Accurate predictions of ice mass loss from Antarctica are crucial for sea-level rise projections. This study investigates the impact of warmer basal temperatures on Antarctic ice sheet mass balance using numerical modeling. Results show that even a small increase in basal warming could lead to increased mass loss and the destabilization of previously frozen areas.
Antarctic ice melt slows Deep Ocean Current with potential Impact on World’s Climate for Centuries
New research by Australian scientists suggests deep Ocean slowdown within […]
Nature Editorial (Nature Climate Change doi:10.1038/nclimate2193): Even if some sceptics consider climate […]
Peter Sinclair: Sherwood’s paper shoots more holes into lingering hopes that […]
