Riverine landscape dynamics of the Upper Ganga River (Haridwar-Narora), India

被引:7
|
作者
Prasad, Satish [1 ]
Saluja, Ridhi [1 ,2 ]
Joshi, Varun [1 ]
Garg, J. K. [1 ,3 ]
机构
[1] Guru Gobind Singh Indraprastha Univ, Univ Sch Environm Management, Delhi, India
[2] Wetlands Int South Asia, A-25 Def Colony, New Delhi, India
[3] Teri Sch Adv Studies, Vasant Kunj Inst Area, New Delhi, India
关键词
Sinuosity; Braiding; Erosion-deposition; LULC; FRAGSTATS; River dynamics; BANK EROSION; LAND-USE; UTTAR-PRADESH; WEST-BENGAL; GIS; BASIN; ACCRETION; PLANFORM; SYSTEMS; RISK;
D O I
10.1007/s10661-021-08868-8
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Earth observation data provides an exceptional opportunity to study the temporal dynamics of large rivers. The availability of spatially continuous, synoptic and temporally repetitive satellite data allows the reconstruction of historical dynamics of large rivers along with the identification of the causal factors. An absolute paucity of information on the effect of hydrogeomorphic processes on the dynamics of the Upper Ganga River (UGR), especially upon its entry in the plains, motivated this research. This study aims to analyse morphological changes in the river channel, map temporal changes in the land use/land cover (LULC) within the riverscape and thereby understand the landscape dynamics in the UGR (Haridwar to Narora) during 1993-2017 by means of earth observation data. The analysis showed that the river remains straight with a sinuosity index of <1; however, the braiding increased considerably (from 3.79 to 4.53). Erosion being more prominent on the left bank in comparison to the right bank with 85.89 km(2) eroded on the left bank in comparison to 59.21 km(2) eroded along the right bank. Riverine landscape has been observed to have a higher rate of accretion in comparison to erosion (8.09 km(2) yr(-1) and 6.04 km(2) yr(-1), respectively). Morphological change has brought a transition in the land use patterns with marked variation in vegetation and agriculture along with built-up. Significant changes in the composition of the LULC are largely due to the manifold increase in the agriculture extent (approximate to 12 times), built-up (5 times) and the decrease in vegetation cover from 43.9% in 1993 to just 10.94% in 2017.
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页数:20
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