首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >Pacific Ocean surface freshwater variability underneath the double ITCZ as seen by satellite sea surface salinity retrievals
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Pacific Ocean surface freshwater variability underneath the double ITCZ as seen by satellite sea surface salinity retrievals

机译:卫星海面盐度反演表明,双重ITCZ下的太平洋海面淡水变化

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摘要

The salinity budget of the upper tropical Pacific Ocean underneath the double Intertropical Convergence Zone (ITCZ) is studied using the Soil Moisture and Ocean Salinity (SMOS) and Aquarius surface salinity observations as well as in situ salinity measurements. In this shallow mixed layer region of the ocean, precipitation effects on the near-surface salinity budget are large, typically leading to a band of fresh sea surface salinity (SSS) between March and June. The role of precipitation during the freshening period is documented here through a direct correlation between the SMOS SSS fields and the monthly accumulated precipitation. During the same period, the mixed layer salinity budget is impacted by advection, which, based on in situ observations, is found to be another important mechanism for the evolution of the near-surface salinity as documented through a connection between the north equatorial eastern Pacific Fresh water pool and this south equatorial freshwater pattern in boreal spring. However, given the information at hand, the near-surface salinity budget cannot be closed, suggesting that other processes are important too, such as nonlinear effects, mixing, and entrainment.
机译:使用土壤水分和海洋盐度(SMOS)和水瓶座表面盐度观测值以及原位盐度测量值研究了热带双热带交汇带(ITCZ)下热带热带太平洋的盐度预算。在海洋的这一浅层混合层区域中,降水对近地表盐度预算的影响很大,通常会导致三月至六月之间的新鲜海面盐度(SSS)带。这里通过SMOS SSS场与月累积降水量之间的直接相关性记录了在清新时期降水的作用。在同一时期,混合层盐度预算受到平流的影响,根据实地观测,平流影响了近地表盐度的另一重要机制,这是通过北赤道东太平洋之间的联系证明的。淡水池和北方春季的赤道南极淡水模式。然而,鉴于现有信息,近地表盐度预算无法关闭,这表明其他过程也很重要,例如非线性效应,混合和夹带。

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