Ramiro Saurral

The transition zone between land and sea in glaciers is an indicator of their stability. An analysis of satellite measurements from 1992 to 2025 has shown that 77% of Antarctica’s coastline has experienced no change. The 23% that did see a reduction in area was concentrated in regions where deep troughs allow access to warmer waters and where the bed slopes inland. These include the Antarctic Peninsula, Wilkes and George V Lands, and West Antarctica, where retreat of this transition line ranged between 10 and 40 km. A total of 12,800 km² of ice has been lost —an area roughly equivalent to almost half the size of Galicia— most of it in West Antarctica. The results are published in the journal PNAS.

A study led by ISGlobal researchers has analysed how the loss of Arctic sea ice influences climate in isolation from other factors related to climate change. Their results, published in the journal Communications Earth and Environment, show that, on a time scale of decades, the loss of Arctic sea ice favours a drier climate in the southwestern United States -in particular in California-, especially in winter. This phenomenon would also affect the climate of Spain and Portugal, leading to wetter conditions in winter, although the effect is weaker.