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Investigation of typhoons by using ECMWF re-analysis data

机译:利用ECMWF再分析资料调查台风

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In this paper the significant wave height (SWH) and the wind field products of ECMWF re-analysis data are used to derive the location of typhoon center, to analyze the temporal and spatial features of the SWH induced by typhoons, and to study the relationships between the SWH and wind speed. The results are compared with merged SWH data from several satellite altimeters (GFO, TOPEX/Poseidon, Jason-1 and Envisat) and wind vectors from QuikSCAT. Typhoon eyes are observed by using SAR and MODIS data. It is shown that (1) the spatial distribution of wind fields from ECMWF re-analysis data is almost in accordance with that of wind fields from QuikSCAT; (2) the spatial distribution of SWH from ECMWF re-analysis data is almost in accordance with that of SWH from merged SWH data; (3) the distribution of higher wind speed and higher wave height are consistent with the SWH and the wind field product of ECMWF re-analysis data; (4) the centers of typhoon waves lag behind the centers of typhoons; (5) the top of typhoon move faster that the bottom in the case of Saomai.
机译:本文利用ECMWF再分析数据的重要波高(SWH)和风场积推算台风中心的位置,分析台风诱发的SWH的时空特征,并研究它们之间的关系。在SWH和风速之间将结果与来自多个卫星高度计(GFO,TOPEX / Poseidon,Jason-1和Envisat)的合并SWH数据以及QuikSCAT的风向矢量进行了比较。通过使用SAR和MODIS数据可以观察到台风眼。结果表明:(1)ECMWF再分析数据中风场的空间分布几乎与QuikSCAT的风场一致; (2)ECMWF重新分析数据中SWH的空间分布几乎与合并SWH数据中SWH的空间分布一致; (3)较高风速和较高波高的分布与SWH和ECMWF再分析数据的风场积一致; (四)台风波中心滞后于台风中心; (5)台风的顶部移动速度比底部的情况要快。

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