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Satellite observation of the Zhejiang Coastal Upwelling in the East China Sea during 2007-2009

机译:2007-2009年中国东海浙江沿海上升流的卫星观测

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In this article, EOS MODIS sea surface temperature (SST) data are used to observe the Zhejiang Coastal Upwelling in the East China Sea. MODIS SST data in summer from 2007 to 2009 are selected and processed. Based on the upwelling's temperature features in SST imagery, a temperature threshold approach is established to measure the physical parameters of the upwelling. And then the temporal and spatial characteristics of the upwelling are analyzed. Results show that the upwelling distributes along the Zhejiang Coast running from south to northeast, and covers an average area of 11,000 square kilometers. The mean temperature of the upwelling is about 25~28°C, and its temperature difference from surrounding non-upwelling waters is in the ranges of 2~4 °C. The upwelling appears in June and develops to its strongest period in July and August, and then it weakens and vanishes in late September. Three years of observational results reveal that the upwelling has short-time, seasonal and interannual variances. The upwelling is also closely related to the coastal topography.
机译:本文使用EOS MODIS海面温度(SST)数据观测东海浙江沿海上升流。选择并处理了2007年至2009年夏季的MODIS SST数据。基于SST图像中上升流的温度特征,建立了一种温度阈值方法来测量上升流的物理参数。然后分析了上升流的时空特征。结果表明,上升流沿浙江沿海从南向东北分布,平均面积为11000平方公里。上升流的平均温度约为25〜28℃,与周围非上升流水的温度差在2〜4℃的范围内。上升出现在6月,并发展到7月和8月的最强时期,然后在9月下旬减弱并消失。三年的观测结果表明,上升流具有短时,季节性和年际变化。上升流也与沿海地形密切相关。

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