The earth s climatic changes show regular periodicities on the time scale of 10~100 ka, which are controlled by orbitally modulated variations in insolation and which can be calculated with great precision for several Ma.
In this article, the calibration method of spectral pyranometers is discussed in detail.
详细讨论了分光总日射表的校准方法。
Based on GMS data of cloud amount during 1992—1994,the distribution of solar energy resource over Tibet region were studied with the help of the non linear relationship between cloud amount and percentage of sunshine and the linear relationship between the later and global radiation Mean while the distributions were corrected through the comparison between cloud amount of 1992—1994 and normal