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EVOLUTION OF THE EXTREME WAVE REGION IN THE NORTH ATLANTIC USING A 23 YEAR HINDCAST

机译:23年以来的预测,大西洋极端波浪区的演变。

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The IOWAGA data base for the North Atlantic region was used to identify the region where extreme values of significant wave height are more likely to occur. The IOWAGA database was obtained from the WAVEWATCH Ⅲ model hindcast using the CFSR (Climate Forecast System Reanalysis) from NOAA The period of the study covers 1990 up to 2012 (23 years). The variability of the significant wave height was assessed by computing return periods for sea storms where the significant wave height exceeds a given threshold. The return periods of sea storms where the H_s exceeds extreme values for the north Atlantic region were computed allowing for the identification of the extreme wave regions which show that extreme waves are more likely to occur in the storm track regions of the tropical and ex-tratropical north Atlantic cyclones.
机译:利用北大西洋地区的IOWAGA数据库确定了更可能出现明显波高的极端值的地区。 IOWAGA数据库是使用NOAA的CFSR(气候预报系统再分析)从WAVEWATCHⅢ模型后播获得的。研究时间涵盖1990年至2012年(23年)。有效波高的变异性是通过计算有效波高超过给定阈值的海暴返回周期来评估的。计算了H_s超过北大西洋区域极端值的海暴返回周期,从而可以确定极端波区域,这表明极端波更有可能发生在热带和非热带的风暴径区域北大西洋气旋。

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