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气流通过水域时的变性 被引量:3

TRANSFORMATION OF AIRFLOW PASSED THROUGH THE WATER AREAS
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摘要 利用量纲分析和数理方法推得了可用解析函数表示的气流通过水域时各气象要素在水上和下风岸陆地上变化的公式,并用1982年1,4,7,10月在江苏兴化县大纵湖专门布点进行水域气候效应系统观测的资料对所得公式进行检验。 In this paper,a model simulating the transformation of airflow passed through the water areas is presented,the model expressing the variations of meteorological elements over the waters is formula (44),(45) and over the downwind land is formula (48).The calculating results(continuing curves) and observational data (dots) of Dazong Lake in Xinghua County of Jiangsu Province are shown in fogure 1-5,which show that the theoretical curves are in good agreement with observations.
作者 傅抱璞
出处 《气象学报》 CSCD 北大核心 1997年第4期440-452,共13页 Acta Meteorologica Sinica
基金 国家教委博士点基金
关键词 水域 气流 变性 大气观测 Waters,Airflow,Transformation.
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  • 7Raymond W. Arritt. The effect of water surface temperature on lake breezes and thermal internal boundary layers[J] 1987,Boundary - Layer Meteorology(1-2):101~125
  • 8Y. Kodama,Dr. F. Eaton,Prof. Dr. G. Wendler. The influence of Lake Minchumina, Interior Alaska, on its surroundings[J] 1983,Archives for Meteorology, Geophysics, and Bioclimatology Series B(3):199~218
  • 9R. G. Bill,R. A. Sutherland,J. F. Bartholic,E. Chen. Observations of the convective plume of a lake under cold-air advective conditions[J] 1978,Boundary - Layer Meteorology(4):543~556

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