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Seasonal Simulations of a Coupled Ice-ocean Model in the Bohai Sea and North Yellow Sea since the Winter of 1997/1998

机译:自1997/1998年以来渤海和北黄海耦合冰海模型的季节性模拟

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A fine-resolution coupled ice-ocean model configured for the Bohai Sea and North Yellow Sea is presented. A horizontal grid spacing of 3.7km×2.8km was used in this coupled model. Seasonal simulations were made from the winters of 1997/1998 to 2008/2009. By comparing of the simulation results and the remote sensing images, the ice-ocean coupled model reasonably reproduces the seasonal variations of the sea ice conditions in the Bohai Sea and North Yellow Sea. The predicted ice-freezing date, ice-ending date and ice periods are in fairly good agreement with observations, and some are even identical to measurements. Moreover, the simulation of maximum sea ice extent date matches well. Normally, the sea ice thickness of the west part in Liaodong bay is less than that of the east part, which can be reproduced well by the ice-ocean coupled model. However, during the melting period, simulated sea ice melts much faster than observations, and the model loses accuracy in simulation of specific ice thickness distribution.
机译:提供了为渤海和北黄海配置的一个精细分辨率耦合的冰海洋模型。在该耦合模型中使用了3.7km×2.8km的水平网格间距。季节性模拟是由1997/1998至2008/2009的冬季制作的。通过比较仿真结果和遥感图像,冰海耦合模型合理地再现了渤海和北黄海的海冰条件的季节变化。预测的冰冻冻结日,冰结束日期和冰期与观察结果相当愉快,有些与测量相同。此外,最大海冰范围日期的模拟匹配良好。通常情况下,辽东湾西部的海冰厚度小于东部的海冰厚度,可以通过冰海洋耦合模型进行良好繁荣。然而,在熔化时期,模拟海冰熔化得比观察结果快得多,并且模型失去了特定冰厚度分布的模拟中的精度。

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