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利用ＩＡＰ－２层ＡＧＣＭ模式，研究了青藏高原冬季积雪状况对华东地区梅汛期降水分布的影响．发现高原隆冬季节积雪多时，华东南部梅汛期降水减少；积雪少时，华东大部梅汛期降水略有增加．
Based on the IAP-2 AGCM model, the effect of winter snow cover over the Tibetan Plateau on the precipitation distribution during the flood season in East China was studied. During the flood season in the plateau, the precipitation decreased in May flood season in eastern China. When the amount of accumulated snow was small, the precipitation in most of East China during May flood season increased slightly.