GETM模型的验证模拟了波罗的海主要流入盐水输送路径的长期盐度场

I. Maljutenko, U. Raudsepp
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引用次数: 14

摘要

利用水动力模式GETM对1966 ~ 2005年波罗的海的水文条件进行了模拟。利用Bornholm盆地、Gotland盆地、芬兰湾和里加湾四个监测站的地表和底部盐度和底部温度的时间序列进行模型验证。该模式通过80年代的停滞期和多次波罗的海大流入事件的模拟期再现了现实条件。模拟的不同深度的盐度和温度与实测结果吻合较好。同时,将海平面和最大冰面积与观测值进行了比较。
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Validation of GETM model simulated long-term salinity fields in the pathway of saltwater transport in response to the Major Baltic Inflows in the Baltic Sea
The hydrodynamic model GETM was used to simulate the hydrographic conditions in the Baltic Sea for the hindcast period from 1966 to 2005. Time series of surface and bottom salinity and bottom temperature at four monitoring stations belonging to the Bornholm Basin, Gotland Basin, the Gulf of Finland and the Gulf of Riga were used for model validation. The model has reproduced realistic conditions through the simulation period that was characterized by stagnation period in the 80s and numerous Major Baltic Inflow events. The simulated salinity and temperature at different depths were in good agreement with measurements. Also, the sea level and maximum ice extent were compared with observations.
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