2011
DOI: 10.1504/ijw.2011.043318
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Water salinity investigation in the Sundarbans rivers in Bangladesh

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Cited by 39 publications
(28 citation statements)
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“…This diversion decreased the average dry season flow in the Ganges from 3114 m 3 sec −1 during the pre-Farakka period to 2010 m 3 sec −1 during the post-Farakka period 9 10 . This diversion of freshwater from the Ganges at Farakka also reduced the dry-season discharge in the Gorai River, the major distributary of the Ganges and the main freshwater source of the PRE upstream, from a pre-Farakka mean flow of 190 m 3 sec −1 in 1973 9 10 to post-Farakka mean flows of 51 m 3 sec −1 in 1977 and 10 m 3 sec −1 in 2008 11 . Consequently, freshwater flow has declined in the SRE by almost 60% since 1977 8 because the SRE is connected by lateral channels to the PRE.…”
mentioning
confidence: 95%
“…This diversion decreased the average dry season flow in the Ganges from 3114 m 3 sec −1 during the pre-Farakka period to 2010 m 3 sec −1 during the post-Farakka period 9 10 . This diversion of freshwater from the Ganges at Farakka also reduced the dry-season discharge in the Gorai River, the major distributary of the Ganges and the main freshwater source of the PRE upstream, from a pre-Farakka mean flow of 190 m 3 sec −1 in 1973 9 10 to post-Farakka mean flows of 51 m 3 sec −1 in 1977 and 10 m 3 sec −1 in 2008 11 . Consequently, freshwater flow has declined in the SRE by almost 60% since 1977 8 because the SRE is connected by lateral channels to the PRE.…”
mentioning
confidence: 95%
“…Hot and humid pre-monsoon season starts from March to May followed by monsoon period from June to September and then October and November post-monsoon months and finally December to February being dry winter period. The Sundarbans is a low-lying floodplain with elevation that varies from 0.9 to 2.11 m above sea level (Spalding 2010;Ghosh et al 2015) and land slope is 0.03 m vertically per km of horizontal distance moving from north to south (Islam and Gnauck 2011). An average relative sealevel rise (RSLR) of 1.07 mm/year from early to mid-Holocene period has been estimated for this region (Islam and Tooley 1999).…”
Section: Study Site and Focusmentioning
confidence: 99%
“…The Sundarbans has experienced notable declines in biodiversity and habitat for tigers and other wildlife as a result of: conversion of forest to other uses (historically paddy fields and more recently shrimp farms); unsustainable exploitation of timber resources and fauna (particularly shrimp fry collection to supply shrimp farms); alterations of the hydrological regime through polder construction and interventions that cut freshwater flows (e.g., the Farakka Barrage in India); and changes in the salinity regime, with saline waters moving further inland (Iftekhar, 2006;Giri, Pengra, Zhu, Singh and Tieszen, 2007;Islam andGnauck, 2011a and2011b). Discharges of domestic and industrial wastewater into surface waters have also been damaging (Ahmad et al, 2010).…”
Section: Biodiversitymentioning
confidence: 99%
“…Salinity is a key factor affecting the mangrove ecosystem, and the Sundarbans has already experienced significant replacement of dominant mangrove species with species that can better tolerate saline conditions (Islam, 2008;Islam and Gnauck, 2011a).…”
Section: Biodiversitymentioning
confidence: 99%