UN World Water Development Report 2025
<p>For billions of people, mountain meltwater is essential for drinking water and sanitation, food and energy security, and the integrity of the environment. But today, as the world warms, glaciers are
<p>For billions of people, mountain meltwater is essential for drinking water and sanitation, food and energy security, and the integrity of the environment. But today, as the world warms, glaciers are
This volume constitutes the proceedings of the 12th Biennial Conference of the Euromediterranean Network of Representative and Experimental Basins (ERB) held in Krakow, Poland, from 18-20 September 2008.
Buenos Aires (Argentina): Argentina
The nature of initial glaciation on Antarctica about 34 million years ago is a mystery.
New York, Boston and other cities on North America's northeast coast could face a rise in sea level this century that would exceed forecasts for the rest of the planet if Greenland's ice sheet keeps melting as fast as it is now, researchers said on Wednesday.
A Nepali sherpa who holds the world record for climbing Mount Everest said on Monday rising temperatures were melting snow and turning the slopes barren, making it even harder to scale the world's tallest peak.
Experts Worry Melting Permafrost May Release More Gas Oslo: A rise in concentrations of a powerful greenhouse gas over the Arctic after a decade of stability is stirring worries about a possible thaw of vast stores trapped in permafrost, experts said.
NEW DELHI: The European Union has launched project
GLACIAL meltdown, global warming, devastating floods, soil erosion, rise in the sea level, salinity, waterlogging, famine, and heavy rainfall are the direct catastrophic consequences of deforestation. It is estimated that Himalayan glaciers are receding by 30 to 50 metres a year and in another 50 years they could be gone altogether.
Theory has suggested that the West Antarctic Ice Sheet may be inherently unstable. Recent observations lend weight to this hypothesis. This article reassess the potential contribution to eustatic and regional sea level from a rapid collapse of the ice sheet and find that previous assessments have substantially overestimated its likely primary contribution.
Volume changes in the Antarctic Ice Sheet are poorly understood, despite the importance of the ice sheet to sea-level and climate variability. Over both millennial and shorter time scales, net water influx to the ice sheet (mainly snow accumulation) nearly balances water loss through ice calving and basal ice shelf melting at the ice sheet margins.