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Titlebook: Climate Change and Island and Coastal Vulnerability; J. Sundaresan,S. Sreekesh,R. Boojh Book 2013 Capital Publishing Company, New Delhi, I

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楼主: Magnanimous
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Paleoclimate of Peninsular India, recourse is taken to natural archives that serve as climate proxies. The prominent proxies that offer annual to seasonal temporal resolution include annual rings of trees (Ramesh et al., 1985; Ramesh et al., 1986a; Ramesh et al., 1986b; Ramesh et al., 1988; Ramesh et al., 1989; Managave et al., 20
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Inventory and Monitoring of Coral Reefs of United Arab Emirates (UAE), Arabian Gulf, Using Remote Seya, 1976; Johannes, 1975). Coral reefs are indicators of environmental and climate changes that cause flashing damage to reefs. As an integral part of reefs, corals are especially vulnerable to anthropogenic pressures and climate change related threats.
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Impact of Climate Change in the Sundarban Aquatic Ecosystems: Phytoplankton as Proxies influencing the partitioning of climate-relevant gases between the ocean and atmosphere (Schlesinger, 2005). In modern day, phytoplankton can be used as excellent proxies for detecting changes in the water column as a result of anthropogenic activities (Moncheva et al., 2001).
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Influence of Suspended Solid on in situ and ex situ Chlorophyll-,: A Case Study of Indian Sundarbans Mitra et al., 1994). In the Indian Sundarbans, approximately 2069 sq. km of area is occupied by the tidal river system or estuaries, which finally end up in the Bay of Bengal. The seven main riverine estuaries from west to east (that contribute considerable sediment load in the aquatic sub-system)
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Role of Sea Level Rise on the Groundwater Quality in Coastal Areas of Sri Lankad water is the largest source of fresh water available on earth, which is exploited to satisfy domestic, agriculture and industrial purposes. Ground water plays a significant role in the overall circulation of water through the hydrologic cycle. It is always considered as a readily available and saf
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Mangrove Responses to Climate Change along the Southwestern Coast of India during Holocene: Evidenceof the world. Indian mangrove vegetation covers about 6749 km. along the 7516 km long coast line, including Island territories (Mandal and Naskar, 2008). The distribution of mangrove areas along the Indian coast is influenced by physical forces such as geomorphology, climate, tidal amplitude and dur
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