2013
DOI: 10.1080/01431161.2013.803629
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An integrated approach to map certain palaeochannels of South India using remote sensing, geophysics, and sedimentological techniques

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Cited by 18 publications
(4 citation statements)
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“…FCC (false colour composite) (Figure 2 a) and true colour imagery of Landsat ETM+ have been generated by taking band combinations of 4, 3 and 2 as well as 3, 2 and 1 respectively. Histogram equalization technique has also been applied on Aster Terra Look and ETM + Pan mosaic data (Figure 2 b) to increase the colour contrast between the palaeo-channel trace and the surrounding region 6 . As the suspected palaeochannel is characterized by thick vegetation, the vegetation enhancement technique normalized difference vegetation index (NDVI) has been applied using ratio of Near Infrared (NIR) Band -Red Band/Near Infrared Band + Red Band to distinguish the vegetation band along the trace of the channel from that in the surrounding region.…”
mentioning
confidence: 99%
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“…FCC (false colour composite) (Figure 2 a) and true colour imagery of Landsat ETM+ have been generated by taking band combinations of 4, 3 and 2 as well as 3, 2 and 1 respectively. Histogram equalization technique has also been applied on Aster Terra Look and ETM + Pan mosaic data (Figure 2 b) to increase the colour contrast between the palaeo-channel trace and the surrounding region 6 . As the suspected palaeochannel is characterized by thick vegetation, the vegetation enhancement technique normalized difference vegetation index (NDVI) has been applied using ratio of Near Infrared (NIR) Band -Red Band/Near Infrared Band + Red Band to distinguish the vegetation band along the trace of the channel from that in the surrounding region.…”
mentioning
confidence: 99%
“…As the suspected palaeochannel is characterized by thick vegetation, the vegetation enhancement technique normalized difference vegetation index (NDVI) has been applied using ratio of Near Infrared (NIR) Band -Red Band/Near Infrared Band + Red Band to distinguish the vegetation band along the trace of the channel from that in the surrounding region. To get the topographic outline of the channel, spatial profiling technique has been applied to Shuttle Radar Topographic Mission (SRTM) data, using methods similar to that of Nandini et al 6 . Spatial profiling refers to the plotting of topographic elevation against distance to obtain the topographic outline (Figure 3 a).…”
mentioning
confidence: 99%
“…An insight into past floodplain activities, paleoclimatic conditions, and estuarine and alluvial depositional responses to prior to sea-level changes can be gained by palaeochannel studies (Kemp & Spooner, 2007;Nandini, Sanjeevi, & Bhaskar, 2013;Ryan, Bostock, Brooke, & Marshall, 2007). Evidence of the past discharge rates and flow regimes as a huge bulk of sedimentary loads is conserved within them (Sylvia & Galloway, 2006).…”
Section: Significance Of Palaeochannelsmentioning
confidence: 99%
“…Aligned depressions along a channel trace may thus help to identify a remnant river valley, which can be detected in spatial profile, i.e. plot of elevation against distance 3,23 across the suspected channel. In the present study, spatial profiles have been drawn across the three transects T1-T3 (suspected to be palaeo-channels) on SRTM data with spatial resolution of 30 m (Figure 6 b).…”
Section: Image Manipulation Techniquesmentioning
confidence: 99%