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Influence of wind climate changes on the mean sea level and current regime in the coastal waters of west Estonia, Baltic Sea

机译:风的气候变化对波罗的海西部爱沙尼亚沿海水域的平均海平面和当前状态的影响

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The response of semi-realistic wind speed increase scenarios to the mean sea level and current regime of semi-enclosed sub-basins in the Baltic Sea is studied with a 2D hydrodynamic model. According to the model output of spatial mean sea levels, an increase in the westerly wind component by 2 m s-1 leads, for example, to a mean sea level rise of up to 3 cm in windward locations in the study area. The sea level change patterns depend on the wind scenario and coastline configuration. The increases in wind speed considered here also lead to enhanced water exchange through the straits, strengthening of the basin-scale circulation, enhancement of up- and downwelling, and increased bottom stresses near coasts.
机译:利用二维流体动力学模型研究了波罗的海半现实风速增加情景对半封闭次流域平均海平面和当前状态的响应。根据空间平均海平面的模型输出,西风分量增加2 m s-1会导致,例如,研究区域内迎风位置的平均海平面上升高达3 cm。海平面的变化模式取决于风况和海岸线配置。这里考虑的风速的增加还导致通过海峡的水交换增加,流域规模的循环加强,上,下涌的增加以及海岸附近海底应力的增加。

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