Fluffy specks of carbon-rich dust found in Antarctica could help explain how the carbon needed for life wound up on Earth.

If some of the spectacular calving of ice shelves in Antarctica is down to global warming, then why did we not see break-ups on the same scale in Greenland, which is much warmer?

This paper explore three key issues that relate to the management of Antarctica in the context of climate change: climate change mitigation; climate change adaptation, in terms of the management strategies that could limit the vulnerability of Antarctica

A new research by US Geological Survey (USGS) has deter- mined that ice shelves are retreating in the southern section of the Antarctic Peninsula due to climate change, which could result in glacier retreat and sea- level rise if warming continues.

Associate Laureate Laureate Cristian Donoso kayaked along Antarctica's rugged coast, documenting the fate of wildlife endangered by global climate change. Now he has returned there with two companions to kayak to a remote section of the Antarctic Peninsula, then turn the kayaks into sleds and scale the Antarctic Andes, exploring the effect of climate change on high glaciers.

Ice and firn core studies provide one of the most valuable tools for understanding the past climate change. In order to evaluate the temporal isotopic variability recorded in ice and its relevance to environmental changes, stable isotopes of oxygen and hydrogen were studied in a firn core from coastal Dronning Maud Land, East Antarctica.

Ice and firn core studies provide one of the most valuable tools for understanding the past climate change. In order to evaluate the temporal isotopic variability recorded in ice and its relevance to environmental changes, stable isotopes of oxygen and hydrogen were studied in a firn core from coastal Dronning Maud Land, East Antarctica.

We

The Hole Helps In Formation Of Special Moist Clouds That Shield The Antarctic Region From Warming Effects
Sindya N Bhanoo

That the hole in Earth

The Southern Ocean is potentially a substantial sink of anthropogenic carbon dioxide; however, the regulation of this carbon sink by the wind-driven Ekman flow, mesoscale eddies and their interaction is under debate.

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