
"Thwaites Glacier Faces Accelerated Melting from Warm Water Intrusion"
The Thwaites Glacier is experiencing accelerated melting as warm water reaches miles inland past its grounding line, contributing to significant ice loss.
All articles tagged with #grounding line

The Thwaites Glacier is experiencing accelerated melting as warm water reaches miles inland past its grounding line, contributing to significant ice loss.

Two new studies shed light on the mysterious realm beneath Antarctica's ice shelves. Using underwater robotics and ground-penetrating radar, scientists have discovered that the melting of the ice shelves is driven by warm ocean water eating away at their undersides. The melting and freezing of seawater within deep crevasses create currents that accelerate the melting process. Additionally, researchers have found that geothermal heat and friction from ice grinding against the ground create rivers of freshwater flowing from the interior of the ice sheets, enhancing melting at the grounding line. These findings highlight the urgent need to reduce carbon emissions to prevent further collapse of Antarctica's glaciers and mitigate the potential rise in sea levels.

A new study has found that the Thwaites Glacier in Antarctica retreated hundreds of meters per day during the pre-satellite era, according to data collected from delicate seafloor landforms. The findings add to a growing body of research on the rapid retreat of Antarctic ice sheets, which has significant implications for global sea level rise. The study highlights the importance of understanding grounding line dynamics and seafloor landforms in predicting future ice-sheet behavior.