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Click Yearly Climate Info
China has a marked continental monsoonal climate
characterized by great variety. Most parts are
in the northern temperate zone while the southern
areas are in the tropical or subtropical zone
and northern areas in the frigid zone.
Most parts of China have clear division between
seasons. In winter, northerly winds from high
latitude areas keep the northern part cold and
dry, while in summer, monsoons from southern coastal
areas bring warm and moisture. In addition, the
climate also varies with the extensive territory
and various topography from region to region.
In north China, such as Xinjiang and Inner Mongolia,
summer is dry and sweltering while winter is formidably
cold. Sandstorms sometimes occur in April in this
area, especially in the Inner Mongolia and Beijing
area.
On the Tibet-Qinghai plateau (about 4,000m above
sea level), winter is long and extremely cold
while summer is short and moderately warm. There
is little precipitation in this area and the temperature
fluctuation is great between day and night.
In central china (the valley along where the Yangtze
River travel), summer is long, hot and humid while
winter is short and cold. In the areas south of
the Yangtze
River, temperature rarely falls below freezing.
In the far south, areas around Guangzhou, the
summer is long, humid and hot while the winter
is short and comfortable,a paradise considered
by many northerners. The rainy season runs from
May through August and typhoons frequently occur
in the southeast coast between July and September.
For detailed information about the Average, Maximun
and Minimum temperatures and the rainfall in Major
Chinese Cities, see our Yearly
Climate Info
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