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首页> 外文期刊>Acta Oceanologica Sinica >On the relationship between convection intensity of South China Sea summer monsoon and air-sea temperature difference in the tropical oceans
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On the relationship between convection intensity of South China Sea summer monsoon and air-sea temperature difference in the tropical oceans

机译:南海夏季风对流强度与热带海洋海气温差的关系

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摘要

The annual, interannual and inter-decadal variability of convection intensity of South China Sea (SCS) summer monsoon and air-sea temperature difference in the tropical ocean is analyzed, and their relationship is discussed using two data sets of 48-a SODA (simple ocean data assimilation) and NCEP/NCAR. Analyses show that in wintertime Indian Ocean (WIO), springtime central tropical Pacific (SCTP) and summertime South China Sea-West Pacific (SSCSWP), air-sea temperature difference is significantly associated with the convection intensity of South China Sea summer monsoon. Correlation of the inter-decadal time scale (above 10 a) is higher and more stable. There is inter-decadal variability of correlation in scales less than 10 a and it is related with the air-sea temperature difference itself for corresponding waters. The inter-decadal variability of the convection intensity during the South China Sea summer monsoon is closely related to the inter-decadal variability of the general circulation of the atmosphere. Since the late period of the 1970s, in the lower troposphere, the cross-equatorial flow from the Southern Hemisphere has intensified. At the upper troposphere layer, the South Asian high and cross-equatorial flow from the Northern Hemisphere has intensified at the same time, Then the monsoon cell has also strengthened and resulted in the reinforcing of the convection of South China Sea summer monsoon.
机译:分析了南海夏季风对流强度的年际,年际和年代际变化以及热带海洋的海气温差,并使用两个48-a SODA(简单)数据集讨论了它们之间的关系。海洋数据同化)和NCEP / NCAR。分析表明,在冬季印度洋(WIO),春季中部热带太平洋(SCTP)和夏季南海西太平洋(SSCSWP)中,海气温度差与南海夏季风的对流强度显着相关。年代际时间尺度(10 a以上)的相关性更高且更稳定。在小于10 a的尺度上,年代际相关性存在变化,并且与相应水域的海气温度差本身有关。南海夏季风对流强度的年代际变化与大气总环流的年代际变化密切相关。自1970年代后期以来,在对流层低层,来自南半球的跨赤道流加剧了。在对流层上层,北半球的南亚高压和跨赤道流同时增强,然后季风单元也加强了,从而增强了南海夏季风的对流。

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