文献类型：期刊文献

英文题名：Impact of Intraseasonal Oscillations on the Activity of Tropical Cyclones in Summer Over the South China Sea: Nonlocal Tropical Cyclones

作者：Ling, Zheng[1,2];Wang, Yuqing[3,4];Wang, Guihua[5];He, Hailun[2]

机构：[1]Guangdong Ocean Univ, Coll Ocean & Meteorol, Zhanjiang, Peoples R China;[2]Minist Nat Resources, State Key Lab Satellite Ocean Environm Dynam, Inst Oceanog 2, Hangzhou, Peoples R China;[3]Univ Hawaii Manoa, Sch Ocean & Earth Sci & Technol, Dept Atmospher Sci, Honolulu, HI 96822 USA;[4]Univ Hawaii Manoa, Sch Ocean & Earth Sci & Technol, Int Pacific Res Ctr, Honolulu, HI 96822 USA;[5]Fudan Univ, Dept Atmospher & Ocean Sci, Inst Atmospher Sci, Shanghai, Peoples R China

年份：2020

卷号：8

外文期刊名：FRONTIERS IN EARTH SCIENCE

收录：SCI-EXPANDED(收录号：WOS:000603395500001)、、EI(收录号：20212810638692)、Scopus(收录号：2-s2.0-85098495685)、WOS

基金：This study was supported by the China Ocean Mineral Resources Research and Development Association Program (DY135-E2-301), the National Key Research and Development Program of China (2019YFC1510100), Natural science team program of Guangdong (2016A030312004), National program on Global Change and Air-Sea interaction (GASI-02-SCS-YGST2-02), Project of Enhancing School with Innovation of Guangdong Ocean University (GDOU2016050240) and program for scientific research start-up funds of Guangdong Ocean University (R17073). The Japan Meteorological Agency best track TC dataset was downloaded from http://www.jma.go.jp/jma/jma-eng/jma-center/rsmc-hp-pub-eg/besttrack.html.The ERA-Interim data were downloaded from http://apps.ecmwf.int/datasets/.The OLR data were downloaded from http://www.esrl.noaa.gov/psd/.

语种：英文

外文关键词：South China Sea; tropical cyclones; Madden-Julian oscillation; quasi-biweekly oscillation; western pacific subtropical high

外文摘要：In addition to tropical cyclones (TCs) locally formed in the South China Sea (SCS), there are also TCs that initially form over the Northwest Pacific (NWP) and move westward to enter the SCS (often called nonlocal TCs). It is unclear how those nonlocal TCs are modulated by the intraseasonal climate variability. In this study, the impacts of two types of intraseasonal oscillations, namely the Madden-Julian Oscillation (MJO) and the quasi-biweekly oscillation (QBWO), on nonlocally formed TCs over the SCS in summer (May-September) are analyzed based on best-track TC data and global reanalysis during 1979-2018. Results show that in the convective phases of both MJO and QBWO, the western Pacific subtropical high shifted more eastward, and more TCs entered the SCS. This is mainly because more TCs formed in the NWP in the convective phases of intraseasonal oscillations and the genesis locations of the NWP TCs shifted westward and closer to the SCS. In addition to TC count, intraseasonal oscillations also affected the intensity of nonlocal TCs entered the SCS, with the influence of QBWO being more significant than MJO. In the convectively active phases of QBWO (phases 2-5), 34 nonlocal TCs reached typhoon intensity, while only two nonlocal TCs reached typhoon intensity in the convectively inactive phases (phases 1, 6, 7, 8). Further analysis indicates that nonlocal TCs often moved with the northwestward propagating convective signals of QBWO, resulting in more and stronger TCs that entered the SCS in the convective phases of QBWO. The mean location that the nonlocal TC entered the SCS also shifted northward with the northward propagation of intraseasonal oscillations.