Abstract. The glacier mass balance is driven by primary processes such as snowfall and surface melt. Secondary processes, like firn pack warming, percolation, and refreezing, are becoming more important even in high-elevation basins, which are triggered by warming Alpine regions. All these processes are functionally re...
Akash M. Patil, Christoph Mayer, T. Jenk et al.· The Cryosphere· 0 citations
Understanding the coastal zone of the Antarctic Ice Sheet (AIS), where it interacts with the Southern Ocean and warmer air masses, is crucial for predicting Antarctica's influence on the global climate and sea level. This region has multiple tipping mechanisms that could trigger large, rapid, and potentially irreversib...
Kenichi Matsuoka, G. Moholdt, Jennifer F. Arthur et al.· Reviews of Geophysics· 2 citations
We use cookies to run the site and, with your consent, for analytics and to show ads.
See our Cookie Policy.