2006
DOI: 10.1016/j.margeo.2005.12.003
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Anomalous inland influx of the River Indus, Gulf of Kachchh, India

Abstract: The Gulf of Kachchh is a funnel shaped, macrotidal water body located in the arid region of northwestern India with ~ 50 cm annual rainfall and insignificant fluvial input. The Gulf waters, however, have high-suspended matter. Time series measurements of total suspended matter (TSM) and synchronous, validated hydrodynamic modeling have been used to decipher the dispersal pathways and the sources of the high turbidity. Contrary to the prevalent offshore reducing trend for most of the Indian Coast, the Gulf is a… Show more

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Cited by 28 publications
(16 citation statements)
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“…The existing data indicate that the Indus River is the only major source of sediments to the GoK, delivering about 59 × 10 6 tons of sediments annually into the ocean (Milliman et al 1982). Similar inference is drawn by several workers using suspended sediment concentration (SSC) and satellite imageries (Kunte et al 2003;Chauhan et al 2006;Ramaswamy et al 2007). However, at the present time there are no data pertaining to the contribution made by the southerly draining rivers of the Kachchh and the rivers from the Saurashtra peninsula.…”
Section: Introductionsupporting
confidence: 83%
See 1 more Smart Citation
“…The existing data indicate that the Indus River is the only major source of sediments to the GoK, delivering about 59 × 10 6 tons of sediments annually into the ocean (Milliman et al 1982). Similar inference is drawn by several workers using suspended sediment concentration (SSC) and satellite imageries (Kunte et al 2003;Chauhan et al 2006;Ramaswamy et al 2007). However, at the present time there are no data pertaining to the contribution made by the southerly draining rivers of the Kachchh and the rivers from the Saurashtra peninsula.…”
Section: Introductionsupporting
confidence: 83%
“…So far the GoK has attracted many workers to study its offshore dynamics in this complex macrotidal regime. There have been several studies of the region which essentially addressed its current dynamics (Shetye 1999), suspended sediment transport (Nair et al 1982;Chauhan 1994;Kunte et al 2003;Chauhan et al 2004Chauhan et al , 2006Ramaswamy et al 2007), sediment character of sea floor (Hashimi et al 1978) and various sedimentation processes (Vora et al 1987;Babu et al 2005;Vethamony et al 2005Vethamony et al , 2007. However, comparatively the understanding of sedimentation along the coastline has remained 'Terra incognita', owing to the lack of work published on its geomorphology and textural attributes (Kar 1993;Maurya et al 2008;Prizomwala et al 2010;Shukla et al 2010).…”
Section: Introductionmentioning
confidence: 99%
“…The term (m 0 /H)N S represents additional nutrient in the system through vertical diffusion from sediments at the depth H. The N S is the sediment nutrient concentration and m 0 refers to vertical mixing rate. As mentioned in Section 2.1.1, sediments in the Gulf of Kachchh are suspended matter and clay particles with high concentration between 21 and 69 mg/l (Chauhan et al, 2006).…”
Section: Nutrient (N)mentioning
confidence: 96%
“…The sediments in the Gulf of Kachchh are suspended matter and clay particles with high concentration between 21 mg/l and 69 mg/l (ref. 18). …”
Section: Description Of the Terms Of The Ecological Modelmentioning
confidence: 99%