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South facing visualization of the Antarctic ice sheet from the Pacific sector of the Southern Ocean (West Antarctic ice sheet, foreground; Antarctic P
South facing visualization of the Antarctic ice sheet from the Pacific sector of the Southern Ocean (West Antarctic ice sheet, foreground; Antarctic Peninsula, to the left; East Antarctic ice sheet, background).
Antarctic Skin Temperature Trends between 1981 and 2007, based on thermal infrared observations made by a series of NOAA satellite sensors. Skin tempe
Antarctic Skin Temperature Trends between 1981 and 2007, based on thermal infrared observations made by a series of NOAA satellite sensors. Skin temperature trends do not necessarily reflect air temperature trends.
Parts of East Antarctica (marked in blue) are currently the only place on Earth to regularly experience negative greenhouse effect during certain mont
Parts of East Antarctica (marked in blue) are currently the only place on Earth to regularly experience negative greenhouse effect during certain months of the year. At greater warming levels, this effect is likely to disappear due to increasing concentrations of water vapor over Antarctica
Antarctic surface temperature trends, in °C/decade. Red represents areas where temperatures have increased the most since the 1950s.
Antarctic surface temperature trends, in °C/decade. Red represents areas where temperatures have increased the most since the 1950s.
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One of Earth's two ice sheets: The Antarctic ice sheet covers about 98% of the Antarctic continent and is the largest single mass of ice on Earth. It
One of Earth's two ice sheets: The Antarctic ice sheet covers about 98% of the Antarctic continent and is the largest single mass of ice on Earth. It has an average thickness of over 2 kilometers.
Glacial flow rate in the Antarctic ice sheet.
Glacial flow rate in the Antarctic ice sheet.
The collapse of the Larsen B ice shelf had profound effects on the velocities of its feeder glaciers.
The collapse of the Larsen B ice shelf had profound effects on the velocities of its feeder glaciers.
Accelerated ice flows after the break-up of an ice shelf
Accelerated ice flows after the break-up of an ice shelf