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Climate Change and Water Resources in South Asia - Chapter 6 ppt

Climate Change and Water Resources in South Asia - Chapter 6 ppt

Climate Change and Water Resources in South Asia - Chapter 6 ppt

... over agreat Indo-Gangetic and Brahmaputra Plain. The water demand for agriculture, industry and urban sector in Nepal, India and Bangladesh is progressively growing and a decline in snow cover ... 1979October 1988(MOS-I)195 6- 5 8(Toposheet): 1 968 1 967 (Gansser, 1970)198 9-9 0(DGM, 1996I)December 1994(Spot 3)December 1993(SPOT XS)a. 195 7-5 9b. 1 96 0 -6 8g. 198 3-8 4h. 198 8-9 0i. 1993j. 1999k. ... 335 and 308 1 1 Budhi Gandaki 60 0 1 - Karnali (Chisapani) 10800 65 - Upper Karnali 300 65 - Pancheshwar 64 80 4 - Tamur/Mewa 100 22 2 Dudh Kosi 300 25 12 Proposed Likhu 4 40 - - 148...
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Climate Change and Water Resources in South Asia - Chapter 1 ppt

Climate Change and Water Resources in South Asia - Chapter 1 ppt

... xxiii1 CLIMATE CHANGE AND WATER RESOURCES IN SOUTH ASIA: ANINTRODUCTIONM. Monirul Qader MirzaQ. K. Ahmad1.1 Introduction 11.2 Water Availability and Demand in South Asia 21.3 Climate Change and ... Gangotri 364 13 (1977 and 1990) 28 Pindari 2,840 120 (184 5-1 966 ) 23 .6 Milam 1,350 107 (184 9-1 957) 12 .6 Poting 262 50 (190 6- 1 957) 5.2 Triloknath 400 26 (1 96 9-1 995) 15.4 Bara Shigri 65 0 18 (197 7-1 995) ... hanges in Soil M oisture C hanges in RunoffC hanges in Ground Water C hanges in Dr oughtC hanges in River FlowC hanges in Floods10 CLIMATE CHANGE AND WATER RESOURCES IN SOUTH ASIA In Nepal...
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Climate Change and Water Resources in South Asia - Chapter 3 ppt

Climate Change and Water Resources in South Asia - Chapter 3 ppt

... 60 1955 865 129 19 56 462 1957 352 1958 389 1959 61 9 1 960 510 1 961 1,374 1 962 348 117 1 963 432 30 1 964 69 0 1 965 79 1 966 180 39 1 967 355 1 968 3,497 221 2 76 1 969 1,408 1970 1,0 76 ... Hardinge Bridge Change (+) Change (+) Change (+) No Change The Kosi Barahkshetra No Change No Change No Change No Change Pandu Change (-) Change (-) Change (-) Change (-) The Bhahmaputra ... Kruskal-Wallis Mann-Whitney U Deviation Ratio a. Peak Discharge Hardwar Change (-) Change (-) Change (-) Change (-) The Ganges Farakka No Change No Change Change (+) No Change Hardinge...
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Climate Change and Water Resources in South Asia - Chapter 2 doc

Climate Change and Water Resources in South Asia - Chapter 2 doc

... sedimenttransport and morphological changes; estimating ground water and changes in ground water volume; forecasting flood volume, depth and duration; assessing changes in land-use; and assessing impacts of changes ... pp.13 5-1 46. Gleick, P.: The Development and Testing of a Water- Balance Model for Climate Impact Assessment:Modeling the Sacramento Basin. Water Resources Research 23 (6) (1987), pp.104 9-1 061 .Gosain, ... branches representing rivers and floodplains. Along the branches h-points and Q-points are located. Flood levels are calculated ath-points and discharge at Q-points. Source: FAP 25, 1994. In order to...
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Climate Change and Water Resources in South Asia - Chapter 4 docx

Climate Change and Water Resources in South Asia - Chapter 4 docx

... pp .6 7-8 4.Downing, T. E. (ed): Climate Change and World Food Security, Springer, Berlin, 19 96, 66 2 pages.Downing, T. E., Ringius, L, Hulme, M. and Waughray, D.: “Adapting to Climate Change in ... “Adapting to Climate Change: A Case Study on Riverine Flood Risks in the Netherlands”. In R. S. J. Tol and A. A. Olsthoorn (eds.), Floods, Flood Management and Climate Change in the Netherlands,Institute ... flooding, it is now certainly appropriate to beginthinking about interventions over the medium- or long-term (like building dikes orinstituting programs of systematic and repeated dredging)...
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Climate Change and Water Resources in South Asia - Chapter 5 pdf

Climate Change and Water Resources in South Asia - Chapter 5 pdf

... 4.03 (-2 5%) 0.81 (-2 0%) 1 .67 (+35%) 2 .61 ( +66 %) GFDL 4.09 (-2 3%) 0.85 (-1 2%) 1 .68 (+ 36% ) 2.48 (+43%) LLNL 4.37 (-1 7%) 0.94 (-2 %) 1 .66 (+34%) 2.13 (+ 36% ) GCM Fo ( 0-3 0 cm) F1 (3 1-9 0 cm) ... Ganges-BrahmaputraLowlands and Delta? Mountain Research and Development 7(3) (1987), pp.25 6- 2 63 .Hofer, T.: Do Land-Use Changes in the Himalayas Affect Downstream Flooding: TraditionalUnderstanding ... BiharPlain; V5 - East Up; V6 West Up; V7 - Haryana; V8 - East Rajasthan; V9 - West MadhayaPradesh; V10 - East Madhaya Pradesh; and V1 1- Nepal** V1 - North Assam; V2 - South Assam; V3 - Sub-Himalayan...
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Climate Change and Water Resources in South Asia - Chapter 7 docx

Climate Change and Water Resources in South Asia - Chapter 7 docx

... of 1 96 1-1 990 over the Indian subcontinent. The projected area-averaged annual M. LAL 165 -1 915 -1 5 -6 -1 6 -1 311 -9 -1 81715 -1 2 -3 123215374483 -6 -1 0 -1 22045 -9 -1 2 -2 124147 -1 125422 -2 5 -1 5 -2 521 -2 8 6 -4 0 -2 002040 60 80100Punjab ... level leadsto intrusion of saline water far into the land mass through the rivers draining into the sea and it also increases ground water contamination by making water saline. Saline water M. LAL ... information on the state-of-the-art thinking about climate change and impacts on water resources. • The timely flows of information among the climate change scientists and the water- management community...
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Climate Change and Water Resources in South Asia - Chapter 9 docx

Climate Change and Water Resources in South Asia - Chapter 9 docx

... public and private water deliverysystems with appropriate legal and financial measures and incentives, includingdelineation of water rights and water pricing;• To bring institutional changes ... sweet water capture fisheries resources are dependent on inland water bodies. The annualflooding and post-flood standing water in the floodplains has a significant role in fishproduction. In the ... increased rainfall and unchanged evapo-transpiration in the monsoon results in increased GW recharge. By contrast, the combination of unchangedrainfall and increased evapo-transpiration in the dry...
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Climate Change and Water Resources in South Asia - Chapter 11 (end) pdf

Climate Change and Water Resources in South Asia - Chapter 11 (end) pdf

... Presented in the Workshop on Democratization in Latin America and South Asia- Creating and Revitalizing Democratic Institutions: Context and Challenge in LatinAmerica and South Asia, 1 8-2 0 April ... non-structural measures include floodforecasting and warning, retention ponds, natural water bodies and drainage network,land-use planning and relief and rehabilitation. Other practiced non-structural ... Tokyo, Japan, 1987.Singh, R.: Practices and Current Status of Flood Forecasting and Management in India, Water Resources Development and Training Center (WRDTC), Indian Institute of Technology,...
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Báo cáo

Báo cáo " Impacts of climate change on water resources in the Huong River basin and adaptation measures " pptx

... 12.7 16. 3 19 .6 22.4 24.7 Year 0.4 0.9 1.2 1.7 2.2 2.7 3.3 4.2 5 .6 7.0 Dec-Feb -0 .9 -1 .8 -2 .4 -3 .6 -4 .6 -5 .7 -6 .9 -8 .9 -1 1.8 -1 4.8 Mar-May 0.4 0.7 1.0 1.4 1.8 2.3 2.8 3 .6 4.7 5.9 ... Dec-Feb -1 .0 -2 .0 -3 .3 -5 .4 -8 .5 -1 2.0 -1 5.4 -1 8.5 -2 1.2 -2 3.4 Mar-May 0.4 0.8 1.3 3.1 3.4 4.8 6. 1 7.4 8.4 9.3 Jun-Aug 0.7 1.1 2.2 3 .6 5 .6 8.0 10.3 12.3 14.2 15 .6 A1FI Sep-Nov ... understanding of the impacts of climate change on water resources in the Huong River basin. Climate change will result in an increase in precipitation in rainy seasons but a decline in dry...
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