|
Jiangsu Province is located in East China and occupies the southern
part of the North China plains and the plains of the Lower Reaches
of the Yangtze River. In the eastern part of the province the
coastline of the Yellow Sea extends as long as over 1,000 kilometers.
Jiangsu Province is adjacent to Shanghai on the east, to Zhejiang
Province on the north, to Anhui Province on the west and to Shandong
Province on the north. It covers an area of more than 100,000
square kilometers, with a population of 65,350,000. The population
density comes out first in China. Most people are of Han Nationality
and some are of Hui Nationality and Man Nationality. The name
"Jiangsu" comes from the combination of the first Chinese
character of "Jiang Ning" and "Su Zhou" (two
prefectures in the Qing Dynasty); its short form is "Su".
The provincial capital is Nanjing.
Topography
The provincial topography is characteristic of plains, with the
majority of places less than 50 meters above sea level. Hilly
land occupies 5% of the provincial area. To the north of Nantong-Yangzhou
Canal is the Huanghuai Plain of North Jiangsu, part of the North
China Plains. Alluvial deposits are widely distributed in the
areas formerly flooded by the Yellow River. Near the Yellow River
there is saline-alkali soil. Lixiahe Area of North Jiangsu refers
to the plain region between the Great Canal and Chuanchang River
to the south of the North Jiangsu General Irrigation Canal. Its
surrounding area is higher than the central part which is less
than 2 meters above sea level, commonly known as "the pan
bottom region". Near Xuzhou and Lianyungang to the north
of the Huanghuai Plain there are remaining hills of Shandong Hills
extending south. Among them hills in Xuzhou area are about loo
meters above sea level, and hills in Lianyungang area about 200
meters above sea level. Yuntai Mountain, as high as 625 meters
above sea level, is the highest mountain in Jiangsu Province.
The Plains of the Lower Reaches of the Yangtze River starts from
Zhenjiang at the western end of the Yangtze River Delta, adjoins
the Plain of North Jiangsu and reaches into the area of Hangzhou
Bay, Zhejiang Province. Most parts of the Plain are normally 2
to 8 meters above sea level and formed by the alluvion of the
Yangtze River. In the higher region of the west there are many
hills, lakes, marshes, ditches and canals. To the south of Yangtze
River is the Plain of South Jiangsu shaped like a plate, with
Lake Tai as the center. The main mountain ranges of the Province
are the Ning Zhen Mountain Range from Nanjing to Zhenjiang on
the western side of the Yangtze River Delta, Maoshan Hills extending
east at the border between Jiangsu Province and Anhui Province,
and Yi Li Hilly Land, which is 300--500 meters above sea level,
between Jiangsu Province and Zhejiang Province. Foothills and
river valleys are plentiful and widespread. In the Ning Zhen Hilly
area Mount Zhong (the Purple Mountain), Mount Tang, Mount Qixia,
Mount Qinglong and Mount Mao are all famous mountains.
Climate
Jiangsu Province is situated in the temperate zone and subtropical
zone, with a humid and semi-humid monsoon climate. China's dividing
line between the temperate zone and the subtropical zone is the
belt between the Huaihe River of Jiangsu Province and North Jiangsu
General Irrigation Canal. The annual average temperature is 130C-160C,
-20C-40C in January, and 260C-290C in July. The highest extreme
temperature is 40.90C (in Zhenjiang on August 22, 1959). Nanjing
area is one of the three well-known "furnaces" in the
Yangtze River basin in the summer season of China. The lowest
extreme temperature is -23.10C (at Qingyi Lake of Shuyang on February
5,1969). The frost-free period lasts about 200--240 days. There
is heavy precipitation in the southeastern part and light precipitation
in the northwestern part. The annual average precipitation is
about 800-1200 millimeters. The recorded heaviest precipitation
of a day is 314.3 millimeters (in Dongtai City on August 21,1965).
There is more rain when plums are ripe at the time when spring
is changing into summer. It rains for a short time, but frequently.
It is a common phenomenon that it is raining while the sun is
shining. Rains of this period are generally called "plum
rains". But on the other hand, because of damp climate and
appropriate temperature, mould grows quickly, so this period is
also called "mould rains". Typhoons often hit this province
at the end of summer and the beginning of autumn.
Rivers and Lakes
There are three large water systems: the Yangtze River, the Huaihe
River and the Shuhe River, all flowing from west to east. The
Great Canal links up south and north. This province has a crisscross
network of rivers and many lakes. In the Lower Reaches of the
Yangtze River, the part of the River from Nanjing to Zhenjiang
is about 1 or 2 kilometers wide. From Jiangyin downward the River
becomes wider, and the widest part is between Nantong and the
estuary, being as wide as more than 18 kilometers. As a result
of the change of the course of the Yellow River, mud and sand
deposit in the Huaihe River, and make the water form Hongze Lake
when it flows into the area of Jiangsu Province. The water of
Hongze Lake passes southward through Gaoyou Lake and by Jiangdu
and enters the Yangtze River at Sanjiangying. Other major rivers
in the North Jiangsu Plain are Shuhe River, Xinyi River, Xinzegang
River, Doulonggang River, Dongtai River and the North Jiangsu
General Irrigation Canal, all flowing into the Yellow Sea from
west to east. Moreover, Tongyu Canal and Tongyang Canal link up
ports, rivers, ditches and canals from east to west and from south
and north in the Lixiahe area of North Jiangsu, thus forming a
region with a complex network of rivers and lakes. Of all the
lakes, Lake Tai to the south of the Yangtze River is the largest
in area, occupying 2,425 square kilometers. Some people believe
that Lake Tai was formed by the asteroids hitting the lake. The
second largest is Hongze Lake, with an area of 1,960 square kilometers.
|