摘要
本文利用３６年月平均地表气温和月降水量资料来探讨华南地区的气候季节的划分，发现用温度和降水组成的矢量场对华南气候进行季节划分比单用温度或降水量场来划分要合适一些，所得结果与人们习惯的根据太阳辐射变化而划分的春夏秋冬有很大差异。
In this paper,the division of seasons for the south China region is discussedby using monthly mean temperature and monthly precipitation for 36 years. The resultsshow:the division of seasons by using temperature-precipitation vector field is more res-onable than by using temperature or precipitation field only, and is much different fromthe traditional division according to the change of solar radiation.
出处
《中山大学学报（自然科学版）》
CAS
CSCD
1994年第2期131-133,共3页
Acta Scientiarum Naturalium Universitatis Sunyatseni
关键词
华南
气候季节
气温
降水量
the south China region, division of seasons,temperature,precipitation.
