Assessing the impacts of human interventions and climate change on fluvial flooding using CMIP6 data and GIS-based hydrologic and hydraulic models

被引:12
|
作者
Mahato, Purushottam Kumar [1 ]
Singh, Dharmaveer [2 ]
Bharati, Birendra [1 ]
Gagnon, Alexandre S. [3 ]
Singh, Bhupendra Bahadur [4 ]
Brema, Javanarayanan [5 ]
机构
[1] Cent Univ Jharkhand, Dept Water Engn & Management, Ranchi, Bihar, India
[2] Symbiosis Int Deemed Univ, Symbiosis Inst Geoinformat, Pune, Maharashtra, India
[3] Liverpool John Moores Univ, Sch Biol & Environm Sci, Liverpool, Merseyside, England
[4] Ctr Climate Change Res, Indian Inst Trop Meteorol, Minist Earth Sci, Pune, Maharashtra, India
[5] Karunya Inst Technol & Sci Deemed Univ, Dept Civil Engn, Coimbatore, Tamil Nadu, India
关键词
Fluvial flooding; land use; land cover; GIS-based hydrologic and hydraulic models; climate change; Brahmani River Basin; LAND USE/COVER CHANGE; SUTLEJ RIVER-BASIN; HEC-HMS MODEL; SURFACE RUNOFF; COVER CHANGE; RISK; URBANIZATION; CATCHMENT; DISTRIBUTIONS; UNCERTAINTY;
D O I
10.1080/10106049.2022.2060311
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 presents an approach for modelling and mapping fluvial flooding, considering both land use/land cover (LULC) change and climate change, and applies it to the Brahmani River Basin in eastern India. Climate change projections were obtained from the Coupled Model Intercomparison Project Phase 6 (CMIP6), and their impacts on the hydrology of the catchment were investigated using HEC-HMS and HEC-RAS software. Results reveal that changes in LULC types, specifically an increase in proportions of agricultural and built-up areas and a decrease in forest cover, as undergone between years 1985 and 2018, have increased peak discharge following a storm, thereby causing an increase in spatial extent of floods of different return periods. Moreover, downscaled climate change scenarios from two General Circulation Models were used to determine potential changes in river discharge according to two GHG emission scenarios from the latest IPCC: SSP245 and SSP585. The projections indicate that peak discharge and the spatial extent of flooded areas will increase for floods with return periods ranging from two to 100 years. This study demonstrates the important influence that changes in LULC have had on the susceptibility of the BRB to flooding, with climate change projected to further enhance the risk of flooding as the century progresses.
引用
收藏
页码:11483 / 11508
页数:26
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