A new ice core study from the West Antarctic Ice Sheet (WAIS) concludes that current dramatic and unusual warming changes on the West Antarctic Ice Sheet may still be in the bounds of natural decadal variability.
In other words, the warming trend signal is still not strong enough to distinguish it above the noise of peak warming periods in multi-decade long cycles involving the Tropical Pacific atmospheric circulation, sea surface temperatures and the El NiƱo (ENSO) cycle.
While acknowledging the rapid warming over the West Antarctic Ice Sheet the authors conclude that "It is unknown whether these changes are part of a longer-term trend."
Related: Global warming in Antarctica: Thwaites and Pine Island Glaciers | Waking the giant: Global Warming in the Weddell Sea | Southern Ocean warming impact on Antarctic Ice Sheet and global sea level | Antarctic Paradox: ocean warming melting ice shelves causing sea ice expansion







