总辐射光当量及其在光气候计算中的应用

THE LIGHT EQUIVALENT OF TOTAL SOLAR RADIATION AND ITS APPLICATION IN THE CALCULATION OF ILLUMINATION CLIMATE

  • 摘要: 本文根据1983—1984年全国14个不同气候特点的日射站每日逐时照度与日射同步观测资料计算了总辐射光当量值,提出用纬度、海拔高度、地面平均绝对湿度和日照时数建立计算总辐射光当量的多元回归方程。用14个测站全年和各月平均总辐射光当量值检验所建立多元回归方程计算的相应总辐射光当量值表明,计算值的相对误差均小于10%。我们用14个测站资料建立的计算总辐射光当量回归方程计算了全国464个测站的总辐射光当量值。总照度可由总辐射光当量与总辐射的乘积获得。根据各测站的总辐射光当量和总辐射值,便可计算出这些测站的光气候值,绘制我国光气候图。

     

    Abstract: From 1983 to 1984, 14 solar radiation observation stations which are located in different parts of our country and with different climate features were chosen for the simultaneous observation of natural illumination with solar radiation hourly every day. In this paper, according to the data the light equivalent of total solar radiation has been given. A multivariate regression equation to calaulate the annual and monthly mean values of the light equivalent of total solar radiation at 14 observation stations is formed.The variables of the equation include latitude, elevation,mean absolute humidity on the surface and the hours of sunshine.The result of the equation shows that the relative error is less than 10 percent.The light equivalents of total solar radiation for 464 observation stations were calculated by means of the multivariate regression equations which were obtained upon the data of 14 observation stations. The total illumination is given by the light equivalent of total radiation multiplying the total radiation.The climate values of total illumination for each station are also calculated according to its light equivalent of total radiation and total solar radiation value. Finally, the climate charts of total illumination for our country have been drawn.

     

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