2012
DOI: 10.1080/10106049.2011.620180
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Understanding dynamics of large rivers aided by satellite remote sensing: a case study from Lower Ganga plains, India

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Cited by 76 publications
(23 citation statements)
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“…River discharge and the sediments are independent variables for stable meandering channels like the Chenab River which have less erosive energy due to which they do not migrate considerably within a small span of time. Therefore a major contribution in morphology and behaviour of a river reach can be caused due to water and sediment discharges from upstream (Yeasmin & Islam, 2011;Sinha & Ghosh, 2012). In-channel structures like check dams increase the potential of downstream erosion (Boix-Fayos et al, 2008).…”
Section: Siltation and Change In River Coursementioning
confidence: 99%
“…River discharge and the sediments are independent variables for stable meandering channels like the Chenab River which have less erosive energy due to which they do not migrate considerably within a small span of time. Therefore a major contribution in morphology and behaviour of a river reach can be caused due to water and sediment discharges from upstream (Yeasmin & Islam, 2011;Sinha & Ghosh, 2012). In-channel structures like check dams increase the potential of downstream erosion (Boix-Fayos et al, 2008).…”
Section: Siltation and Change In River Coursementioning
confidence: 99%
“…The study reach surface morphology is composed of quarternary fluvial processes, underlying uneven geologic basement, long term climatic transformation and superimposition. The present conditions of the south bengal river system are characterised by large amount of water release from the Farakka barrage to the Padma, gradual reduction in the stream power of Ganga's ditributaries (i.e., Bhairab, Jalangi, Mathabhanga and Bhagirathi) (Basu and Sen, 1997;Sinha and Ghosh 2012), southward hanging of the Damodar's distributaries and palaeo existence of its eastward original path etc. (Basu 1964;Rudra 2014).…”
Section: Regional Settingsmentioning
confidence: 99%
“…The channel bank movement largely depends on bank composition and stream power which help to identify whether a channel is avulsed or not (Anderson et al 1996;Keen-Zebert et al 2013). Along with the mentioned factors, coexisting stratigraphic sequences to the channel are very useful evidence to analyse avulsive nature of the channel and new floodplain construction mechanism (Sinha 1996;Sinha and Ghosh 2012). Apart from this, there are many leaving landforms and exhumed features which develop during the transformation of a channel portion to a new floodplain or vice versa.…”
Section: Introductionmentioning
confidence: 99%
“…Several reaches around Narora, Kanpur (both in Class IV), and Farakka (Class X) barrages along the Ganga river have seen significant modifications in terms of channel morphology both upstream and downstream of the barrage (Rudra, ; Sinha & Ghosh, ). The engineering assumption that jacketing the river would increase the velocity leading to scouring has instead resulted in silting of river beds and increased water logging and soil salinity in the adjoining floodplains.…”
Section: Discussionmentioning
confidence: 99%