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首页> 外文期刊>Boreal Environment Research >Wave hindcast statistics in the seasonally ice-covered Baltic sea
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Wave hindcast statistics in the seasonally ice-covered Baltic sea

机译:季节性冰雪覆盖的波罗的海中的波后预报统计

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We used six years of wave hindcasts, calculated by the wave model WAM, to compile wave statistics for the Baltic Sea. The wave model was implemented taking into account the special features of the Baltic Sea: irregular coastline, archipelago and ice. To our knowledge, there is no single way to present annual statistics in seasonally ice-covered seas. We discuss five different possibilities to calculate the statistics, and the differences between them. According to verification against wave buoy and satellite altimeter measure- ments, the quality of the hindcast significant wave height is sufficient for presenting reli- able wave statistics. The mean values of the significant wave height are smaller than 1.5 m. According to the mean values and exceedance probabilities, the severest wave climate is in the Baltic Proper. The wave climate in the other basins is considerably less severe. The maximum hindcast significant wave height is over 9 m, whereas the measured maximum is 8.2 m.
机译:我们使用了由波浪模型WAM计算出的六年海浪后遗症来编制波罗的海的海浪统计数据。实施波浪模型时要考虑到波罗的海的特殊特征:不规则的海岸线,群岛和冰层。据我们所知,没有任何一种方法可以显示季节性冰雪覆盖的海洋中的年度统计数据。我们讨论了五种不同的可能性来计算统计数据,以及它们之间的差异。根据对海浪浮标和​​卫星高度计测量的验证,后播有效波高的质量足以提供可靠的海浪统计数据。有效波高的平均值小于1.5 m。根据平均值和超出概率,最严重的波浪气候是波罗的海。其他盆地的波浪气候严重程度要小得多。最大后验显着波高超过9 m,而实测最大波高为8.2 m。

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