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Application of a wind-driven barotropic model to simulate the seasonal circulation of the northern Arabian Sea

机译:风动力正压模型在模拟阿拉伯海北部季节环流中的应用

摘要

A two dimensional numerical barotropic model based on the depth-integrated equations is presented here. Sensitivity of the model is analyzed by using wind stresses of different months. Real wind data and actual bathymetry are used as an input to obtain the circulation patterns of the northern Arabian Sea during specific seasons. However, the model is also tested with constant depth for comparison. A number of numerical simulations are performed to study the combined effects of wind stress, bathymetry and basin geometry. Since the goal of this study is to simulate the circulation of the northern Arabian sea in accordance with the observed wind stress, therefore, wind stresses of different months like July (the peak os SW monsoon), October (the transition period from SW to NE monsoon), January (the peack of NE monsoon) and April (the transition period from NE to SW monsoon) are used to examine the circulation patterns. The results obtained are satisfactory in that they resemble known patterns.
机译:本文提出了基于深度积分方程的二维数值正压模型。通过使用不同月份的风应力来分析模型的敏感性。实际风速数据和实际测深数据被用作输入,以获取特定季节期间阿拉伯海北部的环流模式。但是,还对模型进行了恒定深度测试以进行比较。进行了许多数值模拟,以研究风应力,测深和盆地几何形状的综合影响。由于本研究的目的是根据观测到的风应力来模拟阿拉伯北部海域的环流,因此,不同月份的风应力,如7月(南半球季风季风),10月(南半球西南向东北过渡期)季风),一月(东北季风的高峰期)和四月(东北向西南季风的过渡期)被用来研究环流模式。获得的结果令人满意,因为它们类似于已知的图案。

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