,"properties":1595,"displayName":1597,"givenName":28,"familyName":28},"8c474d11-4082-4f28-9e60-b06c696bc56a",[1009],[1587],{"id":1588,"sortIndex":32,"affiliation":1589,"properties":28},"6ac4fe67-4d92-407b-ac73-8cbc3a4f51c8",{"id":1588,"createTime":28,"updateTime":28,"relativeEntities":1590,"slug":28,"properties":1591,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1594,"statistic":28},[],{"title":1592},{"VI":1593},"Air Force Institute of Meteorology, Nanjing",[],{"title":1596},{"VI":1597},"Yu Shihua",{"url":1566,"publisher":1599,"properties":1635},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1600,"slug":872,"properties":1601,"entityType":25,"verifyStatus":878,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1604,"manageAffiliations":1609,"indexDatabases":1615,"url":28,"thumbnailPath":28,"statistic":1630,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1602,"title":1603},{"VOID":875},{"EN":877},[1605],{"id":881,"createTime":28,"updateTime":28,"relativeEntities":1606,"label":1607,"description":1608,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":884},{},[1610],{"id":888,"createTime":28,"updateTime":28,"relativeEntities":1611,"slug":28,"properties":1612,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1614,"statistic":28},[],{"title":1613},{"EN":892},[],[1616,1623],{"id":896,"indexDatabase":1617,"url":902,"indexYears":903,"academicFieldIds":1622,"indexDatabaseRanking":906},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1618,"label":1619,"description":1620,"key":781,"publicationTags":1621,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[905],{"id":908,"indexDatabase":1624,"url":920,"indexYears":28,"academicFieldIds":1629,"indexDatabaseRanking":28},{"id":910,"createTime":28,"updateTime":28,"relativeEntities":1625,"label":1626,"description":1627,"key":917,"publicationTags":1628,"standard":28},[],{"EN":913,"VI":913},{"EN":915,"VI":916},[919,813],[922],{"impactFactor":32,"impactFactorByYear":1631,"i10Index":570,"i10IndexLast5Year":140,"totalPublication":927,"totalPublicationByYear":1632,"totalCitation":934,"totalCitationByYear":1633,"totalCitationPerPublication":959,"totalCitationPerPublicationByYear":1634,"hindexLast5Year":141,"hindex":141},{"2012":52,"2013":423,"2014":229,"2015":121,"2016":422,"2017":346,"2018":422,"2019":170,"2020":225,"2021":289,"2022":925,"2023":926},{"1984":127,"1985":137,"1986":140,"1987":138,"1988":134,"1989":133,"1990":134,"1991":202,"1992":142,"1993":137,"1994":139,"1995":69,"1996":135,"1997":69,"1998":139,"1999":352,"2000":142,"2001":158,"2002":325,"2003":162,"2004":151,"2005":208,"2006":208,"2007":567,"2008":157,"2009":354,"2010":929,"2011":358,"2012":930,"2013":354,"2014":211,"2015":931,"2016":530,"2017":566,"2018":932,"2019":157,"2020":330,"2021":154,"2022":933,"2023":574,"2024":142},{"1984":145,"1985":48,"1986":357,"1987":199,"1988":45,"1989":936,"1990":937,"1991":47,"1992":201,"1993":938,"1994":354,"1995":130,"1997":939,"1998":129,"1999":940,"2000":941,"2001":942,"2002":599,"2003":943,"2004":944,"2005":945,"2006":946,"2007":947,"2008":599,"2009":604,"2010":948,"2011":949,"2012":950,"2013":951,"2014":952,"2015":953,"2016":954,"2017":955,"2018":956,"2019":957,"2020":435,"2021":701,"2022":958,"2023":933,"2024":48},{"1984":440,"1985":318,"1986":582,"1987":462,"1988":365,"1989":961,"1990":962,"1991":319,"1992":963,"1993":592,"1994":964,"1995":228,"1997":965,"1998":691,"1999":966,"2000":967,"2001":968,"2002":969,"2003":970,"2004":971,"2005":972,"2006":123,"2007":973,"2008":741,"2009":177,"2010":974,"2011":975,"2012":976,"2013":977,"2014":978,"2015":979,"2016":703,"2017":980,"2018":981,"2019":982,"2020":589,"2021":590,"2022":287,"2023":695,"2024":734},{"pages":1636,"volume":1638},{"VOID":1637},"247-257",{"VOID":1639},"15","1998-06-01",1998,[906,919],{"id":1644,"createTime":1645,"updateTime":1646,"relativeEntities":1647,"slug":1648,"properties":1649,"entityType":1002,"verifyStatus":26,"verifyTime":1646,"verifyNote":1003,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1658,"fullTextUrl":28,"authors":1659,"publicationType":1050,"publisherRelationship":1688,"citationCount":28,"citationInfo":28,"publishDate":1730,"publishYear":1731,"citationAnalyzeStatus":878,"lastCitationAnalyze":28,"indexDatabases":1732,"openAccess":28,"references":28,"isForceReanalyzing":1096},"01fe973c-563d-479f-974d-6e92ac993a91","2024-02-07T04:38:49.592+00:00","2025-01-07T22:01:30.250+00:00",[],"Comparison-of-Advanced-Technology-Microwave-Sounder-Biases-Estimated-Using-Radio-Occultation-and-Hurricane-Florence-2018-Captured-by-NOAA-20-and-S-NPP",{"abstract":1650,"title":1652,"references":1654,"doi":1656},{"EN":1651},"The second Advanced Technology Microwave Sounder (ATMS) was onboard the National Oceanic and Atmospheric Administration (NOAA)-20 satellite when launched on 18 November 2017. Using nearly six months of the earliest NOAA-20 observations, the biases of the ATMS instrument were compared between NOAA-20 and the Suomi National Polar-Orbiting Partnership (S-NPP) satellite. The biases of ATMS channels 8 to 13 were estimated from the differences between antenna temperature observations and model simulations generated from Meteorological Operational (MetOp)-A and MetOp-B satellites’ Global Positioning System (GPS) radio occultation (RO) temperature and water vapor profiles. It was found that the ATMS onboard the NOAA-20 satellite has generally larger cold biases in the brightness temperature measurements at channels 8 to 13 and small standard deviations. The observations from ATMS on both S-NPP and NOAA-20 are shown to demonstrate an ability to capture a less than 1-h temporal evolution of Hurricane Florence (2018) due to the fact that the S-NPP orbits closely follow those of NOAA-20.",{"EN":1653},"Comparison of Advanced Technology Microwave Sounder Biases Estimated Using Radio Occultation and Hurricane Florence (2018) Captured by NOAA-20 and S-NPP",{"VOID":1655},"Andersson, E., J. Pailleux, J.-N. Thepaut, J. R. Eyre, A. P. McNally, G. A. Kelly, and P. Courtier, 1994: Use of cloud-cleared radi¬ances in three\u002Ffour-dimensional variational data assimilation. Quart. J. Roy. Meteorol. Soc., 120, 627–653, https:\u002F\u002Fdoi.org\u002F10.1002\u002Fqj.49712051707.\nAngling, M., 2016: ROM SAF CDOP-2 visiting scientist report 28: A new software tool for reducing systematic residual ionospheric errors in GNSS-RO level 3 products, SAF\u002FROM\u002F DMI\u002FREP\u002FVS\u002F28.\nATBD, J. A., 2013: Joint Polar Satellite System (JPSS) Advanced Technology Microwave Sounder (ATMS) SDR Calibration Algorithm Theoretical Basis Document (ATBD), JPSS ATBD#1.\nCulverwell, I. D., H. W. Lewis, D. Offiler, C. Marquardt, and C. P. Burrows, 2015: The Radio Occultation Processing Pack-age, ROPP’. Atmospheric Measurement Techniques, 8, 1887–1899, https:\u002F\u002Fdoi.org\u002F10.5194\u002Famt-8-1887-2015.\nDerber, J. C, and W.-S. Wu, 1998: The use of TOVS cloud-cleared radiances in the NCEP SSI analysis system. Mon. Wea. Rev., 126, 2287–2299, https:\u002F\u002Fdoi.org\u002F10.1175\u002F1520-0493(1998)126\u003C2287:TUOTCC>2.0.CO;2.\nEyre, J. R., G. A. Kelly, A. P. McNally, E. Andersson, and A. Persson, 1993: Assimilation of TOVS radiance information through one-dimensional variational analysis. Quart. J. Roy. Meteorol. Soc, 119, 1427–1463, https:\u002F\u002Fdoi.org\u002F10.1002\u002Fqj.49711951411.\nGorbunov, M. E., K. B. Lauritsen, H.-H. Benzon, G. B. Larsen, S. Syndergaard, and M. B. Sørensen, 2011: Processing of GRAS\u002FMETOP radio occultation data recorded in closed-loop and raw-sampling modes. Atmospheric Measurement Techniques, 4, 1021–1026, https:\u002F\u002Fdoi.org\u002F10.5194\u002Famt-4-1021-2011.\nHealy, S. B., and J. R. Eyre, 2000: Retrieving temperature, water vapour and surface pressure information from refractive - index profiles derived by radio occultation: A simulation study. Quart. J. Roy. Meteorol. Soc, 126, 1661–1683, https:\u002F\u002Fdoi.org\u002F10.1002\u002Fqj.49712656606.\nKim, E., C. H. J. Lyu, K. Anderson, R. Vincent Leslie, and W. J. Blackwell, 2014: S-NPP ATMS instrument prelaunch and on-orbit performance evaluation. J. Geophys. Res., 119, 5653–5670, https:\u002F\u002Fdoi.org\u002F10.1002\u002F2013JD020483.\nKuo, Y.-H., T.-K. Wee, S. Sokolovskiy, C. Rocken, W. Schreiner, D. Hunt, and R. A. Anthes, 2004: Inversion and error estimation of GPS radio occultation data. J. Meteorol. Soc. Japan, 82, 507–531, https:\u002F\u002Fdoi.org\u002F10.2151\u002Fjmsj.2004.507.\nKursinski, E. R., G. A. Hajj, J. T. Schofield, R. P. Linfield, and K. R. Hardy, 1997: Observing Earth’s atmosphere with radio occultation measurements using the Global Positioning System. J. Geophys. Res., 102, 23429–23465, https:\u002F\u002Fdoi.org\u002F10.1029\u002F97JD01569.\nLiu, Q. H., Y. Xue, and C. Li, 2013: Sensor-based clear and cloud radiance calculations in the community radiative transfer model. Appl. Opt., 52, 4981–4990, https:\u002F\u002Fdoi.org\u002F10.1364\u002FAO.52.004981.\nNielsen, J. K., S. Syndergaard, and K. B. Lauritsen, 2016: NRT Level 2b and 2c lD-Var products (Metop-A: GRM-02, 03, 04, 05) (Metop-B: GRM-41, 42, 43, 44). ROM SAF CDOP-2.\nQin, Z., X. Zou, and F. Weng, 2012: Comparison between linear and nonlinear trends in NOAA-15 AMSU-A brightness tem-peratures during 1998–2010. Climate Dyn., 39, 1763–1779, https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00382-012-1296-1.\nTian, X. X., and X. L. Zou, 2016: ATMS- and AMSU-A-derived hurricane warm core structures using a modified retrieval al-gorithm. J. Geophys. Res., 121, 12630–12646, https:\u002F\u002Fdoi.org\u002F10.1002\u002F2016JD025O42.\nTian, X. X., and X. L. Zou, 2018: Capturing size and intensity changes of hurricanes irma and maria (2017) from polar-orbiting satellite microwave radiometers. J. Atmos. Sci., 75, 2509–2522, https:\u002F\u002Fdoi.org\u002F10.1175\u002FJAS-D-17-0315.1.\nTian, X. X., X. L. Zou, and S. P. Yang, 2018: A limb correction method for the microwave temperature sounder 2 and its ap-plications. Adv. Atmos. Sci., 35, 1547–1552, https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00376-018-8092-8.\nTian, X. X., and X. L. Zou, 2019: A comprehensive 4D-Var vortex initialization using a nonhydrostatic axisymmetric TC model with convection accounted for. Tellus A, 71, 1–15, https:\u002F\u002Fdoi.org\u002F10.1080\u002F16000870.2019.1653138.\nWang, X., and X. L. Zou, 2012: Quality assessments of Chinese FengYun-3B microwave temperature sounder (MWTS) measurements. IEEE Trans. Geosci. Remote Sens., 50, 4875–4884, https:\u002F\u002Fdoi.org\u002F10.1109\u002FTGRS.2012.2196438.\nWeng, F. Z., and Coauthors, 2013: Calibration of Suomi national polar-orbiting partnership advanced technology microwave sounder. J. Geophys. Res., 118, 11187–11200, https:\u002F\u002Fdoi.org\u002F10.1002\u002Fjgrd.50840.\nZou, X., and Z. Zeng, 2006: A quality control procedure for GPS radio occultation data. J. Geophys. Res., III, D02112, https:\u002F\u002Fdoi.org\u002F10.1029\u002F2005JD005846.\nZou, X. L., and X. X. Tian, 2018: Hurricane warm-core retrievals from AMSU-a and remapped atms measurements with rain contamination eliminated. J. Geophys. Res., 123, 10815–10829, https:\u002F\u002Fdoi.org\u002F10.1029\u002F2018JD028934.\nZou, X. L., H. Liu, and Y. H. Kuo, 2019: Occurrence and detection of impact multipath simulations of bending angle. Quart. J. Roy. Meteorol. Soc, 721, 1690–1704, https:\u002F\u002Fdoi.org\u002F10.1002\u002Fqj.3520.\nZou, X. L., and X. X. Tian, 2019: Comparison of ATMS striping noise between NOAA-20 and S-NPP and noise impact on warm core retrieval of Typhoon Jelawat (2018). IEEE Journal of Selected Topics in Applied Earth Observations and Re-mote Sensing, 12, 2504–2512, https:\u002F\u002Fdoi.org\u002F10.1109\u002FJSTARS.2019.2891683.\nZou, X., F. Weng, B. Zhang, L. Lin, Z. Qin, and V. Tallapragada, 2013: Impacts of assimilation of ATMS data in HWRF on track and intensity forecasts of 2012 four landfall hurricanes. J. Geophys. Res., 118, 11558–11576, https:\u002F\u002Fdoi.org\u002F10.1002\u002F2013JD020405.\nZou, X. L., L. Lin, and F. Z. Weng, 2014: Absolute calibration of ATMS upper level temperature sounding channels using GPS RO observations. IEEE Trans. Geosci. Remote Sens., 52, 1397–1406, https:\u002F\u002Fdoi.org\u002F10.1109\u002FTGRS.2013.2250981.",{"VOID":1657},"10.1007\u002Fs00376-019-9119-5","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs00376-019-9119-5",[1660,1675],{"id":1661,"sortIndex":32,"researcher":28,"roles":1662,"affiliations":1663,"properties":1672,"displayName":1674,"givenName":28,"familyName":28},"1c899338-0361-4fb2-8c13-23a4245c02f5",[1009],[1664],{"id":1665,"sortIndex":32,"affiliation":1666,"properties":28},"f94a4f43-d6b1-4f83-89c6-f3e49b9b942d",{"id":1665,"createTime":28,"updateTime":28,"relativeEntities":1667,"slug":28,"properties":1668,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1671,"statistic":28},[],{"title":1669},{"VI":1670},"Earth Science System Interdisciplinary Center, University of Maryland, College Park, USA",[],{"title":1673},{"VI":1674},"Xiaoxu Tian",{"id":1676,"sortIndex":40,"researcher":28,"roles":1677,"affiliations":1678,"properties":1685,"displayName":1687,"givenName":28,"familyName":28},"635a4655-f644-4488-a64f-de89da2327b1",[1009],[1679],{"id":1665,"sortIndex":32,"affiliation":1680,"properties":28},{"id":1665,"createTime":28,"updateTime":28,"relativeEntities":1681,"slug":28,"properties":1682,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1684,"statistic":28},[],{"title":1683},{"VI":1670},[],{"title":1686},{"VI":1687},"Xiaolei Zou",{"url":1658,"publisher":1689,"properties":1725},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1690,"slug":872,"properties":1691,"entityType":25,"verifyStatus":878,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1694,"manageAffiliations":1699,"indexDatabases":1705,"url":28,"thumbnailPath":28,"statistic":1720,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1692,"title":1693},{"VOID":875},{"EN":877},[1695],{"id":881,"createTime":28,"updateTime":28,"relativeEntities":1696,"label":1697,"description":1698,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":884},{},[1700],{"id":888,"createTime":28,"updateTime":28,"relativeEntities":1701,"slug":28,"properties":1702,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1704,"statistic":28},[],{"title":1703},{"EN":892},[],[1706,1713],{"id":896,"indexDatabase":1707,"url":902,"indexYears":903,"academicFieldIds":1712,"indexDatabaseRanking":906},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1708,"label":1709,"description":1710,"key":781,"publicationTags":1711,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[905],{"id":908,"indexDatabase":1714,"url":920,"indexYears":28,"academicFieldIds":1719,"indexDatabaseRanking":28},{"id":910,"createTime":28,"updateTime":28,"relativeEntities":1715,"label":1716,"description":1717,"key":917,"publicationTags":1718,"standard":28},[],{"EN":913,"VI":913},{"EN":915,"VI":916},[919,813],[922],{"impactFactor":32,"impactFactorByYear":1721,"i10Index":570,"i10IndexLast5Year":140,"totalPublication":927,"totalPublicationByYear":1722,"totalCitation":934,"totalCitationByYear":1723,"totalCitationPerPublication":959,"totalCitationPerPublicationByYear":1724,"hindexLast5Year":141,"hindex":141},{"2012":52,"2013":423,"2014":229,"2015":121,"2016":422,"2017":346,"2018":422,"2019":170,"2020":225,"2021":289,"2022":925,"2023":926},{"1984":127,"1985":137,"1986":140,"1987":138,"1988":134,"1989":133,"1990":134,"1991":202,"1992":142,"1993":137,"1994":139,"1995":69,"1996":135,"1997":69,"1998":139,"1999":352,"2000":142,"2001":158,"2002":325,"2003":162,"2004":151,"2005":208,"2006":208,"2007":567,"2008":157,"2009":354,"2010":929,"2011":358,"2012":930,"2013":354,"2014":211,"2015":931,"2016":530,"2017":566,"2018":932,"2019":157,"2020":330,"2021":154,"2022":933,"2023":574,"2024":142},{"1984":145,"1985":48,"1986":357,"1987":199,"1988":45,"1989":936,"1990":937,"1991":47,"1992":201,"1993":938,"1994":354,"1995":130,"1997":939,"1998":129,"1999":940,"2000":941,"2001":942,"2002":599,"2003":943,"2004":944,"2005":945,"2006":946,"2007":947,"2008":599,"2009":604,"2010":948,"2011":949,"2012":950,"2013":951,"2014":952,"2015":953,"2016":954,"2017":955,"2018":956,"2019":957,"2020":435,"2021":701,"2022":958,"2023":933,"2024":48},{"1984":440,"1985":318,"1986":582,"1987":462,"1988":365,"1989":961,"1990":962,"1991":319,"1992":963,"1993":592,"1994":964,"1995":228,"1997":965,"1998":691,"1999":966,"2000":967,"2001":968,"2002":969,"2003":970,"2004":971,"2005":972,"2006":123,"2007":973,"2008":741,"2009":177,"2010":974,"2011":975,"2012":976,"2013":977,"2014":978,"2015":979,"2016":703,"2017":980,"2018":981,"2019":982,"2020":589,"2021":590,"2022":287,"2023":695,"2024":734},{"pages":1726,"volume":1728},{"VOID":1727},"269-277",{"VOID":1729},"37","2020-02-12",2020,[906,919],{"id":1734,"createTime":1735,"updateTime":1736,"relativeEntities":1737,"slug":1738,"properties":1739,"entityType":1002,"verifyStatus":26,"verifyTime":1736,"verifyNote":1003,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1748,"fullTextUrl":28,"authors":1749,"publicationType":1050,"publisherRelationship":1779,"citationCount":28,"citationInfo":28,"publishDate":1820,"publishYear":1258,"citationAnalyzeStatus":878,"lastCitationAnalyze":28,"indexDatabases":1821,"openAccess":28,"references":28,"isForceReanalyzing":1096},"02310c0f-e85a-4040-a60e-1d90dac88e9c","2024-01-20T06:06:42.892+00:00","2025-02-01T16:07:29.014+00:00",[],"Latitudinal-and-Scan-dependent-Biases-of-Microwave-Humidity-Sounder-Measurements-and-Their-Dependences-on-Cloud-Ice-Water-Path",{"abstract":1740,"title":1742,"references":1744,"doi":1746},{"EN":1741},"The relationship between differences in microwave humidity sounder (MHS)–channel biases which represent measured brightness temperatures and model-simulated brightness temperatures, and cloud ice water path (IWP) as well as the influence of the cloud liquid water path (LWP) on the relationship is examined. Seven years (2011–17) of NOAA-18 MHS-derived measured brightness temperatures and IWP\u002FLWP data generated by the NOAA Comprehensive Large Array-data Stewardship System Microwave Surface and Precipitation Products System are used. The Community Radiative Transfer Model, version 2.2.4, is used to simulate model-simulated brightness temperatures using European Center for Medium-Range Weather Forecasts reanalysis data as background fields. Scan-angle deviations of the MHS window channel biases range from −1.7 K to 1.0 K. The relationships between channels 2, 4, and 5 biases and scan angle are symmetrical about the nadir. The latitude-dependent deviations of MHS window channel biases are positive and range from 0–7 K. For MHS non-window channels, the latitudinal deviations between measured brightness temperatures and model-simulated brightness temperatures are larger when the detection height is higher. No systematic warm or cold deviations are found in the global spatial distribution of difference between measured brightness temperatures and model-simulated brightness temperatures over oceans after removing scan-angle and latitudinal deviations. The corrected biases of five different MHS channels decrease differently with respect to the increase in IWP. This decrease is stronger when LWP values are higher.",{"EN":1743},"Latitudinal and Scan-dependent Biases of Microwave Humidity Sounder Measurements and Their Dependences on Cloud Ice Water Path",{"VOID":1745},"Auligné, T., A. P. McNally, and D. P. Dee, 2007: Adaptive bias correction for satellite data in a numerical weather prediction system. Quart. J. Roy. Meteor. Soc., 133, 631–642, https:\u002F\u002Fdoi.org\u002F10.1002\u002Fqj.56.\nChen, Y., F. Z. Weng, Y. Han, and Q. H. Liu, 2008: Validation of the community radiative transfer model by using CloudSat data. J. Geophys. Res., 113, D00A03, https:\u002F\u002Fdoi.org\u002F10.1029\u002F2007JD009561.\nChen, Y., Y. Han, P. Van Delst, and F. Z. Weng, 2010: On water vapor Jacobian in fast radiative transfer model. J. Geophys. Res., 115, D12303, https:\u002F\u002Fdoi.org\u002F10.1029\u002F2009JD013379.\nDee, D. P., 2005: Bias and data assimilation. Quart. J. Roy. Meteor. Soc., 131(613), 3323–3343, https:\u002F\u002Fdoi.org\u002F10.1256\u002Fqj.05.137.\nErrico, R. M., P. Bauer, and J. F. Mahfouf, 2007: Issues regarding the assimilation of cloud and precipitation data. J. Atmos. Sci., 64(11), 3785–3798, https:\u002F\u002Fdoi.org\u002F10.1175\u002F2006JAS2044.1.\nGeer, A. J., P. Bauer, and P. Lopez, 2010: Direct 4D-Var assimilation of all-sky radiances. Part II: Assessment. Quart. J. Roy. Meteor. Soc., 136(652), 1886–1905, https:\u002F\u002Fdoi.org\u002F10.1002\u002Fqj.681.\nHan, Y., F. Z. Weng, Q. H. Liu, and P. Van Delst, 2007: A fast radiative transfer model for SSMIS upper atmosphere sounding channels. J. Geophys. Res., 112, D11121, https:\u002F\u002Fdoi.org\u002F10.1029\u002F2006JD008208.\nHan, Y., P. Van Delst, Q. H. Liu, F. Z. Weng, B. H. Yan, R. Treadon, and J. Derber, 2006: JCSDA community radiative transfer Model (CRTM)—Version 1. NOAA Tech, Rep. NESDIS 122, 40 pp.\nJiang, J. H., and Coauthors. 2012: Evaluation of cloud and water vapor simulations in CMIP5 climate models using NASA “A-Train” satellite observations. J. Geophys. Res., 117, D14105, https:\u002F\u002Fdoi.org\u002F10.1029\u002F2011JD017237.\nLi, X., and X. L. Zou, 2017: Bias characterization of CrIS radiances at 399 selected channels with respect to NWP model simulations. Atmospheric Research, 196, 164–181, https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.atmosres.2017.06.007.\nMie, G., 1908: Contribution on the optics of turbid media, especially colloidal metal sols. Ann. Phys., 25, 377–442.\nQin, Z. K., and X. L. Zou, 2016: Development and initial assessment of a new land index for microwave humidity sounder cloud detection. J. Meteor. Res., 30(1), 12–37, https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs13351-016-5076-4.\nRoebeling, R. A., and I. Holleman, 2009: SEVIRI rainfall retrieval and validation using weather radar observations. J. Geophys. Res., 114, D21202. https:\u002F\u002Fdoi.org\u002F10.1029\u002F2009JD012102.\nSeto, S., N. Takahashi, and T. Iguchi, 2005: Rain\u002Fno-rain classification methods for microwave radiometer observations over land using statistical information for brightness temperatures under no-rain conditions. J. Appl. Meteor., 44(8), 1243–1259, https:\u002F\u002Fdoi.org\u002F10.1175\u002FJAM2263.1.\nThépaut, J. N., 2003: Satellite data assimilation in numerical weather prediction: An overview. Proceedings of ECMWF Seminar on Recent Developments in Data Assimilation for Atmosphere and Ocean, ECMWF, Reading, UK, 8–12 September 2003, 75–96.\nWeng, F. Z., 2007: Advances in radiative transfer modeling in support of satellite data assimilation. J. Atmos. Sci., 64, 3799–3807, https:\u002F\u002Fdoi.org\u002F10.1175\u002F2007JAS2112.1.\nWeng, F. Z., and N. C. Grody, 1994: Retrieval of cloud liquid water using the special sensor microwave imager (SSM\u002FI). J. Geophys. Res., 99(D12), 25 535–25 551, https:\u002F\u002Fdoi.org\u002F10.1029\u002F94JD02304.\nWeng, F. Z., and N. C. Grody, 2000: Retrieval of ice cloud parameters using a microwave imaging radiometer. J. Atmos. Sci., 57(8), 1069–1081, https:\u002F\u002Fdoi.org\u002F10.1175\u002F1520-0469(2000)057\u003C1069:ROICPU>2.0.CO;2.\nWeng, F. Z., N. C. Grody, R. Ferraro, A. Basist, and D. Forsyth, 1997: Cloud liquid water climatology from the Special Sensor Microwave\u002FImager. J. Climate, 10(5), 1086–1098, https:\u002F\u002Fdoi.org\u002F10.1175\u002F1520-0442(1997)010\u003C1086:CLWCFT>2.0.CO;2.\nWeng, F. Z., L. M. Zhao, R. R. Ferraro, G. Poe, X. F. Li, and N. C. Grody, 2003: Advanced microwave sounding unit cloud and precipitation algorithms. Radio Sci., 38(4), 8068, https:\u002F\u002Fdoi.org\u002F10.1029\u002F2002RS002679.\nWeng, F., X. Zou, X. Wang, S. Yang, and M. D. Goldberg, 2012: Introduction to Suomi National Polar-Orbiting Partnership advanced technology microwave sounder for numerical weather prediction and tropical cyclone applications. J. Geophys. Res., 117, D19112, https:\u002F\u002Fdoi.org\u002F10.1029\u002F2012jd018144.\nXue, J. S., 2009: Scientific issues and perspective of assimilation of meteorological satellite data. Acta Meteorologica Sinica, 67(6), 903–911, https:\u002F\u002Fdoi.org\u002F10.11676\u002Fqxxb2009.088. (in Chinese with English abstract)\nZou, X. L., Z. K. Qin, and F. Z. Weng, 2013: Improved quantitative precipitation forecasts by MHS radiance data assimilation with a newly added cloud detection algorithm. Mon. Wea. Rev., 141, 3203–3221, https:\u002F\u002Fdoi.org\u002F10.1175\u002FMWR-D-13-00009.1.",{"VOID":1747},"10.1007\u002Fs00376-019-8190-2","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs00376-019-8190-2",[1750,1765],{"id":1751,"sortIndex":32,"researcher":28,"roles":1752,"affiliations":1753,"properties":1762,"displayName":1764,"givenName":28,"familyName":28},"f817fe42-f8b0-4e75-b91c-d304f7661315",[1009],[1754],{"id":1755,"sortIndex":32,"affiliation":1756,"properties":28},"81ae4ad5-66db-4f09-899f-3d9fd85e3c42",{"id":1755,"createTime":28,"updateTime":28,"relativeEntities":1757,"slug":28,"properties":1758,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1761,"statistic":28},[],{"title":1759},{"VI":1760},"Joint Center of Data Assimilation for Research and Applications, Nanjing University of Information Science and Technology, Nanjing, China",[],{"title":1763},{"VI":1764},"Anqi Cai",{"id":1766,"sortIndex":40,"researcher":28,"roles":1767,"affiliations":1768,"properties":1777,"displayName":1687,"givenName":28,"familyName":28},"a079e00c-a1a4-4bed-b0de-b4b43999615d",[1009],[1769],{"id":1770,"sortIndex":32,"affiliation":1771,"properties":28},"11f3961f-0e10-4b32-99a3-a6ad9587edbd",{"id":1770,"createTime":28,"updateTime":28,"relativeEntities":1772,"slug":28,"properties":1773,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1776,"statistic":28},[],{"title":1774},{"VI":1775},"Earth System Science Interdisciplinary Center, University of Maryland, College Park, USA",[],{"title":1778},{"VI":1687},{"url":1748,"publisher":1780,"properties":1816},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1781,"slug":872,"properties":1782,"entityType":25,"verifyStatus":878,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1785,"manageAffiliations":1790,"indexDatabases":1796,"url":28,"thumbnailPath":28,"statistic":1811,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1783,"title":1784},{"VOID":875},{"EN":877},[1786],{"id":881,"createTime":28,"updateTime":28,"relativeEntities":1787,"label":1788,"description":1789,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":884},{},[1791],{"id":888,"createTime":28,"updateTime":28,"relativeEntities":1792,"slug":28,"properties":1793,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1795,"statistic":28},[],{"title":1794},{"EN":892},[],[1797,1804],{"id":896,"indexDatabase":1798,"url":902,"indexYears":903,"academicFieldIds":1803,"indexDatabaseRanking":906},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1799,"label":1800,"description":1801,"key":781,"publicationTags":1802,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[905],{"id":908,"indexDatabase":1805,"url":920,"indexYears":28,"academicFieldIds":1810,"indexDatabaseRanking":28},{"id":910,"createTime":28,"updateTime":28,"relativeEntities":1806,"label":1807,"description":1808,"key":917,"publicationTags":1809,"standard":28},[],{"EN":913,"VI":913},{"EN":915,"VI":916},[919,813],[922],{"impactFactor":32,"impactFactorByYear":1812,"i10Index":570,"i10IndexLast5Year":140,"totalPublication":927,"totalPublicationByYear":1813,"totalCitation":934,"totalCitationByYear":1814,"totalCitationPerPublication":959,"totalCitationPerPublicationByYear":1815,"hindexLast5Year":141,"hindex":141},{"2012":52,"2013":423,"2014":229,"2015":121,"2016":422,"2017":346,"2018":422,"2019":170,"2020":225,"2021":289,"2022":925,"2023":926},{"1984":127,"1985":137,"1986":140,"1987":138,"1988":134,"1989":133,"1990":134,"1991":202,"1992":142,"1993":137,"1994":139,"1995":69,"1996":135,"1997":69,"1998":139,"1999":352,"2000":142,"2001":158,"2002":325,"2003":162,"2004":151,"2005":208,"2006":208,"2007":567,"2008":157,"2009":354,"2010":929,"2011":358,"2012":930,"2013":354,"2014":211,"2015":931,"2016":530,"2017":566,"2018":932,"2019":157,"2020":330,"2021":154,"2022":933,"2023":574,"2024":142},{"1984":145,"1985":48,"1986":357,"1987":199,"1988":45,"1989":936,"1990":937,"1991":47,"1992":201,"1993":938,"1994":354,"1995":130,"1997":939,"1998":129,"1999":940,"2000":941,"2001":942,"2002":599,"2003":943,"2004":944,"2005":945,"2006":946,"2007":947,"2008":599,"2009":604,"2010":948,"2011":949,"2012":950,"2013":951,"2014":952,"2015":953,"2016":954,"2017":955,"2018":956,"2019":957,"2020":435,"2021":701,"2022":958,"2023":933,"2024":48},{"1984":440,"1985":318,"1986":582,"1987":462,"1988":365,"1989":961,"1990":962,"1991":319,"1992":963,"1993":592,"1994":964,"1995":228,"1997":965,"1998":691,"1999":966,"2000":967,"2001":968,"2002":969,"2003":970,"2004":971,"2005":972,"2006":123,"2007":973,"2008":741,"2009":177,"2010":974,"2011":975,"2012":976,"2013":977,"2014":978,"2015":979,"2016":703,"2017":980,"2018":981,"2019":982,"2020":589,"2021":590,"2022":287,"2023":695,"2024":734},{"pages":1817,"volume":1819},{"VOID":1818},"557-569",{"VOID":1256},"2019-03-23",[906,919],{"id":1823,"createTime":1824,"updateTime":1825,"relativeEntities":1826,"slug":1827,"properties":1828,"entityType":1002,"verifyStatus":26,"verifyTime":1825,"verifyNote":1003,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1837,"fullTextUrl":28,"authors":1838,"publicationType":1050,"publisherRelationship":1902,"citationCount":28,"citationInfo":28,"publishDate":1944,"publishYear":1945,"citationAnalyzeStatus":878,"lastCitationAnalyze":28,"indexDatabases":1946,"openAccess":28,"references":28,"isForceReanalyzing":1096},"0247baa0-f75e-4b93-ade9-7c738c6e5e9f","2024-01-26T17:29:33.328+00:00","2025-02-14T19:33:46.368+00:00",[],"Approximations-of-the-scattering-phase-functions-of-particles",{"abstract":1829,"title":1831,"references":1833,"doi":1835},{"EN":1830},"Based on anomalous diffraction theory and the modified Rayleigh-Debye approximation, a physically realistic model in bridging form is described to approximate the scattering phase function of particles. When compared with the exact method, the bridging technique reported here provides a reasonable approximation to the Mie results over a broader range of angles and size parameters, and it demonstrates the advantage of being computationally economic. In addition, the new phase function model can be essentially extended to other shapes and conveniently used in more complicated scattering and emission problems related to the solutions of the radiative transfer equations.",{"EN":1832},"Approximations of the scattering phase functions of particles",{"VOID":1834},"Acquista, C., 1976: Light scattering by tenuous particles: A generalization of the Rayleigh-Gans-Rocard approach. Applied Optics, 15, 2932–2936.\nBourrly, C., P. Chiappetta, and T. Lemaire, 1989: Electromagnetic scattering by large rotating particles in the eikonal formalism. Optics Communications, 70, 173–176.\nCaldas, M., and V. Semião, 2001: A new approximate phase function for isolated particles and polydispersions. Journal of Quantitative Spectroscopy & Radiative Transfer, 68, 521–542.\nChen, T. W., 1984: Generalized eikonal approximation. Physical Review (C), 30, 585–592.\nChu, C. M., and S. W. Churchill, 1955: Representation of the angular distribution of radiation scattered by a spherical particle. Journal of the Optical Society of America, 45, 958–962.\nChylek, P., and J. D. Klett, 1991a: Absorption and scattering of electromagnetic radiation by prismatic columns: Anomalous diffraction approximation. Journal of the Optical Society of America, A8, 1713–1720.\nChylek, P., and J. D. Klett, 1991b: Extinction cross section of nonspherical particles in the anomalous diffraction approximation. Journal of the Optical Society of America, A8, 274–281.\nCornette, W. M., and J. G. Shanks, 1992: Physically reasonable analytic expression for the single-scattering phase function. Applied Optics, 31, 3152–3160.\nDraine, B. T., 2003: Scattering by interstellar dust grains. I. Optical and ultraviolet. Astrophysical Journal, 598, 1017–1035.\nFournier, G. R, and B. T. N. Evans, 1991: Approximation to extinction efficiency for randomly oriented spheroids. Applied Optics, 30, 2042–2048.\nFournier, G. R., and J. L. Forand, 1994: Analytic phase function for ocean water. Proceedings of the International Society for Optical Engineering (SPIE), Vol. 2258, Ocean Optics XII, J. S. Jaffe, Ed., 194–201pp.\nFournier, G. R., and B. T. N. Evans, 1996: Approximation to extinction efficiency from randomly oriented circular and elliptical cylinders. Applied Optics, 35, 4271–4282.\nGreeberg, J. M., and A. S. Meltzer, 1960: Scattering by nonspherical particles. Journal of Applied Physics, 31, 82–84.\nGordon, J. E., 1985: Simple method for approximating Mie scattering. Journal of the Optical Society of America, A2, 156–159.\nGross, D. A., and P. Latimer, 1970: General solutions for the extinction and absorption efficiency of arbitrary oriented cylinders by anomalous diffraction approximation methods. Journal of the Optical Society of America, 60, 904–907.\nHenyey, L. C., and J. L. Greenstein, 1941: Diffuse radiation in the galaxy. Astrophysical Journal, 93, 70–83.\nIrvine, W. M., 1965: Multiple scattering by large particles. Astrophysical Journal, 142, 1563–1575.\nKahnert, F. M., 2003: Numerical methods in electromagnetic scattering theory. Journal of Quantitative Spectroscopy & Radiative Transfer, 79–80, 775–824.\nKattawar, G. W., 1975: A three-parameter analytic phase function for multiple scattering calculations. Journal of Quantitative Spectroscopy & Radiative Transfer, 15, 839–849.\nKhlebtsov, N. G., 1984: Integral equation for problems of light scattering matrix for soft spheroids comparable in size with the wavelength of light. Optics & Spectroscopy, 46, 292–295.\nKhlebtsov, N. G., and A. G. Melnikov, 1991: Integral equation for light scattering problems: Application to the orientationally induced birefringence of colloidal dispersions. Journal of Colloid and Interface Science, 142, 396–408.\nKhlebtsov, N. G., A. G. Melnikov, and V. A. Bogatyrev, 1991: The linear dichroism and birefringence of colloidal dispersions: Approximate and exact approaches. Journal of Colloid and Interface Science, 146, 463–478.\nKlett, J. D., and R. A. Sutherland, 1992: Approximate methods for modeling the scattering properties of non-spherical particles: Evaluation of the Wentzel-Kramers-Brillouin method. Applied Optics, 31, 373–386.\nLiou, K. N., 2002: An Introduction to Atmospheric Radiation. 2nd ed. Academic, San Diego, 169–252.\nLiu, P., 1994: A new phase function approximating to Mie scattering for radiative transport equations. Physics in Medicine and Biology, 39, 1025–1036.\nLiu, Y., W. P. Arnott, and J. Hallet, 1998: Anomalous diffraction theory for arbitrarily oriented finite circular cylinders and comparison with exact T-matrix results. Applied Optics, 37, 5019–5030.\nMaslowska, A., P. J. Flatau, and G. L. Stephen, 1994: On the validity of the anomalous diffraction theory to light scattering by cubes. Optics Communications, 107, 35–40.\nMcKellar, B. H. J., and M. A. Box, 1981: The scaling group of the radiative transfer equation. J. Atmos. Sci., 38, 1063–1068.\nMeeten, G. H., 1982: An anomalous diffraction theory of linear birefringence and dichroism in colloidal dispersions. Journal of Colloid and Interface Science, 87, 407–415.\nMishchenko, M. I., W. J. Wiscombe, J. W. Hovenier, and L. D. Travis, 2000: Overview of scattering by nonspherical particles. Light Scattering by Nonspherical Particles: Theory, Measurements, and Applications. M. I. Mishchenko et al., Eds., Academic, San Diego, 29–60.\nModest, M. F., 2003: Radiative Heat Transfer. 2nd ed. Academic, New York, 362–368.\nMuinouen, K., 1996: Light scattering by Gaussian random particles: Rayleigh and Rayleigh—Gans approximations. Journal of Quantitative Spectroscopy & Radiative Transfer, 55, 603–613.\nNapper, D. H., 1967: A diffraction theory approach to the total scattering by cubes. Colloid & Polymer Science, 218, 41–46.\nPerrin, J. M., and P. Chiappetta, 1985: Light scattering by large particles, I: A new theoretical description in the eikonal picture. Optica Acta, 32, 907–921.\nPerrin, J. M., and P. Chiappetta, 1986: Light scattering by large particles, II: A vectorical description in the eikonal picture. Optica Acta, 33, 1001–1022.\nReynolds, L. O., and N. J. McCormick, 1980: Approximate two-parameter phase function for light scattering. Journal of the Optical Society of America, 70, 1206–1212.\nSaxon, D. S., 1955: Lectures on the scattering of light. Scientific Report No.9 Contract AF19 (122)–239, Meteorology Department, Univ. California, Los Angeles, 51–62.\nSharma, S. K., and A. K. Roy, 2000: New approximate phase functions: Test for nonspherical particles. Journal of Quantitative Spectroscopy & Radiative Transfer, 64, 327–337.\nSharma, S. K., A. K. Roy, and D. J. Somerford, 1998: New approximate phase functions for scattering of unpolarized light by dielectric particles. Journal of Quantitative Spectroscopy & Radiative Transfer, 60, 1001–1010.\nShimizu, K., 1983: Modification of the Rayleigh-Debye approximation. Journal of the Optical Society of America, 73, 504–507.\nStreekstra, G. J., A. G. Hooekstra, and R. M. Heethaar, 1994: Anomalous diffraction by arbitrarily oriented ellipsoids: Application in ektacytometry. Applied Optics, 33, 7288–7296.\nSun, W., and Q. Fu, 2001: Anomalous diffraction theory for arbitrarily oriented hexagonal crystals. Journal of Quantitative Spectroscopy & Radiative Transfer, 63, 727–737.\nVan de Hulst, H. C., 1957: Light Scattering by Small Particles. John Wiley & Sons, New York, 172–195pp.\nWriedt, T., 1998: A review of elastic light scattering theories. Particle & Particle Systems Characterization, 15, 67–74.\nXu, M., and R. R. Alfano, 2003: Anomalous diffraction of light with geometrical path statistics of rays and a Gaussian ray approximation. Optics Letters, 28(3), 179–181.\nZhao, J.-Q., 2003: Light scattering by arbitrary shaped particles. Ph. D. dissertation, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, 49–50.\nZhao, J.-Q., and Y.-Q. Hu, 2003: Bridging technique for calculating the extinction efficiency of arbitrary shaped particles. Applied Optics, 42, 4937–45.",{"VOID":1836},"10.1007\u002Fs00376-006-0802-y","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs00376-006-0802-y",[1839,1863,1876,1889],{"id":1840,"sortIndex":32,"researcher":28,"roles":1841,"affiliations":1842,"properties":1860,"displayName":1862,"givenName":28,"familyName":28},"c7881191-894f-497d-9ed5-3d2f3f93dc1e",[1009],[1843,1851],{"id":1844,"sortIndex":32,"affiliation":1845,"properties":28},"548d1b85-733a-41e9-8425-33eb77d676c3",{"id":1844,"createTime":28,"updateTime":28,"relativeEntities":1846,"slug":28,"properties":1847,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1850,"statistic":28},[],{"title":1848},{"VI":1849},"State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 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investigate the Madden–Julian Oscillation (MJO) signal in wintertime stratospheric ozone over the Tibetan Plateau and East Asia using the harmonized dataset of satellite ozone profiles. Two different MJO indices—the all-season Real-Time multivariate MJO index (RMM) and outgoing longwave radiation-based MJO index (OMI)—are used to compare the MJO-related ozone anomalies. The results show that there are pronounced eastward-propagating MJO-related stratospheric ozone anomalies (mainly within 20–200 hPa) over the subtropics. The negative stratospheric ozone anomalies are over the Tibetan Plateau and East Asia in MJO phases 4–7, when MJO-related tropical deep convective anomalies move from the equatorial Indian Ocean towards the western Pacific Ocean. Compared with the results based on RMM, the MJO-related stratospheric column ozone anomalies based on OMI are stronger and one phase ahead. Further analysis suggests that different sampling errors, observation principles and retrieval algorithms may be responsible for the discrepancies among different satellite measurements. The MJO-related stratospheric ozone anomalies can be attributed to the MJO-related circulation anomalies, i.e., the uplifted tropopause and the northward shifted westerly jet in the upper troposphere. Compared to the result based on RMM, the upper tropospheric westerly jet may play a less important role in generating the stratospheric column ozone anomalies based on OMI. Our study indicates that the circulation-based MJO index (RMM) can better characterize the MJO-related anomalies in tropopause pressure and thus the MJO influence on atmospheric trace gases in the upper troposphere and lower stratosphere, especially over subtropical East Asia.",{"EN":1957},"Satellite measurements of the Madden–Julian oscillation in wintertime stratospheric ozone over the Tibetan Plateau and East Asia",{"VOID":1959},"Bertaux, J. L., and Coauthors, 2010: Global ozone monitoring by occultation of stars: An overview of GOMOS measurements on ENVISAT. Atmos. Chem. Phys., 10, 12091–12148, doi: 10.5194\u002Facp-10–12091-2010.\nDee, D. P., and Coauthors, 2011: The ERA-Interim reanalysis: configuration and performance of the data assimilation system. Quart. J. Roy. Meteor. Soc., 137, 553–597, doi: 10.1002\u002F qj.828.\nFischer, H., and Coauthors, 2008: MIPAS: An instrument for atmospheric and climate research. Atmos. Chem. Phys., 8, 2151–2188, doi: 10.5194\u002Facp-8–2151-2008.\nGarfinkel, C. I., S. B. Feldstein, D. W. Waugh, C. Yoo, and S. Lee, 2012: Observed connection between stratospheric sudden warmings and the Madden–Julian Oscillation. Geophys. Res. Lett., 39, L18807, doi: 10.1029\u002F2012GL053144.\nGao, X. H., and J. L. Stanford 1990: Low-frequency oscillations in total ozone measurements. J. Geophys. Res., 95, 13797–13806.\nKiladis, G. N., J. Dias, K. H. Straub, M. C. Wheeler, S. N. Tulich, K. Kikuchi, K. M. Weickmann, and M. J. Ventrice, 2014: A comparison of OLR and circulation-based indices for tracking the MJO. Mon. Wea. Rev., 142, 1697–1715. doi: http:\u002F\u002Fdx.doi. org\u002F10.1175\u002FMWR-D-13-00301.1.\nKyröla, E., and Coauthors, 2004: GOMOS on Envisat: an overview. Advances in Space Research, 33, 1020–1028.\nLau, W. K.-M., and D. E. Waliser, 2012: Intraseasonal Variability in the Atmosphere-ocean Climate System. 2nd ed. Springer, Heidelberg, Germany, 581 pp.\nLi, K.-F., B. Tian, D. E. Waliser, M. J. Schwartz, J. L. Neu, J. R. Worden, and Y. L. Yung, 2012: Vertical structure of MJOrelated subtropical ozone variations from MLS, TES, and SHADOZ data. Atmos. Chem. Phys., 12, 425–436.\nLiebman, B., and C. A. Smith, 1996: Description of a complete (interpolated) outgoing longwave radiation dataset. Bull. Amer. Meteor. Soc., 77, 1275–1277.\nLiu, C. X., Y. Liu, Z. N. Cai, S. T. Gao, D. R. Lu, and E. Kyrola, 2009: A Madden-Julian Oscillation-triggered record ozone minimum over the Tibetan Plateau in December 2003 and its association with stratospheric “low-ozone pockets”. Geophys. Res. Lett., 36, L15830, doi: 10.1029\u002F2009GL039025.\nLiu, C. X., Y. Liu, Z. N. Cai, S. T. Gao, J. C. Bian, X. Liu, and K. Chance, 2010: Dynamic formation of extreme ozone minimum events over the Tibetan Plateau during northern winters 1987–2001. J. Geophys. Res., 115, D18311, doi: 10.1029\u002F2009JD013130.\nLiu, C. X., B. J. Tian, K.-F. Li, G. L. Manney, N. J. Liversey, Y. L. Yung, and D. E. Waliser, 2014: Northern Hemisphere mid-winter vortex-displacement and vortex-split stratospheric sudden warmings: Influence of the Madden-Julian Oscillation and Quasi-Biennial Oscillation. J. Geophys. Res., 119, 12599–12620, doi: 10.1002\u002F2014JD021876.\nMadden, R. A., and P. R. Julian, 1971: Detection of a 40–50 day oscillation in the zonal wind in the tropical Pacific. J. Atmos. Sci., 28, 702–708.\nMadden, R. A., and P. R. Julian, 1972: Description of global-scale circulation cells in the tropics with a 40–50 day period. J. Atmos. Sci., 29, 1109–1123.\nRahpoe, N., C. von Savigny, M. Weber, A. V. Rozanov, H. Bovensmann, and J. P. Burrows, 2013: Error budget analysis of SCIAMACHY limb ozone profile retrievals using the SCIATRAN model. Atmospheric Measurement Techniques, 6, 2825–2837, doi: 10.5194\u002Famt-6-2825-2013.\nSabutis, J. L., J. L. Stanford, and K. P. Bowman, 1987: Evidence for 35-50 day low frequency oscillations in total ozone mapping spectrometer data. Geophys. Res. Lett., 14, 945–947.\nSofieva, V. F., and Coauthors, 2013: Harmonized dataset of ozone profiles from satellite limb and occultation measurements. Earth System Science Data, 5, 349–363, doi: 10.5194\u002Fessd-5-349-2013.\nTamminen, J., and Coauthors, 2010: GOMOS data characterisation and error estimation. Atmos. Chem. Phys., 10, 9505–9519, doi: 10.5194\u002Facp-10–9505-2010.\nTian, B. J., Y. L. Yung, D. E. Waliser, T. Tyranowski, L. Kuai, E. J. Fetzer, and F. W. Irion, 2007: Intraseasonal variations of the tropical total ozone and their connection to the Madden-Julian Oscillation. Geophys. Res. Lett., 34, L08704, doi: 10.1029\u002F2007GL029451.\nTian, B. J., D. E. Waliser, R. A. Kahn, and S. Wong, 2011: Modulation of Atlantic aerosols by the Madden-Julian Oscillation. J. Geophys. Res., 116, D15108, doi: 10.1029\u002F2010JD015201.\nTian, B., and D. E. Waliser, 2012: Chemical and biological impacts. Intraseasonal Variability in the Atmosphere-Ocean Climate System, 2nd ed., W. K. M. Lau and D. E. Waliser, Eds., Springer-Verlag, Berlin, Heidelberg, 569–585.\nVentrice, M. J., M. C. Wheeler, H. H. Hendon, C. J. Schreck III, C. D. Thorncroft, and G. N. Kiladis, 2013: A modified multivariate Madden-Julian Oscillation index using velocity potential. Mon. Wea. Rev., 141, 4197–4210, doi: 10.1175\u002FMWR-D-12–00327.1.\nWaliser, D. E., 2012: Predictability and forecasting. Intraseasonal Variability in the Atmosphere-Ocean Climate System. 2nd ed., W. K. M. Lau and D. E. Waliser, Eds., Springer-Verlag, Berlin, Heidelberg, 433–476.\nWheeler, M. C., and H. H. Hendon, 2004: An all-season real-time multivariate MJO index: Development of an index for monitoring and prediction. Mon. Wea. Rev., 132, 1917–1932.\nZhang, C. D., 2005: Madden-Julian Oscillation. Rev. Geophys., 43, RG2003, doi: 10.1029\u002F2004RG000158.\nZhang, C. D., 2013: Madden-Julian Oscillation: Bridging weather and climate. Bull. Amer. Meteor. 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Houghton et al., Cambridge University Press, 572 pp.",{"id":28,"text":2207,"url":28,"identifiers":28},"Ma Zhuguo, 1999: The relationship between the soil moisture and climate variability over East China and a model used for retrieving soil moisture, Ph. D. Thesis, Institute of Atmospheric Physics, Chinese Academy of Sciences, 121 pp (in Chinese).",{"id":28,"text":2209,"url":28,"identifiers":28},"Parkinson, C. L., and W. M. Washington, 1979: A large—scale numerical model of sea ice. J. Geophys. Res., 84, 311–337.",{"id":28,"text":2211,"url":28,"identifiers":28},"Semtner, Jr. A. J., 1976: A model for the thermodynamic growth of sea ice in numerical investigations of climate. J. Phys. Oceanogr., 6, 379–389.",{"id":28,"text":2213,"url":28,"identifiers":28},"Shea, D. 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