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Vertical characteristics revealed by biweekly and synoptic variability of upper sea temperature in the northern South China Sea

机译:南海北部地区每两周一次和天气变化的天气特征揭示垂直特征

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摘要

On the basis of the analysis of the sea temperature data that are observed from the three automatic temperature line acquisition sysem mooring buoys deployed in the central South China Sea (SCS) during South China Sea monsoon experiment, vertical features of biweekly and synoptic variability are discussed. There are five vertical modes, that is, subsurface temperature variability is in phase with, out of phase with, leads to, lags the surface temperature variability, and at depths within the subsurface layer the upper and lower temperature variations are out of phase. The formation of these vertical modes is related to the property of low-level atmospheric forcing and to the background in atmosphere and ocean. Wind stress curl is the main driving factor in forming Modes 1 and 3, and wind stresses in forming Modes 2 and 4.
机译:在对南海季风试验期间部署在南海中部(SCS)的三个自动温度线采集系统系泊浮标观察到的海水温度数据进行分析的基础上,讨论了每两周的垂直特征和天气变化。有五种垂直模式,即地下温度变化与表面温度变化同相,异相,导致,滞后,并且在地下层深度内,上下温度变化异相。这些垂直模式的形成与低空大气强迫的性质以及大气和海洋的背景有关。风应力卷曲是形成模式1和3的主要驱动因素,风应力是形成模式2和4的主要应力。

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