2023
DOI: 10.1007/978-3-031-21086-0_5
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Flood Dynamics, River Erosion, and Vulnerability in the Catchment of Dharla and Dudhkumar Rivers in Bangladesh

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Cited by 2 publications
(2 citation statements)
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“…The characteristics of river channel patterns, categorized as straight, meandering and braided patterns, are largely determined by a number of geomorphological variables including the slope, discharge and bed material size [17][18][19]. Several scholars have classified channel patterns (the bird's eye view of channel configuration) of both the Ganges and Brahamaputra-Jamuna Rivers as braided channels as they are divided into multiple channels by the existence of chars (bars or islands), and these separated channels afterward converge as well as get divided again [9,[20][21]. The primary characteristics of the braided rivers include highly variable discharge, bed-load abundance, easily erodible banks, steep slopes, and mid-channel bars, shoals and islands (charland) [22].…”
Section: River Channel Patterns and Charland Formationmentioning
confidence: 99%
“…The characteristics of river channel patterns, categorized as straight, meandering and braided patterns, are largely determined by a number of geomorphological variables including the slope, discharge and bed material size [17][18][19]. Several scholars have classified channel patterns (the bird's eye view of channel configuration) of both the Ganges and Brahamaputra-Jamuna Rivers as braided channels as they are divided into multiple channels by the existence of chars (bars or islands), and these separated channels afterward converge as well as get divided again [9,[20][21]. The primary characteristics of the braided rivers include highly variable discharge, bed-load abundance, easily erodible banks, steep slopes, and mid-channel bars, shoals and islands (charland) [22].…”
Section: River Channel Patterns and Charland Formationmentioning
confidence: 99%
“…Several scholars have classified both the Ganges and Brahamaputra-Jamuna Rivers as having braided channel patterns (based on a bird's eye view of channel configuration), as the presence of chars divides these rivers into multiple channels, which alternately converge and diverge over the river's length [11,14,24]. The primary characteristics of braided channels include highly variable discharge, bed-load abundance, easily erodible banks, steep slopes, and mid-channel bars, shoals, and islands (charland) [25]. Generally, these islands are seasonally unstable.…”
Section: River Channel Patterns and Charland Formationmentioning
confidence: 99%