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首页> 外文期刊>Acta Meteorologica Sinica >SOME CHARACTERISTICS OF AIR-SEA EXCHANGE FOR THE SCS SUMMER MONSOON DURING THE SCSMEX IN 1998
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SOME CHARACTERISTICS OF AIR-SEA EXCHANGE FOR THE SCS SUMMER MONSOON DURING THE SCSMEX IN 1998

机译：1998年SCSMEX期间SCS夏季风气海交换的某些特征

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摘要

Atmospheric and oceanic data collected by "Shiyan 3" and "Kexue 1" during the IOP in SCSMEX 98 (Ding et al. 2002) were used to calculate the air-sea turbulent flux exchange. Here the calculation was based on the bulk aerodynamic formulas, which had considered the influence of wind speed and atmospheric stratification. Some characteristics of air-sea exchange were analyzed by examining the results. We found that the onset of the summer monsoon began in the southern region of the South China Sea on May 21 and extended northward to the whole SCS region. There were obvious differences in the characteristics of atmosphere and sea structure, air-sea turbulent flux exchange between south and north. Moreover, the variation of SST is mainly related to the latent flux transfer besides global radiation. We also gave an explanation for the later onset and weakness of the summer monsoon, and a comparison with westerly wind burst in the western tropical Pacific Ocean from 1992 to 1993.
机译：在SCSMEX 98的IOP中由“十堰3”和“科学1”收集的大气和海洋数据（Ding等，2002）用于计算海-气湍流通量交换。这里的计算是基于整体空气动力学公式，其中考虑了风速和大气分层的影响。通过检查结果分析了海气交换的一些特征。我们发现，夏季风的爆发始于5月21日的南海南部地区，并向北延伸至整个南海地区。南北之间大气海结构特征，海气湍流通量交换特征明显不同。此外，SST的变化主要与潜在辐射通量的传递有关，除了整体辐射。我们还解释了夏季风的后发和弱势，并与1992年至1993年西部热带太平洋西风爆发的比较。

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