摘要
本文对Nickerson的中尺度模式作了一些修改,加入了地表热量平衡方程和一个13层的土壤层模式,并对Therry等的行星边界层参数化形式作了调整.使之较好地模拟出太阳辐射和地表温度的日变化.对不同地形、纬度和夏、冬季海陆风的模拟表明,本模式具有较强的海陆风模拟能力.
A modification version of the two-dimensional mesoscale model, originally developed by Nickerson et al., is used to study numerical experiments on the sea breeze circulation. Among the modifications to the model are the incorporation of a surface heat budget, a (13) layer soil model, a modified parameterization for the planetary boundary layer developed by Therry et al., as well as a more accurate numerical representation of the solar radiation at the model top and the surface temperature in the model. Some sea breezes over different terrain, at different latitudes and during the summer and the winter are simulated, thereby confirming the ability of the model to reproduce the known properties of this mesoscale phenomenon.
出处
《大气科学》
CSCD
北大核心
1993年第3期359-368,共10页
Chinese Journal of Atmospheric Sciences
