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Spatial and temporal variability of sea surface temperature and warming trends in the Yellow Sea

机译:黄海中海表温度的时空变化和变暖趋势

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The spatial and temporal variability of sea surface temperatures (SST) in the Yellow Sea was investigated using satellite data and in-situ measurements over 29 years from 1981 to 2009. We found that the first empirical orthogonal function (EOF) mode of SST variability, which accounts for 47.59% of the total SST variance, exhibited a warming signal during the study period. We examined the relationships between the dominant EOF mode, long-term trends of SST changes and in-situ temperatures, and bathymetry. As a result, the shallow regions demonstrated more significant increasing rates than the deep area in the Yellow Sea. Vertical stratification of the water column revealed long-term changes, which led to differential surface warming. The warming rates decayed monotonically with depth. The spatial features of long-term SST warming trends were most remarkable near the Yangtze River, due to the effect of river discharge. Abrupt changes in the time-varying amplitude of the first EOF mode in winter could be explained by Arctic Oscillation. (C) 2014 Elsevier B.V. All rights reserved.
机译:利用1981年至2009年这29年间的卫星数据和原位测量方法,对黄海海表温度(SST)的时空变化进行了研究。我们发现,SST的第一个经验正交函数(EOF)模式是占总SST差异的47.59%,在研究期间显示出变暖信号。我们检查了主要的EOF模式,SST变化的长期趋势和原位温度与测深之间的关系。结果,与黄海深层地区相比,浅层地区的增长速度更为显着。水柱的垂直分层显示了长期变化,这导致了不同的表面变暖。升温速率随深度单调衰减。受河流流量的影响,长江附近海域SST长期变暖趋势的空间特征最为明显。冬季第一个EOF模式的时变幅度的突然变化可以用北极涛动解释。 (C)2014 Elsevier B.V.保留所有权利。

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