Latest Antarctic ice sheet Stories
A new dataset called Bedmap2 gives a clearer picture of Antarctica from the ice surface down to the bedrock below.
Alaska’s melting glaciers remain one of the largest contributors to the world’s rising sea levels.
Researchers have found that ancient geodynamics elevated segments of ancient shorelines over millions of years. This made the shorelines appear higher now than they originally were millions of years ago.
A new 1000-year Antarctic Peninsula climate reconstruction shows that summer ice melting has intensified almost ten-fold, and mostly since the mid 20th Century.
According to a new study, the dramatic glacial melt in Western Antarctica is due to natural variation and cannot be attributed directly to carbon emissions.
A growing number of studies have pegged global warming and climate change as a cause of sea ice decline in recent decades. However, a newly published study in the journal Nature Geoscience is showing a vastly different scenario.
Antarctica's topography began changing from flat to fjord-filled starting about 34 million years ago, according to a new report from a University of Arizona-led team of geoscientists.
A new study has traced glacial ice entering the ocean along the western Antarctic Peninsula using a unique 12,000-year record of microscopic marine algae fossils.
The uncertainty of future sea level rise is getting a little clearer thanks to research being conducted by a team of scientists.
Antarctica is the Earths southernmost continent; it contains the geographic South Pole. It’s situated in the Antarctic area of the Southern Hemisphere, almost completely south of the Antarctic Circle, and is bordered by the Southern Ocean. It’s the fifth-largest continent at 5.4 million sq miles. On average, it is the driest, coldest, and windiest continent as well as having the highest average elevation of all the continents. Considered a desert, the annual precipitation is only 8...
- Forsooth! indeed! originally a parenthetical phrase used in repeating the words of another with more or less contempt or disdain.