A need to revisit hydrologic responses to urbanization by incorporating the feedback on spatial rainfall patterns

被引:33
作者
Yang, Long [1 ]
Tian, Fuqiang [1 ]
Niyogi, Dev [2 ]
机构
[1] Tsinghua Univ, Dept Hydraul Engn, State Key Lab Hydrosci & Engn, Beijing 100084, Peoples R China
[2] Purdue Univ, Dept Agron, Dept Earth Atmosphere & Planetary Sci, W Lafayette, IN 47906 USA
基金
美国国家科学基金会;
关键词
Hydrologic response; Urbanization; Rainfall; Spatial heterogeneity;
D O I
10.1016/j.uclim.2015.03.001
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This study highlights the changes in the hydrologic responses to urbanization under idealized spatial heterogeneity in rainfall distribution. The study builds off recent assessments which show that urban areas modify the spatial rainfall pattern in its vicinity. Numerical experiments were conducted over an idealized watershed by prescribing different spatial patterns of rainfall and impervious coverage. Hydrologic responses were characterized by four metrics: flow distribution, daily variation, frequency of floods, and interannual runoff variability, as well as relative changes in flood magnitudes under different scenarios. Results indicate that hydrological response depends on both the spatial extent of urban coverage and the spatial patterns of rainfall. The most noticeable hydrologic variations and relative changes of flood magnitudes occur when the watershed is moderately urbanized (with 20-30% impervious coverage in the watershed). A factor separation scheme was employed to determine the synergistic effect of land surface and rainfall heterogeneity on flood magnitudes. Increases in flood magnitudes induced by urbanization could be underestimated by as much as 50% if spatial rainfall patterns are ignored. This study highlights the need for considering urban meteorological feedback while examining hydrologic responses to urbanization with both the changes of impervious coverage and spatial rainfall patterns considered. (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:128 / 140
页数:13
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