摘要
本文利用东北地}9个日射站、3个探空站的实测资料,建立了计算该区域总辐射和冷季各月地表反射率的经验公式,确定了M.E.别尔梁德有效辐射经验公式中的云减弱系数,对东北地区辐射平衡各分量进行了细致计算。在此基础上,探讨了东北地区地表面辐射平衡的分布规律及其成因。
In the paper northeast China refers to Heilongjiang,Jilin and Liao- ning provinces.There are nine insolation-observing stations in northeast China.The equations of total radiation and ground albedo in winter are established based on the solar radiation data and climatic data from the nine insolation-observing stations from 1961 to 1980. The equation of total radiation is Q=S_0(a+bS)where,Q is total radiation;So is astronomical radiation;S relative sunshine;a and b regression coefficients. The equation of ground albedo in winter is A=0.331765+0.332506n/N-0.005886H where,A is ground albedo;n days of snow cover;N days of each month in winter;H the sun's altitude. For effective radiation,the following equation is adopted: E=0.95σ[(0.39-0.058e^(1/2)T^4+(T_0~4-T^4)](1-Cn) where,E is effective radiation;σ Stefan-Boltzman constant,which eq- uals 5.68E-8;T_0,T,e,n and C represent the means of ground tempera- ture,air temperature,absolute humidity,cloudiness and a coefficient, respectively. The annual and monthly values of total radiation,effective radiation and net radiation for 166 stations in northeast China are calculated. Their characteristics of distribution in space and time are discussed. The results indicate that northeast China is rich in solar radiation res- ource.The amounts of annual total radiation,annual effective radiation and annual net radiation are 4100-5300MJ/m^2,1600-2200MJ/m^2,and 1470-2480MJ/m^2,respectively.In respect to the spatial distribution,the annual total radiation in south is more than that in north.There is an increasing tendency of total radiation from east to west.The effective radiation increases from east to west,and the net radiation decreases from south to north.As for the annual variation,the smallest and lar- gest monthly values of total radiation and net radiation are in Decem- ber,and May or June,respectively;the smallest monthly value of effec- tive radiation is in February or July,and the largest in March.
出处
《地理科学》
CSSCI
CSCD
北大核心
1990年第4期338-346,共9页
Scientia Geographica Sinica
关键词
地表
辐射平衡
总辐射
反射率
Total radiation
Effective radiation
Ground albedo
Net radiation
