HIMALDOC 9 records found  Search took 0.01 seconds. 
Year: 2014
Summary Assessing local climate change impacts requires downscaling from Global Climate Model simulations
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Year: 2013
River flow is a reflection of the input of moisture and its transformation in storage and transmission over the catchment
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Year: 2012
The Upper Indus Basin (UIB) covers an area of more than 200,000 km2 and has an elevation range from below 1000 to over 8000 m above sea level
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Year: 2012
The Upper Indus Basin (UIB) covers an area of more than 200,000 km2 and has an elevation range from below 1000 to over 8000 m above sea level
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Year: 2010
Pakistan is highly dependent on water resources originating in the mountain sources of the upper Indus for irrigated agriculture which is the mainstay of its economy
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Year: 2006
Temperature data for seven instrumental records in the Karakoram and Hindu Kush Mountains of the Upper Indus Basin (UIB) have been analyzed for seasonal and annual trends over the period 1961–2000 and compared with neighboring mountain regions and the Indian subcontinent
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Year: 2005
The mountainous region of the Upper Indus Basin is a critical source of water for Pakistan
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Year: 2003
Since much of the flow abstracted from the River Indus for irrigation originates in the Himalayas, Karakoram and Hindu Kush Mountains, an understanding of hydrological regimes of mountain rivers is essential for water resources management in Pakistan
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Year: 1999
Most of the flow in the River Indus from its upper mountain basin is derived from melting snow and glaciers
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HIMALDOC 9 records found  Search took 0.01 seconds. 
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8 Archer, D. R.
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