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Frontiers of Environmental Science & Engineering

ISSN 2095-2201

ISSN 2095-221X(Online)

CN 10-1013/X

Postal Subscription Code 80-973

2018 Impact Factor: 3.883

Front Envir Sci Eng    2013, Vol. 7 Issue (5) : 769-776    https://doi.org/10.1007/s11783-013-0542-z
RESEARCH ARTICLE
Land use/cover change effects on floods with different return periods: a case study of Beijing, China
Yueling WANG1, Xiaoliu YANG2()
1. Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; 2. College of Urban and Environmental Sciences, Peking University, Beijing 100871, China
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Abstract

In this study, an approach integrating digital land use/cover change (LUCC) analysis, hydraulic modeling and statistical methods was applied to quantify the effect of LUCC on floods in terms of inundation extent, flood arrival time and maximum water depth. The study took Beijing as an example and analyzed five specific floods with return periods of 20-year, 50-year, 100-year, 1000-year and 10000-year on the basis of LUCC over a nine-year period from 1996 to 2004. The analysis reveals that 1) during the period of analysis Beijing experienced unprecedented LUCC; 2) LUCC can affect inundation extent and flood arrival time, and floods with longer return periods are more influenced; 3) LUCC can affect maximum water depth and floods with shorter return periods are more influenced; and 4) LUCC is a major flood security stressor for Beijing. It warns that those cities having experienced rapid expansion during recent decades in China are in danger of more serious floods and recommends that their actual land use patterns should be carefully assessed considering flood security. This integrated approach is demonstrated to be a useful tool for joint assessment, planning and management of land and water.

Keywords inundation extent      flood arrival time      maximum water depth      shallow flow model     
Corresponding Author(s): YANG Xiaoliu,Email:xlyang@urban.pku.edu.cn   
Issue Date: 01 October 2013
 Cite this article:   
Yueling WANG,Xiaoliu YANG. Land use/cover change effects on floods with different return periods: a case study of Beijing, China[J]. Front Envir Sci Eng, 2013, 7(5): 769-776.
 URL:  
https://academic.hep.com.cn/fese/EN/10.1007/s11783-013-0542-z
https://academic.hep.com.cn/fese/EN/Y2013/V7/I5/769
Fig.1  The topographic elevation of Beijing
Fig.2  Framework of the 2D SFM
from1996to 2004
1234567total 1996
11199.9247.4131.7237.26252.6682.42138.021789.41
245.16167.024.130.0429.778.3383.9368.32
334.516.9537.832.9639.146.5212.33140.24
467.192.35.14636.36114.8473.75598.061587.55
5533.7182.9283.16173.11936.94191.77327.553329.15
6110.9427.257.5374.56152.98421.83221.321016.41
7116.12216.885.04538.46189.97218.464782.376067.3
total 20042107.46640.73174.521492.742716.31003.086163.55
C0.180.740.24-0.06-0.18-0.010.02
A318.05272.4134.28-94.81-612.85-13.3396.25
B35.3430.273.81-10.53-68.09-1.4810.69
Tab.1  Cross tabulation matrix of LUCC in Beijing 1996-2004.
land use/coverManning roughness coefficient
urban land (incl. rural road, town land, rural residence and mining land, railway, highway, airports, ports and wharfs)0.016
bare land (incl. saline alkali land, swamp, sand land, bare rock, threshing ground specially designated land and unutilized land)0.025
ponds (incl. aquaculture)0.027
grassland (incl. reed and mudflat)0.03
cultivated land (incl. pasture, irrigation and water conservancy works, ridge, river, lake, reservoir, confined feeding operations, green house and aquatic operations)0.035
heavy brush0.075
forest0.15
Tab.2  Manning roughness coefficients corresponding to land use/cover (summarized from [27] and [28])
Fig.3  The flood hydrographs with different flood return periods upstream from Beijing
Fig.4  Flood extent of the five floods: (a) 20-year; (b) 50-year; (c) 100-year; (d) 1,000-year; (e) 10,000-year (Green- flooded in both 1996 and 2004; Blue- flooded in 2004)
Fig.5  Inundation extent differences of the five floods between 1996 and 2004 along flooding time
Fig.6  Cumulative areal distribution of the difference of maximum water depth at grid cells between 1996 and 2004
Fig.7  Cumulative areal distribution of the difference of flood arrival time of the five floods between 1996 and 2004
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