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Multi-temporal Scale Characteristics and Its Causes of Intraseasonal Oscillation of Sea Surface Temperature in the Pacific

机译:太平洋海表温度季节内多尺度尺度变化特征及其成因

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摘要

In the context of daily NMC sea surface temperature (SST), 10-m winds (Vμ) and monthly mixed layer depth ( mld ) data, the climatic and anomaly characteristics are researched, with investigating the maintaining mechanisms of SST intraseasonal oscillation ( SST ) on the different time scales. The results show that 1) there are three high SST intensity areas in the Pacific, which are the tropical eastern Pacific existing for the whole year,the northwest Pacific for the boreal spring, summer and autumn, and the southwest Pacific for the austral summer half year; They all appear in the smallest areas and the seasons of mixed layer depth ( mld ). 2) The interannual anomaly of SST over the above areas shows marked negative correlation relationship with that of mld physically, which is more direct than that with SST anomaly. 3) The basal coupled pattern of May-September Vφand SST for the North Pacific, which is obtained by time -lagged Singular Value Decomposition (SVD), disclose a negative feedback process considering drift and sensible heat as power. This process existing in the smallest mld areas is the maintaining mechanism of strong SST.
机译:在每日NMC海面温度(SST),10米风(Vμ)和每月混合层深度(mld)数据的背景下,研究了气候和异常特征,并研究了SST季节内振荡(SST)的维持机制。 )在不同的时间范围内。结果表明:1)太平洋地区有3个高SST强度区域,它们是全年存在的热带东太平洋地区,北,北,北,北,北,北,北,北,北,北,北,北,北,北,南太平洋是夏季南半球。年;它们都出现在最小的区域和混合层深度(mld)的季节。 2)在上述区域,SST的年际异常与MLD的年际异常呈明显的负相关,比SST异常的年际异常更为直接。 3)通过时滞奇异值分解(SVD)获得的北太平洋5月至9月VST和SST的基础耦合模式,揭示了一种以漂移和显热为动力的负反馈过程。存在于最小mld区域中的此过程是强SST的维持机制。

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