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《Scientia Geographica Sinica》 1990-04
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Chen Mingrong (Department of GeoGraphy,Northwest University,Xi′an)  
The climate regions of China are distinguished by the equivalent accumulated temperature as the first index of temperature zone and aridity as the second index of climate type of moisture.The equation of equivalent accumulated tempearature is ΣT_e=(ρ_0/ρ)ΣT_h where ΣT_h and ρ are the active accumulated temperature,and the air density from meteorological stations,respectively;h is altitude;ρ_0 is the air density at sea level;ΣT_e is equivalent accumulated tempera- ture.Using equivalent accumulated temperature to divide temperature zone in both the Yunnan-Guizhou Plateau and the Qinghai-Xizang Pla- teau,the limiting indexes of temperature zones correspond to those of plain region of east China.
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Chinese Journal Full-text Database 10 Hits
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