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Modeling Drift Currents in a Shallow Basin with Allowance for Variations in Tangential Stresses Induced by Wind Waves

机译:考虑风浪引起的切向应力变化的浅水盆地流场模拟

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A coupling model for calculating wind-driven currents and waves in a shallow basin with allowance for current-wave interactions is introduced.The model is constructed on the basis of the three-dimensional sigma-coordinate model of currents [3] and the SWAN(Simulating Waves Nearshore)spectral wave model [4].The effect of waves on currents is taken into account in the coefficients of surface and bottom friction through rough-ness parameters.Results of combined modeling of stationary fields of currents and waves generated by spatially homogeneous wind are correlated with the corresponding results of separate modeling for a cylindrical basin of constant depth and the water area of Lake Donuzlav(the northwestern coast of the Crimea).The allowance for the effect of waves during calculation of tangential wind stresses in the model of currents is shown to be among major factors intensifying water circulation and forming spatial inhomogeneities of the vortex type.In addition,some cases of local decreases in tangential wind stresses are revealed;they appear when the lake is penetrated from the side of the open sea by relatively long waves,which significantly decrease the roughness of the water surface.
机译:引入了一种在浅海盆地中考虑风浪相互作用而计算风驱动流和波浪的耦合模型。该模型是基于三维水流的sigma坐标模型[3]和SWAN(近海模拟波谱波模型[4]。通过粗糙度参数将波对电流的影响考虑在表面和底部的摩擦系数中。风与恒定深度的圆柱形盆地和Donuzlav湖(克里米亚的西北海岸)水域的单独建模的相应结果相关。在模型的切向风应力计算中,考虑了波浪效应洋流被证明是加剧水循环并形成旋涡类型的空间非均匀性的主要因素之一。揭示了切向风应力的减小;当湖泊从远海一侧被相对长的波浪穿透时,它们就会出现,这会大大降低水面的粗糙度。

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