
Antarctica Glacier Named for Glasgow Climate Negotiations at COP26
The Antarctic Place Naming Commission has agreed to name glaciers on the Southern Continent after city locations of past and present climate treaties.
The ice sheet that drains into West Antarctica’s Amundsen Sea is about the size of Texas and two miles thick. Home to two of Antarctica’s five biggest glaciers–Pine Island and Thwaites–this region holds enough ice to raise global sea level 1.2 meters. Understanding how the ice changed from the last ice age to today will help us predict future sea level rise. Join Lamont-Doherty marine geologist Frank Nitsche on his voyage aboard the Swedish ice-breaking ship, the Oden.
The Antarctic Place Naming Commission has agreed to name glaciers on the Southern Continent after city locations of past and present climate treaties.
A new study shows, for the first time, evidence of a link between human-caused global warming and melting of the West Antarctic Ice Sheet.
An international collaboration will study the wasting of the Thwaites glacier, which already accounts for around 4 percent of current global sea-level rise, and could collapse within decades or centuries.
If just the West Antarctic Ice Sheet were to melt, it would raise global sea level by 6 meters. That’s more than a theoretical problem. West Antarctica is losing ice mass, and scientists are worried.
After a surprisingly smooth crossing of the Southern Ocean, with favorable winds we arrived back in Hobart, Tasmania. The weather maps show that we just got ahead of another big storm system.
In addition to understanding potential pathways for “warmer” circumpolar deep water to reach the ice shelf, we are also measuring what the structure and properties of the water column are and determining if there is already warmer water on or near the continental shelf that could already interact with the glaciers of East Antarctica today.
One of the goals of this expedition is to investigate if water from the Southern Ocean with temperatures above the melting point of glaciers could reach the glaciers in East Antarctica, and if there are any obstacles on the seafloor of the shelf that impact the ability of such water to reach the glaciers and ice streams.
Several days ago we reached our main work areas along the margin of East Antarctica. Our expedition is relatively late in the season and the seas around Antarctica are starting to freeze.
We are less than a day away from our first study area on the continental shelf in front of the Dibble Glacier. As we approach Antarctica we are starting our science program with a 4500 meter deep CTD and multibeam acquisition.
We are now aboard the R/V Palmer and on our way to East Antarctica. Due to two storms in our direct way we are heading west first to go around the storms and we’ll then head south on their backside.