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Changes in river networks and their storage and regulation capacities in the Rapidly Urbanized Taihu Basin, China
Author(s) -
Xu Yu,
Xu Youpeng,
Wu Lei
Publication year - 2018
Publication title -
hydrological processes
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.222
H-Index - 161
eISSN - 1099-1085
pISSN - 0885-6087
DOI - 10.1002/hyp.13257
Subject(s) - tributary , drainage basin , urbanization , flood control , hydrology (agriculture) , drainage , environmental science , drainage density , flood myth , china , floodplain , structural basin , geography , physical geography , geology , ecology , geomorphology , cartography , geotechnical engineering , archaeology , biology
Abstract Owing to the crucial environmental and hydrological functions of river systems and intensive human disturbance, further investigations of their change patterns and flood control functions are urgently needed. The Rapidly Urbanized Taihu Basin (RUTB) was selected as the study region to investigate changes in the river networks, the relationship between changes in river systems and urbanization, and the changes in the static drainage storage capacity ( SC ) and regulation capacity ( RC ) from the 1980s to the 2010s. The results indicated that the total drainage density in RUTB decreased by 10.17%. For the first‐, second‐, and third‐order rivers, the changes are +7.61%, −14.35%, and −17.84%, respectively. Spatially, the change pattern of the third‐order river drainage density displayed significant spatial clustering. The ratio of main to tributary river length ( Rmt ) was increased from 0.31 in the 1980s to 0.39 in the 2010s. Spatially, the drastic increases were found in the south‐east of Wu–Cheng–Xi–Yu, the east of Yang–Cheng–Dian–Mao, and the central southern part of Hang–Jia–Hu. Results moreover show that urbanization has the greatest influence on the third‐order drainage density, especially around the secondary and rapidly developing cities. The demand for flood control has led to a slight increase in the density of main rivers. The values of SC and RC decreased by 0.69% and 40.61% in RUTB, respectively. These changes were mainly concentrated around the major cities and urban corridors. The decrease in SC was caused by the decay of the river system, and the reduction in RC was caused by a combination of river system degradation and increase in ordinary water levels.