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Three Types of South Pacific Subtropical Mode Waters: Their Relation to the Large-Scale Circulation of the South Pacific Subtropical Gyre and Their Temporal Variability

机译:三种类型的南太平洋副热带水域:它们与南太平洋副热带高压大尺度环流的关系及其时间变异性

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摘要

A detailed spatial distribution of South Pacific Subtropical Mode Water (SPSTMW) and its temporal variation were investigated using the World Ocean Atlas (WOA) 2001 climatology and high-resolution expendable bathythermograph (HRX) line data. In the WOA 2001 climatology, SPSTMW can be classified into western and eastern parts. A detailed examination of spatial distributions using HRX-PX06 line data revealed that the eastern part can be further divided into two types by the Tasman Front (TF) extension. Consequently, SPSTMW can be classified into three types, referred to in the present study as the West, North, and South types. The West type, situated in the recirculation region of the East Australia Current (EAC), has a core layer temperature (CLT) of about 19.1℃; the North type, in the region north of the TF extension, has a CLT of about 17.6℃; and the South type, in the region south of the TF extension, has a CLT of about 16.0℃. The long-term (> 6 yr) variations in the inventories of the three types were dissimilar to each other. The short-term (< 6 yr) and long-term variations in the mean CLT of the North and South types were greater than that of the West type. Winter cooling in the previous year may have influenced the short-term variation in the South-type CLT. Moreover, the strength of the EAC may have influenced long-term variation in the West-type inventory and thickness and in the North-type thickness and CLT.
机译:利用《世界海洋地图集》(WOA)2001年的气候学资料和高分辨率消耗性水热仪(HRX)线数据,研究了南太平洋亚热带模式水(SPSTMW)的详细空间分布及其时间变化。在WOA 2001气候中,SPSTMW可以分为西部和东部两部分。使用HRX-PX06线数据对空间分布进行的详细检查显示,塔斯曼阵线(TF)扩展可以将东部进一步分为两种类型。因此,SPSTMW可以分为三种类型,在本研究中称为西方,北方和南方类型。西部类型位于东澳大利亚洋流(EAC)的回流区,核心层温度(CLT)约为19.1℃。 TF延伸区以北的北部类型的CLT约为17.6℃。在TF扩展带以南的区域中,南部类型的CLT约为16.0℃。三种类型的库存的长期(> 6年)差异互不相同。北部和南部类型的平均CLT的短期(<6年)和长期变化大于西方类型。前一年的冬季降温可能影响了南型CLT的短期变化。此外,EAC的强度可能已经影响了西式库存和厚度以及北式厚度和CLT的长期变化。

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