Exploring the channel connectivity structure of the August 2008 avulsion belt of the Kosi River, India: Application to flood risk assessment
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Cites background from "Exploring the channel connectivity ..."
...This breach resulted in amajor avulsion of the Kosi River, which shifted by ~120 km eastward — one of the greatest avulsions in a large river in recent years (Mishra, 2008; Sinha, 2009; Kale, 2011; Sinha et al., 2013)....
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...Sinha et al. (2013) also postulated the avulsive course of the Kosi from one of the potential sites for avulsion identified in this paper (reach 4)....
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...In a recent work, Sinha et al. (2013) analysed the channel connectivity structure of the Kosi (D) Avulsed course 26° 87° 87° false colour composite of Landsat image of 2003 showing the Kosi River basin, (C) detailed 003), (D) detailed view of the study area showing the Kosi River during the…...
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...Our analysis of the connectivity structure for the pre- and postavulsion period (Sinha et al., 2013) has shown that the ‘structural’ connectivity of the paleochannel network on the fan surface provided the pathway for the avulsion channel during the August 2008 event....
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"Exploring the channel connectivity ..." refers methods in this paper
...A normalized difference water index (NDWI) was calculated, as it helps to delineate the surface-water features more accurately (McFeeters, 1996)....
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"Exploring the channel connectivity ..." refers background in this paper
...Class I represents an example of dry paleochannel with full structural connectivity (Wainwright et al., 2011) but with no functional connectivity, whereas class III represents an active channel with full structural and functional connectivity (Bracken and Croke; 2007; Wainwright et al., 2011)....
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