陆面过程的参数化方法是大气物理学家研究的重点，也是水文学家越来越关注的问题。
Methods for land surface process parametrization are a focal point for atmospheric physicists to investigate, and also a problem for hydrologists to be increasingly concerned about.
为改进陆面过程的参数化，初步探讨了模式中陆面气象要素次网格尺度不均匀性分布对模拟计算结果的影响。
To improve the parameterization of land surface processes, a preliminary analysis of the impact of subgrid land surface heterogeneity on model results is carried out.
许多大气模式中虽然考虑了陆面水文过程，但与目前常用的水文模型相比，大气模式中的陆面参数化方案大都比较简单。
Although most GCMs include land surface hydrological processes, the land surface parameterization in GCMs are still simpler than the common used hydrological model.
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