中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Role of the phase transition of intraseasonal oscillation on the south china sea summer monsoon onset

文献类型:期刊论文

作者Shao, Xie1,2; Huang, Ping1; Huang, Rong-Hui1
刊名Climate dynamics
出版日期2015-07-01
卷号45期号:1-2页码:125-137
关键词Intraseasonal oscillation (iso) South china sea summer monsoon (scssm) Monsoon onset
ISSN号0930-7575
DOI10.1007/s00382-014-2264-8
通讯作者Huang, ping(huangping@mail.iap.ac.cn)
英文摘要The present study investigates the role of intraseasonal oscillation (iso) on the south china sea (scs) summer monsoon onset based on the daily reanalysis data for a 33-year period from 1979 to 2011. the scs summer monsoon (scssm) onset always occurs during the developing phase of iso at which the iso develops from inactive convection and easterly anomalies to active convection and westerly anomalies. in the scssm onset season (april-july), the change rate of the zonal winds of iso over the scs is around twice as large as the increase rate of the climatological westerly winds. therefore, the monsoon onset, which is a process requiring the westerly winds to increase up to a certain threshold, only occurs during iso's developing phase. furthermore, the monsoon onsets tend to occur at the active (inactive) convection and developing phase of iso in the early (late) onset years. in the early-onset years, a strong active phase of iso is needed to prompt monsoon onset because of the undeveloped climatological easterly winds at the onset period, whereas in the late-onset years the developed climatological westerly winds will prompt the monsoon onset as long as the suppressive role of the inactive phase of iso starts relieving. due to the constraint of iso's developing phase on the scssm onset, an earlier iso's developing phase occurring in the monsoon onset season will induce an earlier scssm onset. the low-frequency variation, with a period greater than 90 days, can also modify the role of iso's developing phase, especially when the developing phase of iso occurs at the early season of the monsoon onset.
WOS关键词WESTERN NORTH PACIFIC ; TROPICAL CYCLONE ACTIVITY ; COUPLED EQUATORIAL WAVES ; INTERANNUAL VARIABILITY ; EAST-ASIA ; MODULATION ; CLIMATOLOGY ; DEFINITION ; CONVECTION ; PREDICTION
WOS研究方向Meteorology & Atmospheric Sciences
WOS类目Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000354712500007
出版者SPRINGER
URI标识http://www.irgrid.ac.cn/handle/1471x/2376564
专题中国科学院大学
通讯作者Huang, Ping
作者单位1.Chinese Acad Sci, Ctr Monsoon Syst Res, Inst Atmospher Phys, Beijing 100190, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
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GB/T 7714
Shao, Xie,Huang, Ping,Huang, Rong-Hui. Role of the phase transition of intraseasonal oscillation on the south china sea summer monsoon onset[J]. Climate dynamics,2015,45(1-2):125-137.
APA Shao, Xie,Huang, Ping,&Huang, Rong-Hui.(2015).Role of the phase transition of intraseasonal oscillation on the south china sea summer monsoon onset.Climate dynamics,45(1-2),125-137.
MLA Shao, Xie,et al."Role of the phase transition of intraseasonal oscillation on the south china sea summer monsoon onset".Climate dynamics 45.1-2(2015):125-137.

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来源:中国科学院大学

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