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Low-Frequency Variability of the Yellow Sea Cold Water Mass Identified from the China Coastal Waters and Adjacent Seas Reanalysis

机译:来自中国沿海水域和邻近海獭的黄海冷水量的低频变异性

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摘要

This study uses the China Coastal Waters and Adjacent Seas Reanalysis (CORA) data to investigate the interannual and decadal variability of the Yellow Sea cold water mass (YSCWM) and its relationship to climate indices including the Arctic Oscillation (AO), El Niño/Southern Oscillation (ENSO), and Pacific Decadal Oscillation (PDO). On the interannual timescale, the strong correlation between winter PDO and the YSCWM may indicate the dominant effect of winter PDO on the YSCWM through the modulation of local heat flux and wind stress. It is also found that the local wind stress and heat flux in summer have little impact on the interannual variability of the YSCWM. On the decadal time scale, the YSCWM is associated with winter AO and winter PDO. Winter AO mainly controls local heat flux, modulating the decadal variability of the YSCWM. In contrast, winter PDO is strongly connected with winter heat flux and wind stress to modulate the decadal variability of the YSCWM. In summer, for three climate factors, ENSO is the dominant factor controlling the decadal variability of the YSCWM.
机译:本研究利用中国沿海水域和邻近的海水分析(Cora)数据来调查黄海冷水质量(YSCWM)的际和截止变异性及其与气候指标的关系,包括北极振荡(AO),ElNiño/南方振动(ENSO),和太平洋二等振荡(PDO)。在际时间尺度上,冬季PDO与YSCWM之间的强烈相关性可以通过调制局部热通量和风力应力来表示冬季PDO对YSCWM的显着效果。还发现夏季的局部风力和热量通量对YSCWM的续际变化几乎没有影响。在截止时间表上,YSCWM与冬季AO和冬季PDO相关联。冬季AO主要控制局部热通量,调制YSCWM的二等变化。相比之下,冬季PDO与冬季热通量和风力应力强烈连接,以调节YSCWM的二等变化。夏季,对于三种气候因素,ENSO是控制YSCWM的二等变异性的主导因素。

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