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Tu Xiaoling,Zhou Mingyu,Sheng Shaohua.The mesoscale numerical simulation of the flow field of the Hainan Island and the Leizhou Peninsula[J].Acta Oceanologica Sinica,1993,(2):219-235
The mesoscale numerical simulation of the flow field of the Hainan Island and the Leizhou Peninsula
The mesoscale numerical simulation of the flow field of the Hainan Island and the Leizhou Peninsula
投稿时间:1992-05-25  修订日期:1992-06-20
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Tu Xiaoling National Research Center for Marine Environmental Forecast, Beijing 100081, China 
Zhou Mingyu National Research Center for Marine Environmental Forecast, Beijing 100081, China 
Sheng Shaohua National Research Center for Marine Environmental Forecast, Beijing 100081, China 
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中文摘要:
      The flow field over Hainan Island and the Leizhou Peninsula in summer and winter is discussed with three-dimensional mesoscale model developed in the University of Virginia and using the representative meteorological data of January and July.
Simulation results indicate that the local weather characteristics over the Hainan Island are distinctly influenced by the Wuzhi Mountain terrain. The cloudy or rainfall weather over the northeast of the Wuzhi Mountain occurs easily, under proper large-scale conditions of flow, temperature and humidity. while west wind prevails. The overcast or rainfall weather is often induced by strong convection in the afternoon over west of the Hainan Island under easterly prevailing wind.
英文摘要:
      The flow field over Hainan Island and the Leizhou Peninsula in summer and winter is discussed with three-dimensional mesoscale model developed in the University of Virginia and using the representative meteorological data of January and July.
Simulation results indicate that the local weather characteristics over the Hainan Island are distinctly influenced by the Wuzhi Mountain terrain. The cloudy or rainfall weather over the northeast of the Wuzhi Mountain occurs easily, under proper large-scale conditions of flow, temperature and humidity. while west wind prevails. The overcast or rainfall weather is often induced by strong convection in the afternoon over west of the Hainan Island under easterly prevailing wind.
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