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首页> 外文期刊>Acta Meteorologica Sinica >Application and Study of Precipitation Schemes in Weather Simulation in Summer and Winter over China
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Application and Study of Precipitation Schemes in Weather Simulation in Summer and Winter over China

机译:降水方案在中国夏季和冬季天气模拟中的应用研究。

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摘要

Through simulation of summer and winter precipitation cases in China, the cloud precipitation schemes of model were examined. Results indicate that it is discrepant between convective precipitation simulated by the Kain-Fritsch (KF) scheme and Betts-Miller (BM) scheme in summer, the former scheme is better than the latter in this case. The ambient atmosphere may be varied by different convective schemes. The air is wetter and the updraft is stronger in the KF scheme than in the BM scheme, which can induce the more grid scale precipitation in the KF scheme, i.e., the different cumulus schemes may have the different and important effect on the grid scale precipitation. However, there is almost no convective rain in winter in northern China, so the effect of cumulus precipitation on the grid scale precipitation can be disregarded. Therefore, the gird scale precipitation is primary in the winter of northern China.
机译:通过对中国夏季和冬季降水情况的模拟,检验了该模型的云降水方案。结果表明,Kain-Fritsch(KF)方案模拟的对流降水与Betts-Miller(BM)方案模拟的夏季之间存在差异,在这种情况下,前者的方案要好于后者。周围大气可以通过不同的对流方案来改变。与BM方案相比,KF方案中的空气更湿润,上升气流更强,这可以在KF方案中诱发更多的网格规模降水,即不同的积云方案可能会对网格规模的降水产生不同而重要的影响。 。然而,中国北方冬季几乎没有对流降雨,因此可以忽略积雨对网格规模降水的影响。因此,网格规模的降水是中国北方冬季的主要降水。

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