中国的大部分地区位于北温带，气候温和，四季分明，适宜人类居住与生存。大陆性季风气候是中国气候的主要特点。每年9月至次年4月，干寒的冬季风从西伯利亚和蒙古高原吹来，寒冷干燥，南北温差甚大。每年的4月至9月，暖湿的夏季风从东部和南
部海洋吹来，普遍高温多雨，南北温差甚小。中国从南至北呈现出赤道带、热带、亚热带、暖温带、温带、寒温带六个温度带；降水量从东南向西北逐渐减少，各地年平均降水量差异很大，东南沿海可达1500毫米以上，而西北内陆还不到200毫米。
China lies mainly in the north temperate zone, characterized by a warm climate and distinctive seasons, with a climate well suited for habitation. From September to April the following year, dry and cold winter monsoons blow from Siberia and the Mongolian Plateau, resulting in cold and dry winters and great differences in the temperatures of north and south China. From April to September, warm and humid summer monsoons blow from the seas in the east and south, resulting in overall high temperatures and plentiful rainfall, and little differences in the temperatures of north and south China. In terms of temperature, the nation can be sectored from south to north into equatorial, tropical, subtropical, warm-temperate, temperate, and cold-temperate zones. Precipitation gradually declines from the southeastern coastal areas to the northwestern inland areas , and the average annual precipitation varies greatly from place to place. In southeastern coastal areas, it reaches over 1,500 mm, while in northwestern areas, it drops to below 200 mm.
