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首页> 外文期刊>Selected Topics in Applied Earth Observations and Remote Sensing, IEEE Journal of >Erratum to “Distinct Characteristics of SST Variabilities in the Sulawesi Sea and the Northern Part of the Maluku Sea During the Southeast Monsoon” [Jun 19 1763-1770]
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Erratum to “Distinct Characteristics of SST Variabilities in the Sulawesi Sea and the Northern Part of the Maluku Sea During the Southeast Monsoon” [Jun 19 1763-1770]

机译：勘误表“东南季风期间苏拉威西海和马鲁古海北部海域海表温度的不同特征” [6月19日，1763-1770]

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摘要

The Sulawesi Sea and the northern part of theMaluku Sea belong to the western equatorial Pacific that is influenced by the Mindanao Current. During the southeast (SE) monsoon, contrasting sea surface temperature (SST) distributions occur between these two seas. The purpose of this research is to investigate the mechanisms of contrasting SST distribution in the Sulawesi Sea and the northern part of the Maluku Sea under the condition of strong southerly wind during the SE monsoon season. Our analysis was based on satellite observations. Warmer (colder) SSTs are identified in the Sulawesi Sea (northern part of the Maluku Sea), which correspond to the weaker (stronger) southerly wind speed. Strong southerly winds in the northern part of the Maluku Sea generate eastwardEkmanmass transport (EMT) that carries thewater mass away from the coast, inducing upwelling. In contrast, the southerly winds fromtheMaluku Sea are blocked by theGorontalo andNorth Sulawesi Mountains, creating low-wind areas in the Sulawesi Sea that are located on the lee side of those mountains. Furthermore, the existence of a valley between those mountains acts as a wind gap that channels the southerly wind to the Sulawesi Sea. Since the seaward EMT is weak and the latent heat release is not dominant, SSTs in front of the wind gap are only slightly reduced, possibly through the mechanisms of oceanic mixing.
机译：苏拉威西海和马卢古海的北部属于受棉兰老流影响的赤道西太平洋。在东南（SE）季风期间，这两个海之间出现了相反的海表温度（SST）分布。这项研究的目的是研究东南季风季节在南风强烈的情况下，苏拉威西海和马鲁古海北部海域海表温度分布的对比机制。我们的分析基于卫星观测。在苏拉威西海（马鲁古海的北部）发现了更暖（冷）的海温，这与南风的弱（强）相对应。马鲁古海北部的强南风产生向东的埃克曼马斯运输（EMT），将水团带离海岸，引发上升流。相比之下，来自马卢古海的南风被哥伦打洛山脉和北苏拉威西山脉阻挡，在苏拉威西海中位于这些山脉背风处的低风区域。此外，在这些山脉之间存在一个山谷，这是一个风道，将南风引导到苏拉威西海。由于向海的EMT弱，潜热释放不占主导地位，因此可能通过海洋混合机制使风隙前的SST仅略微减少。

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