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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Processes influencing wind-induced current profiles in near coastal stratified regions
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Processes influencing wind-induced current profiles in near coastal stratified regions

机译:影响沿海分层地区风生电流剖面的过程

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Cross sectional and single point models of wind-induced currents in a stratified sea coastal region are used to determine the role of internal waves due to various wind periods upon mixing and current profiles. The limitations of a point model in reproducing current profiles are also examined. Calculations are performed with both fixed vertical diffusion coefficients and those derived from a turbulence closure model. Wind forcing at sub-inertial, inertial and super-inertial frequencies together with a wind impulse are considered. Results show that the offshore extent of the coastal boundary layer where mixing occurs depends upon the frequency of the wind forcing. The extent of this region and offshore propagation of internal waves influences the offshore variability of current profiles and the extent to which they can be reproduced by a single point model. Calculations with periodic wind forcing show that within the coastal boundary layer a point model cannot reproduce the current profile due to the internal pressure gradients associated with the internal wave field. However outside this region, current profiles from a point model are in good agreement with those computed with the cross section model when a barotropic pressure gradient forcing proportional to the local wind forcing is included. In the case of transient wind forcing, the inertial period dominates and determines the offshore extent of the coastal boundary layer. The transient nature of the response is such that although the single point model, outside the coastal region can reproduce the surface current due to direct wind forcing, the current at depth is not reproduced. The offshore extent of the coastal boundary layer computed with the turbulence energy model is comparable to that found with fixed diffusion coefficients although in some cases there are important differences which influence current profiles. (C) 2003 Elsevier Ltd. All rights reserved. [References: 26]
机译:分层的沿海地区中的风流的横截面和单点模型用于确定由于混合和电流分布的各种风周期引起的内波作用。还研究了点模型在复制当前轮廓时的局限性。使用固定的垂直扩散系数和从湍流闭合模型得出的数值进行计算。考虑了在亚惯性,惯性和超惯性频率上的风力以及风的冲击。结果表明,发生混合的沿海边界层的离岸范围取决于强迫风的频率。该区域的范围和内部波的离岸传播会影响电流剖面的离岸变化性,以及可以通过单点模型再现的程度。带有周期性风强迫的计算表明,在海岸边界层内,由于与内部波场相关的内部压力梯度,点模型无法重现当前剖面。但是,在该区域之外,当包括与局部风强迫成比例的正压梯度压力时,来自点模型的当前曲线与用横截面模型计算的电流曲线非常吻合。在瞬时强迫风的情况下,惯性周期起主导作用,并决定了海岸边界层的离岸范围。响应的瞬态性质是,尽管在沿海区域之外的单点模型由于直接的风强迫可以重现表面电流,但在深处却没有重现电流。用湍流能模型计算的海岸边界层的离岸范围可与采用固定扩散系数得到的范围相媲美,尽管在某些情况下会影响电流分布。 (C)2003 Elsevier Ltd.保留所有权利。 [参考:26]

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