For temperature in this region, its annual and daily periodis varation are influenced strongly by cloud and rain acting; its change of year to year is identical with home and abroad. In some district there are the maximum elevation of dally range and the minmumelev alion of annual range of temperature. But they are different from maximum elevation of precipitation. There are better correlation between themal climatic elements, they possess more and less alike distributive law of space, and longitudinal latitudinal effect and elevation effect and its secondary effect. And it has become possible to the castimate in quantilty these themal clements for the district of a lack of meteorological station.