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Associations between the Western North Pacific Monsoon and the South China Sea Monsoon


doi: 10.1007/s00376-002-0030-z

  • Based on the interannual variability of convection over the tropical western North Pacific (WNP), a region of 130°-160°E, 10°-20°N, a composite analysis is performed on the fields of surface temperature,outgoing longwave radiation and 850 hPa zonal wind. The composite results show that the weaker (stronger) WNP convection is related to the El Nino (La Nina)-pattern sea surface temperature (SST)anomalies in the preceding winter and in spring. A comparison with previous results indicates that a similar spatial and temporal distribution of SST anomalies is also associated with the onsets of both the WNP and South China Sea (SCS) monsoons.The composite results also show that the weaker (stronger) convection over the WNP corresponds to the easterly (westerly) anomalies that extend westward from the WNP into the Bay of Bengal. A numerical experiment by an atmospheric general circulation model shows a similar result. In addition, during weaker (stronger) convection summer, the convection over the WNP and lower-level zonal winds over the SCS exhibit a small (large) extent of seasonal evolution.
  • [1] Xinyu LI, Riyu LU, 2019: Seesaw Pattern of Rainfall Anomalies between the Tropical Western North Pacific and Central Southern China during Late Summer, ADVANCES IN ATMOSPHERIC SCIENCES, 36, 261-270.  doi: 10.1007/s00376-018-8130-6
    [2] Liu Qinyu, Jia Yinglai, Wang Xiaohua, Yang Haijun, 2001: On the Annual Cycle Characteristics of the Sea Surface Height in South China Sea, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 613-622.  doi: 10.1007/s00376-001-0049-6
    [3] Zhang Renhe, Zhao Gang, Tan Yanke, 2001: Meridional Wind Stress Anomalies over Tropical Pacific and the Onset of El Nino. Part Ⅰ: Data Analysis, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 467-480.  doi: 10.1007/s00376-001-0038-9
    [4] WANG Xin, ZHOU Wen, LI Chongyin, WANG Dongxiao, 2012: Effects of the East Asian Summer Monsoon on Tropical Cyclone Genesis over the South China Sea on an Interdecadal Time Scale, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 249-262.  doi: 10.1007/s00376-011-1080-x
    [5] CHEN Xiao, YAN Youfang, CHENG Xuhua, QI Yiquan, 2013: Performances of Seven Datasets in Presenting the Upper Ocean Heat Content in the South China Sea, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 1331-1342.  doi: 10.1007/s00376-013-2132-1
    [6] Zhang Renhe, Zhao Gang, 2001: Meridional Wind Stress Anomalies over the Tropical Pacific and the Onset of El Ni?o Part Ⅱ: Dynamical Analysis, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 1053-1065.  doi: 10.1007/s00376-001-0022-4
    [7] Yan Junyue, 1997: Observational Study on the Onset of the South China Sea Southwest Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 277-287.  doi: 10.1007/s00376-997-0026-9
    [8] HE Jinhai, JU Jianhua, WEN Zhiping, L\"U Junmei, JIN Qihua, 2007: A Review of Recent Advances in Research on Asian Monsoon in China, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 972-992.  doi: 10.1007/s00376-007-0972-2
    [9] Qingwei ZENG, Yun ZHANG, Hengchi LEI, Yanqiong XIE, Taichang GAO, Lifeng ZHANG, Chunming WANG, Yanbin HUANG, 2019: Microphysical Characteristics of Precipitation during Pre-monsoon, Monsoon, and Post-monsoon Periods over the South China Sea, ADVANCES IN ATMOSPHERIC SCIENCES, 36, 1103-1120.  doi: 10.1007/s00376-019-8225-8
    [10] Peng HU, Wen CHEN, Shangfeng CHEN, Lin WANG, Yuyun LIU, 2022: The Weakening Relationship between ENSO and the South China Sea Summer Monsoon Onset in Recent Decades, ADVANCES IN ATMOSPHERIC SCIENCES, 39, 443-455.  doi: 10.1007/s00376-021-1208-6
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    [12] Zi-Liang LI, Ping WEN, 2017: Comparison between the Response of the Northwest Pacific Ocean and the South China Sea to Typhoon Megi (2010), ADVANCES IN ATMOSPHERIC SCIENCES, 34, 79-87.  doi: 10.1007/s00376-016-6027-9
    [13] Hepeng ZHENG, Yun ZHANG, Lifeng ZHANG, Hengchi LEI, Zuhang WU, 2021: Precipitation Microphysical Processes in the Inner Rainband of Tropical Cyclone Kajiki (2019) over the South China Sea Revealed by Polarimetric Radar, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 65-80.  doi: 10.1007/s00376-020-0179-3
    [14] HU Wenting, WU Renguang, 2015: Relationship between South China Sea Precipitation Variability and Tropical Indo-Pacific SST Anomalies in IPCC CMIP5 Models during Spring-to-Summer Transition, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 1308-1318.  doi: 10.1007/s00376-015-4250-4
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    [17] CHEN Guanghua, HUANG Ronghui, 2008: Influence of Monsoon over the Warm Pool on Interannual Variation on Tropical Cyclone Activity over the Western North Pacific, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 319-328.  doi: 10.1007/s00376-008-0319-7
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Manuscript History

Manuscript received: 10 January 2002
Manuscript revised: 10 January 2002
通讯作者: 陈斌, bchen63@163.com
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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Associations between the Western North Pacific Monsoon and the South China Sea Monsoon

  • 1. Institute of Atmospheric Physics, Chinese Academy of Scienes, Beijing 100080,Department of Earth Science. Chosun University, Kwangju, Korea,CGAM, Department of Meteorology, University of Reading, Reading, United Kingdom

Abstract: Based on the interannual variability of convection over the tropical western North Pacific (WNP), a region of 130°-160°E, 10°-20°N, a composite analysis is performed on the fields of surface temperature,outgoing longwave radiation and 850 hPa zonal wind. The composite results show that the weaker (stronger) WNP convection is related to the El Nino (La Nina)-pattern sea surface temperature (SST)anomalies in the preceding winter and in spring. A comparison with previous results indicates that a similar spatial and temporal distribution of SST anomalies is also associated with the onsets of both the WNP and South China Sea (SCS) monsoons.The composite results also show that the weaker (stronger) convection over the WNP corresponds to the easterly (westerly) anomalies that extend westward from the WNP into the Bay of Bengal. A numerical experiment by an atmospheric general circulation model shows a similar result. In addition, during weaker (stronger) convection summer, the convection over the WNP and lower-level zonal winds over the SCS exhibit a small (large) extent of seasonal evolution.

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