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                Climate

                  Sichuan is located in the transitional zone between Qinghai-Tibet Plateau and the eastern plains and therefore has complex and diverse climates with rather obvious regional differences and vertical changes. There are distinct disparities between east and west Sichuan as well. Sichuan is generally divided into three major climate zones: humid subtropical climate zone of Sichuan Basin, sub-humid and subtropical climate zone of southwest Sichuan’s mountainous regions, and alpine climate zone of high mountains and plateaus of northwest Sichuan.

                  The overall characteristics of Sichuan’s climate can be summarized as follows: monsoon climate is obvious and rain and heat happens in the same seasons; regional climate differences are prominent in that the east is characterized by warm winters, early springs, hot summers, rainy autumns, much cloud and fog, little sunshine and a long growing season while the west is characterized by coldness, long winters, almost no summer, sufficient sunshine, concentrated rainfall and distinct dry and rainy seasons; vertical climate changes are significant and climate types are varied; meteorological disasters happen in various forms with a high frequency and large scope, which are mainly droughts, rainstorms, floods and cold weather.

                 
                 
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