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
ΣTe=（ρ0/ρ）ΣTh
where ΣTh and ρ are the active accumulated temperature,and the air density from meteorological stations,respectively;h is altitude;ρ0 is the air density at sea level;ΣTe is equivalent accumulated temperature.Using equivalent accumulated temperature to divide temperature zone in both the Yunnan-Guizhou Plateau and the Qinghai-Xizang Plateau,the limiting indexes of temperature zones correspond to those of plain region of east China.
Chen Mingrong
. A PRELIMINARY STUDY ON CLIMATE RE-GIONALIZATION IN CHINA[J]. SCIENTIA GEOGRAPHICA SINICA, 1990
, 10(4)
: 308
-315,387
.
DOI: 10.13249/j.cnki.sgs.1990.04.308
[1] 中国科学院自然区划工作委员会:中国气候区划(初稿),科学出版社,1959年.
[2] 中央气象局编制:中国气候区划,载中国气候图集,地图出版社,1976年.
[3] 丘宝剑、卢其尧.中国农业气侯区划试论,地理学报,35(2), 1980年.
[4] 陈咸吉:中国气候区划新探,气象学报,40(1), 1982年.
[5] 丘宝剑.中国农业气候区划再论,地理学报,38(2), 1983年.
[6] L.P.史密斯(于系民译):农业气象学方法,农业出版社,1981年.
[7] 陈明荣:试论平原与高原气温的不等效性,气候研究——天地生相互影响问题(纪念么忱生教授从事气象工作和教育五十周年专刊),气象出版社,1988年.
[8] 林振耀、吴样定:青藏高原气候区划,地理学报,36(1),1981年.
[9] Penman, H. L,; Woburn irrigation 1951-1959, J. Agri. Sci., Vol,58, Parts,1962,
[10] Robertson, G. W.;作物气象生态译丛,农业出版社,1984年.
