The Yangtze is the longest and most economically important river in Asia and the fifth largest in the world in terms of flow. It is also the largest river entirely within a single country. Its estuary had an estimated annual flow of 995.8 km/a (31,550 m/s) between 1955 and 2021.
The last gauging station on the river is at Datong (30°50′57.9192″N 117°43′47.4096″E / 30.849422000°N 117.729836000°E / 30.849422000; 117.729836000 ). At this location, the water flow is regularly monitored. The chart below is based on average flows between 1950 and 2020.
1950–1970
Year
Average discharge (m/s)
1950
30,880
1951
26,167
1952
33,456
1953
28,272
1954
43,062
1955
29,215
1956
26,388
1957
25,696
1958
26,860
1959
24,500
1960
24,282
1961
27,800
1962
29,403
1963
27,455
1964
32,513
1965
27,581
1966
24,376
1967
27,675
1968
29,340
1969
27,518
1970
31,100
1971–1990
Year
Average discharge (m/s)
1971
22,680
1972
22,021
1973
33,706
1974
26,450
1975
31,444
1976
26,262
1977
28,617
1978
21,415
1979
22,962
1980
32,065
1981
28,340
1982
30,737
1983
35,822
1984
28,178
1985
26,591
1986
23,190
1987
27,342
1988
27,596
1989
31,093
1990
27,430
1991–2020
Year
Average discharge (m/s)
1991
28,813
1992
25,325
1993
31,516
1994
24,697
1995
31,672
1996
30,133
1997
24,602
1998
45,970
1999
34,752
2000
28,908
2001
23,064
2002
32,489
2003
28,593
2004
23,283
2005
33,589
2006
17,376
2007
22,497
2008
25,640
2009
23,032
2010
37,266
2011
15,962
2012
36,386
2013
23,220
2014
29,567
2015
30,824
2016
33,878
2017
30,186
2018
21,150
2019
29,163
2020
34,763
References
Jinyou, Lu; Yonghui, Zhu; Zhongwu, Jin; Xiaohu, Guo; Chao, Guo; Peng, Chen; Yanjun, Wang; Chengwei, Hu; Yuan, Yuan (2023). "Evolution of the main channel of the Yangtze River" . Scientific Research Institute : 283–306. doi :10.1002/rvr2.52 .
"The BOH" .
Yunping, Yang; Mingjin, Zhang; Jinhai, Zheng; Lingling, Zhu (2023). "Sediment sink-source transitions in the middle and lower reaches of the Yangtze River estuary" . Frontiers in Marine Science . 10 . doi :10.3389/fmars.2023.1201533 .
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