Antarctica Climate Surprises May Be Ahead, Says Study
For Antarctica in the 21st century, two disctict climate scenarios appear plausible, according to Paul Mayewski, director of the Climate Change Institute at the University of Maine. Examination of climate models, plus records of climate change developed through ice cores, reveal the possibility of future climate surprises in the Southern Hemisphere, he says.
“In a nutshell, the review describes how the examination of past analogs compared to model projections differ, and the implications,” he says.
Mayewski and fellow researchers with Antarctic Climate in the 21st century (AntClim21), a Scientific Research Programme of the Scientific Committee on Antarctic Research (SCAR), discovered potentially different forecasts as part of a published review they developed for the scientific community.
Climate models suggest that continued strengthening and poleward contraction of the Southern Ocean westerly wind belt will affect Antarctica’s 21st century environment, Mayewski says.
Ice core records suggest continued southward displacement of the westerlies, but weakened westerlies that allow greater entry of warm marine air masses into Antarctica.
Abrupt Collapses of Glaciers
Mayewski says implications for the ice core-derived past analog scenario are serious; wind-driven infiltration of warmed water into the coastal zone could result in abrupt collapses of glaciers in these regions and accelerated global sea-level increase.
Changes in the westerly jet structure could cause other surprises on a regional scale that could significantly affect weather extremes, ocean circulation, carbon uptake, sea ice extent and sea-level rise.
Evidence from Earth’s climate history supports the possibility of such a surprise in the rate of ice-sheet response and climate change in the Southern Hemisphere, he says.
For example, around 14,500 years ago, global sea level rose by 20 meters, at a rate of 4 meters per 100 years. Marine sediment reconstructions and modeling studies indicate the rise was partially due to a rapidly collapsing West Antarctic ice sheet.