Hydrometeorological consequences on the water balance in the Ganga river system under changing climatic conditions using land surface model

被引:8
|
作者
Ul Hasan, Mohd Sayeed [1 ,2 ]
Rai, Abhishek Kumar [1 ]
Ahmad, Zeesam [2 ]
Alfaisal, Faisal M. [3 ]
Khan, Mohammad Amir [4 ]
Alam, Shamshad [3 ]
Sahana, Mehebub [5 ]
机构
[1] Indian Inst Technol Kharagpur, Ctr Oceans Rivers Atmosphere & Land Sci, Kharagpur 721302, West Bengal, India
[2] Aliah Univ, Dept Civil Engn, New Town 700160, West Bengal, India
[3] King Saud Univ, Coll Engn, Dept Civil Engn, Riyadh 11421, Saudi Arabia
[4] Galgotias Coll Engn & Technol, Dept Civil Engn, Greater Noida 201306, Uttar Pradesh, India
[5] Univ Manchester, Sch Environm Educ & Dev, Dept Geog, Oxford Rd, Manchester M13 9PL, Lancs, England
关键词
GLDAS; GIS; Land Surface Model; K Test; Noah; Water Budget; MANN-KENDALL; TRENDS; EVAPOTRANSPIRATION; PRECIPITATION; STRATEGIES; VEGETATION;
D O I
10.1016/j.jksus.2022.102065
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The United Nations Sustainable Development Goal (SDG) ensures adequately accessible water and management for all. Due to the rapid increase in population and industries along the Ganga river, it is necessary to estimate the water budget to fulfill the demand for water in the future. The Mann-Kendall (MK) test conducted on the Noah-Land Surface Model data for 72 years results in a maximum declining trend of water budget in the Yamuna Lower (Q = -3.82 BCM/year), and a minimum in the Damodar sub-basin (Q = -0.10 BCM/year). All the sub-basins show an increase in groundwater level (mbgl) except the Kali Sindh, which shows a decreasing trend (Q = -0.07 m/year). The percentage change was also estimated in all the sub-basins, including various parameters such as precipitation, evapotranspiration, runoff, water budget, and temperature. The extremely severe groundwater drought was estimated using the Standard Groundwater Level Index (SGWLI), from which the values for the Ram Ganga Confluence (SGWLI = 2.44; 2005), Upper stream of Gomti (SGWLI = 2.06; 2014), Ghaghra (SGWLI = 2.22; 2005), Ram Ganga (SGWLI = 2.28; 2005), Yamuna Lower (SGWLI = 2.13; 2007), Kali Sindh (SGWLI = 2.30,2.67; 2002, 2003), Chambal Upper (SGWLI = 2.30,2.20; 2001, 2003), Son (SGWLI = 2.02; 2010), Gandak (SGWLI = 2.37; 2010), Kosi (SGWLI = 2.08; 2012), Damodar (SGWLI = 2.72; 2010), and Bhagirathi (SGWLI = 2.06; 2014) were obtained for a total of 62,050 observed well data.The obtained in-situ point data is converted into the surface raster using a geostatistical technique. Our results show a declining trend in the water budget of all the 19 sub-basins of the Ganga basin and also the groundwater drought in several parts. (c) 2022 The Author(s). Published by Elsevier B.V. on behalf of King Saud University. This is an open access
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页数:19
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