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Multidecadal ensemble hindcast of wave fields in the Baltic Sea

机译:波罗的海波场的多年代合奏后铸

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Several versions of the wave climate of the Baltic Sea are reconstructed by means of the spectral wave model WAM with a resolution about 3 nautical miles. This model (optionally covering different frequency range) is forced with two versions of wind fields and with and without the information about sea ice. We discuss the wave fields calculated for 1957–2008 (52 years) using high-resolution COSMO wind hindcast and for 1970–2007 (38 years) using slightly adjusted geostrophic wind fields from the Swedish Meteorological and Hydrological Institute database. The runs are performed in parallel with and without ice information. We provide a comparison of spatial distributions of the main climatological parameters (average wave heights, higher percentiles of wave heights etc., formal trends of these quantities) for these runs. All simulations replicate the well-known features of the Baltic Sea wave climate as the moderate average wave heights, extensive intermittency of wave properties and substantial spatial anisotropy of typical and extreme wave heights, with relatively severe wave climate in the eastern parts of the Baltic Proper and its sub-basins. The simulations also indicate widespread differences in the long-term behavior of average wave heights and higher percentiles of the wave heights in different sea areas.
机译:波罗的海的波浪气候的几种版本是通过光谱波模型WAM重建的,其分辨率约为3海里。该模型(可选地覆盖不同的频率范围)在两个版本的风场的作用下,带有或不带有有关海冰的信息。我们讨论了使用高分辨率COSMO风后向预报的1957–2008年(52年)和1970–2007年(38年)的波浪场,这些波浪场使用了瑞典气象水文研究所数据库中经过略微调整的地转风场。这些运行在有无冰信息的情况下并行执行。我们对这些运行的主要气候参数(平均波高,波高的更高百分位数等,这些量的形式趋势)的空间分布进行了比较。所有模拟都复制了波罗的海波浪气候的众所周知的特征,如中等平均波浪高度,广泛的波浪特性间歇性以及典型和极端波浪高度的较大的空间各向异性,而波罗的海东部地区的波浪气候相对严峻及其子盆地。这些模拟还表明,在不同海域中,平均波高的长期行为和波高的较高百分位数存在广泛差异。

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