摘要
作者以等效积温划分温度带,能避免出现水平温度带与垂直温度带指标界限不一致的缺点,用于秦岭及其山麓地区温度带的划分,符合该地区的实际。
The equation of equivalent accumulated temperature iswhere Th and p are the active accumulated temperature and the air density from meteorological stations respectively; h is altitude, p 0 is the air density at sea level; Te is equivalent accumulated temperature. Using .T e to divide vertical temperature zones in Qinling Mountain Range, the limiting indexes of temperature zones correspond with those of plain regions in the eastern part of China.
出处
《地理研究》
CSSCI
CSCD
北大核心
1992年第3期27-31,共5页
Geographical Research
关键词
气候
区划
等效温度
温度带
秦岭
Climate regionalization, temperature zone, equivalent accumutated temperature
