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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:1997/1998年冬季以来渤海和北黄海冰海耦合模式的季节性模拟

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A fine-resolution coupled ice-ocean model configured for the BohaiSea and North Yellow Sea is presented. A horizontal grid spacing of3.7km×2.8km was used in this coupled model. Seasonal simulationswere made from the winters of 1997/1998 to 2008/2009. By comparingof the simulation results and the remote sensing images, the ice-oceancoupled model reasonably reproduces the seasonal variations of the seaice conditions in the Bohai Sea and North Yellow Sea. The predictedice-freezing date, ice-ending date and ice periods are in fairly goodagreement with observations, and some are even identical tomeasurements. Moreover, the simulation of maximum sea ice extentdate matches well. Normally, the sea ice thickness of the west part inLiaodong bay is less than that of the east part, which can be reproducedwell by the ice-ocean coupled model. However, during the meltingperiod, simulated sea ice melts much faster than observations, and themodel loses accuracy in simulation of specific ice thickness distribution.
机译:提出了为渤海和北黄海配置的高分辨率高分辨率冰洋耦合模型。在该耦合模型中使用了3.7km×2.8km的水平网格间距。从1997/1998年至2008/2009年冬季进行了季节性模拟。通过将模拟结果与遥感图像进行比较,冰海耦合模型合理地再现了渤海和北黄海海况的季节性变化。预测的冰冻日期,结冰日期和冰期与观测值相当吻合,有些甚至与测量值相同。此外,最大海冰延伸时间的模拟也很匹配。通常,辽东湾西部的海冰厚度小于东部的海冰厚度,可以通过冰海耦合模型很好地再现。但是,在融化期间,模拟的海冰融化的速度比观测值快得多,并且该模型在模拟特定冰厚度分布方面失去了准确性。

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