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首页> 外文期刊>Geophysical Research Letters >Multisatellite observation on upwelling after the passage of Typhoon Hai-Tang in the southern East China Sea
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Multisatellite observation on upwelling after the passage of Typhoon Hai-Tang in the southern East China Sea

机译:东海南部台风海棠过后上升流的多卫星观测

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The serial remote sensing based imageries clearly revealed large scale of upwelling within large regional enhancement of chlorophyll-a (Chl-a) concentration in the southern East China Sea (ECS) after the passage of super typhoon Hai-Tang in July 2005. After the typhoon on 22 July, the upwelling area (<26 degrees C) expanded rapidly to 9146 km 2 on the shelf-break. The large increased upwelling persisted for more than a week. Ocean color images also reveled that high Chl-a concentration of >3.0 mg/m(3) appeared in the shelf region, where the high Chl-a pattern matched the upwelling in terms of location and time. On the other hand, a large offshore SST cooling was also observed mainly to the right of typhoon track on 20 July, it lasted in a period of 2-3 days. This paper provides clear and high-resolution evidence that typhoon significant increased upwelling and Chl-a concentration in the southern ECS.
机译:2005年7月超级台风海棠通过后,基于遥感的系列影像清楚地揭示了东中国南部南部(ECS)叶绿素a(Chl-a)浓度在较大区域内的大幅上升。在7月22日的台风中,陆架上升区(<26摄氏度)迅速扩展至9146 km 2。大量增加的上升流持续了一个多星期。海洋彩色图像还显示,货架区域出现了高Chl-a浓度> 3.0 mg / m(3),在该区域中,高Chl-a模式在位置和时间方面与上升流相匹配。另一方面,主要在7月20日的台风轨道右侧也观察到了大型海上SST冷却,持续了2-3天。本文提供了清晰而高分辨率的证据,表明台风明显增加了南部ECS的上升流和Chl-a浓度。

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