Numerical study of wind effect on green island wake

S. Liang, N. Kuo, D. Doong, T. Hsu
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Abstract

Wind effect on Kuroshio-induced island wake downstream the Green Island, Taiwan is studied using a depth-averaged shallow-water model. Seasonal monsoon effect on spatial-temporal scales, such as aspect ratio, dimensionless width, and Strouhal number as well as propagation speed of the vortices of Reynolds number 50 is studied. It is found that northeast monsoon has more pronounced effect in wake characteristics than southwest monsoon does, in terms of flow speed and recirculation zone, the aspect ratio, and dimensionless width. Vortices are pushed back close to the island with a smaller size of recirculation when Kuroshio flows against the northeast monsoon; Vortices are pushed farther downstream with a larger size of recirculation when Kuroshio flows in favor of the southwest monsoon. However, wind effect on temporal variation of island wake seems insignificant. The Strouhal number is between 0.116 and 0.125 from numerical simulations. This value is close to result of previous reports.
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风对绿岛尾流影响的数值研究
利用深度平均浅水模式研究了台湾绿岛下游黑潮诱导岛屿尾流的风效应。研究了季节季风对雷诺数为50的涡旋的展弦比、无量纲宽度、斯特罗哈尔数和传播速度等时空尺度的影响。研究发现,东北季风对尾迹特征的影响比西南季风对尾迹特征的影响更为显著,主要表现在流速和环流带、展弦比、无因次宽度等方面。当黑潮对着东北季候风流动时,涡旋被推回靠近岛屿,再环流规模较小;当黑潮对西南季风有利时,涡旋被进一步推向下游,再环流规模更大。风对岛屿尾流时间变化的影响不明显。数值模拟结果表明,Strouhal数在0.116 ~ 0.125之间。这个值接近于以前报告的结果。
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