The more ice is melted of the Antarctic Filchner-Ronne shelf, the more ice flows into the ocean, and the more the region contributes to global sea-level rise. Unlike some some other parts of Antarctica, this region is not characterized by instabilities which, once triggered, can lead to persistent ice discharge into the ocean even without a further increase of warming. So for the Filchner-Ronne ice, this is a tiny bit of good news....