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Upper ocean responses to category 5 typhoon Megi in the western north Pacific
  • 期刊名称:Acta Oceanol. Sin.
  • 时间:0
  • 页码:51-58
  • 分类:P444[天文地球—大气科学及气象学] Q178.53[生物学—水生生物学;生物学—普通生物学]
  • 作者机构:[1]Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China, [2]State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China
  • 相关基金:Foundation item: The National Basic Research Program "973" Program of China under contract No. 2009CB421202; the National Natural Science Foundation of China under contract Nos 40976110 and 40706061; the Public Science and Technology Research Funds Projects of Ocean under contract No. 200905012; the Zhejiang Provincial Natural Science Foundation of China under contract No. Y5090381.
  • 相关项目:海洋水色偏振遥感研究
中文摘要:

范畴 5 台风 Megi 是在 2010 世界的最强烈的台风。它为 5 d 在华南海(SCS ) 逗留了并且引起了卫星图象检测的一个重要浮游植物花蕾。在这研究,作者由使用叶绿素调查了生物的海洋和对台风 Megi 的物理回答 -- 一(chl -- 一) 集中,海表面温度(SST ) ,海表面高度异例(SSHA ) ,海表面风大小源于不同卫星并且在 situ 数据。chl -- 集中(> 3 mg/m3 ) 与从 2002 ~ 2009 平均的 10 月的吝啬的水平比较在台风经过以后在 SCS 增加了三十次。风压力卷屈和 upwelling 的关系地,作者发现 upwelling 的速度比台风前时期在台风期间是超过十次。而且,混合的层加深了大约 20 m。这些表明 chl 的改进 -- 集中被强壮的垂直混合和 upwelling 触发。沿着台风的轨道,冷却的最大的海表面(68 ? 噁剈?慤慴 桴??

英文摘要:

Category 5 typhoon Megi was the most intense typhoon in 2010 of the world. It lingered in the South China Sea (SCS) for 5 d and caused a significant phytoplankton bloom detected by the satellite image. In this study, the authors investigated the ocean biological and physical responses to typhoon Megi by using chlorophyll-a (chl-a) concentration, sea surface temperature (SST), sea surface height anomaly (SSHA), sea surface wind measurements derived from different satellites and in situ data. The chl-a concentration (〉3 mg/m3) increased thirty times in the SCS after the typhoon passage in comparison with the mean level of October averaged from 2002 to 2009. With the relationship of wind stress curl and upwelling, the authors found that the speed of upwelling was over ten times during typhoon than pre-typhoon period. Moreover, the mixed layer deepened about 20 m. These reveal that the enhancement of chl-a concentration was triggered by strong vertical mixing and upwelling. Along the track of typhoon, the maximum sea surface cooling (6-8~C) took place in the SCS where the moving speed of typhoon was only 1.4-2.8 m/s and the mixed layer depth was about 20 m in pre-typhoon period. However, the SST drop at the east of the Philippines is only 1-2~C where the translation speed of typhoon was 5.5-6.9 m/s and the mixed layer depth was about 40 m in pre-typhoon period. So the extent of the SST drop was probably due to the moving speed of typhoon and the depth of the mixed layer. In addition, the region with the largest decline of the sea surface height anomaly can indicate the location where the maximum cooling occurs.

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