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2024年1月4日发(作者：win11安装oracle11g)
types of climate泛读总结
China has a marked continental monsoon climate
characterized by great parts of China are in the
northern temperate zone while parts of the southern area are
in the tropical or subtropical zone and parts of the northern
area in the Frigid Zone.
Most of China lies in the north temperature
zone,characterized by a warm climate and clear division between
seasons,a climate well suited for
winter,northerly winds from high latitude areas keep the
northern parts cold and dry;while in summer,monsoons from
eastern and southern coastal areas bring warmness and moisture.
The climate also varies with the extensive territory and
various topography from region to northern
China,summer is warm and short,while winter is cold and
southern China,summer is long,humid and hot,and the winter
short and warm,with temperature rarely below
central China(the valley area along the Yangtze
River),division between seasons is clear--summer is long,hot
and humid while winter,short and cold.
In northwestern China,such as Xinjiang and Inner
Mongolia,summer is dry and sweltering and winter is formidably
the Qinghai-Tibet Plateau(about 4,000 meters above sea
level)in southwestern China,winter is extremely cold and
summer is short and moderately warm,with little precipitation
and great difference in temperature between day and night.
Climate Zone
China sees various other types of climate due to its vast
ature belts from south to north appear in this
order:tropical zone,subtropical zone,temperate zone,medium
temperate zone and frigid temperate is also a
vertical climatic zone on the Qinghai-Tibet Plateau in
southwestern China.
Situated in the eastern part of the Asian continent and
facing the Pacific,China also has a prominent monsoon
addition,other types of climate,such as alpine
climate,plateau climate,desert climate,forest climate and
basin climate,coexist in China,due to complicated topography
and a great disparity in elevation.
Monsoon Climate
Most of China has a continental monsoon
September to April of the following year,the dry and cold winter
monsoon blow from Siberia and the Mongolian Plateau,resulting
in cold and dry winters and great differences in the
temperatures of northern and southern 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 difference in the temperatures
of northern and southern China.
In addition,cold wave,cyclone,intermittent drizzles and
typhoon are also the results of monsoon by
monsoon,the rainy season runs from May through to August and
typhoons frequently occur in the southeast coast between July
and September.
Precipitation
China has an average annual precipitation of 629
millimeters,which is unevenly distributed both regionally and
itation gradually declines from the
southeastern area to the
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