A new paper published by Frontiers, led by Assistant Professor (Research) Christopher Horvat, challenges our current understanding of the Antarctic ecology and the lifecycles of growth that happen under the ice. 

"We're going to see almost a foot – somewhere between nine and 11 inches – of sea level rise by 2050 – a generation and a half, we see that amount," Fox-Kemper explained while standing at the waters’ edge. "And the 2050 numbers are already baked in. So even if we were to cut all of our emissions today, we still are going to see sea level rise."

Sharp fronts and eddies that are ubiquitous in the world ocean, as well as features such as shelf seas and under-ice-shelf cavities, are not captured in climate projections. Such small-scale processes can play a key role in how the large-scale ocean and cryosphere evolve under climate change, posing a challenge to climate models.

A new global analysis of the last 19 million years of seafloor spreading rates found they have been slowing down. Geologists want to know why the seafloor is getting sluggish.

Composition of air bubbles can help scientists date Antarctica’s ice caps

A unified model for transient subglacial water pressure and basal sliding

A new study led by Prof. Steve Clemens proves that monsoons will become more destructive