A STUDY OF THE RADIATIOD BALANCE, HEAT BALANCE AND HEAT AND COLD SOURCES ON THE EARTH'S SURFACE IN EASTERN ASIA
Gao Guo-dong, Lu Yu-rong(Department of Meteorology. Naking University)
In this paper, we have suggested the following formulas for determining the total radiation (Q + q), the direct radiation (Q) and diffused radiation (q) :The value of effective outgoing radiation is given by E = E0(I - cn) The equation of heat balance for the land is R + LB + QA + P = 0 For annual period the heat balance equation is simplyE + LB + p = 0Using the routine meteorological observations of more than 300 stations, we have calculated with the formulas as mentioned above the amounts of the radiation balance, heat balance, heat and cold sources, and plotted a series of maps showing their distributions in eastern Asia. The features of their geographical distributions and annual variations are analyzed.