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The “shallow-waterness” of the wave climate in European coastal regions

机译:欧洲沿海地区海浪气候的“浅水度”

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In contrast to deep water waves, shallow water waves are influenced by bottom topography, which has consequences for the propagation of wave energy as well as for the energy and momentum exchange between the waves and the mean flow. The ERA-Interim reanalysis is used to assess the fraction of wave energy associated with shallow water waves in coastal regions in Europe. We show maps of the distribution of this fraction as well as time series statistics from eight selected stations. There is a strong seasonal dependence and high values are typically associated with winter storms, indicating that shallow water wave effects can occasionally be important even in the deeper parts of the shelf seas otherwise dominated by deep water waves.
机译:与深水波相反,浅水波受底部地形的影响,这对波能的传播以及波与平均流之间的能量和动量交换具有影响。 ERA-Interim重新分析用于评估欧洲沿海地区与浅水波有关的波能比例。我们显示了这部分分布的地图以及来自八个选定站点的时间序列统计信息。由于强烈的季节依赖性,冬季暴风雨通常伴随着较高的数值,这表明即使在深海浪占主导的深海架子海中,浅水浪影响有时也会很重要。

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