摘要
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.
The impacts of winter snow cover of Tibetan Plateau on the precipitation of East China during Meiyu season are studied by using IAP 2 layer AGCM model. The results show that the precipitation in southern East China during Meiyu season decreases when winter snow cover of Tibetan Plateau increases, and the precipitation in the most part of East China during Meiyu season increases a little when winter snow cover of Tibetan Plateau decreases.
出处
《应用气象学报》
CSCD
北大核心
1997年第A00期110-115,共6页
Journal of Applied Meteorological Science
关键词
青藏高原
冬季
积雪
梅汛期
数值试验
降水
Tibetan Plateau Winter snow cover East China Meiyu season Numerical experiment