Study Ties One-Fifth of Pine Island Glacier Retreat to Climate Change
About 4km of the Pine Island glacier's retreat, or roughly a fifth of the total, traces to climate change, according to a study in the Cryosphere reported by Carbon Brief. The authors describe it as the first attribution study of glacier retreat on Antarctica.
The Pine Island and Thwaites glaciers together account for almost half the sea level rise driven by Antarctic ice-sheet melt, according to Carbon Brief. Pine Island alone has contributed a fifth of net ice loss from the West Antarctic ice sheet, and that ice sheet drives almost all of Antarctica's ice loss over the past 40 years.
Sediment records place the start of the glacier's retreat in the 1940s, according to Carbon Brief. The timing lines up with a strong El Nino, a recurring tropical Pacific pattern that pushed a large pulse of warm water toward the ice sheet.
Climate reconstructions point to the 1960s as the moment human-caused warming began lifting the volume of warm water reaching the West Antarctic ice sheet, according to Carbon Brief. That puts the human fingerprint about 20 years behind the retreat that was already underway.
Deeper in the record, the West Antarctic ice sheet has pulled back roughly 500km since the last glacial maximum around 20,000 years ago, with most of that retreat falling between 10,000 and 20,000 years ago, according to Carbon Brief.
Source: carbonbrief.org (opens in a new tab)1 sourcePermalink