A new paper published in Nature finds that a majority of the outlet glaciers along the East Antarctic ice sheet have advanced in size over the past 20 years from 1990 to 2010.
According to the paper, “Despite large fluctuations between glaciers—linked to their size—three [significant] patterns emerged: 63 per cent of glaciers retreated from 1974 to 1990, 72 per cent advanced from 1990 to 2000, and 58 per cent advanced from 2000 to 2010.” According to the authors, “In the 1970s and 80s, temperatures were rising and most glaciers retreated. During the 1990s, temperatures decreased and most glaciers advanced. And the 2000s saw temperatures increase and then decrease, leading to a more even mix of retreat and advance.” “When it was warm and the sea-ice decreased, most glaciers retreated, but when it was cooler and the sea ice increased, the glaciers advanced.” [Note: Antarctic sea ice is currently near record-high levels]
Excerpt from the paper:
Here we present multidecadal trends in the terminus position of 175 ocean-terminating outlet glaciers along 5,400 kilometres of the margin of the East Antarctic ice sheet, and reveal widespread and synchronous changes. Despite large fluctuations between glaciers—linked to their size—three epochal patterns emerged: 63 per cent of glaciers retreated from 1974 to 1990, 72 per cent advanced from 1990 to 2000, and 58 per cent advanced from 2000 to 2010.
Aug. 28, 2013 — The world’s largest ice sheet could be more vulnerable to the effects of climate change than previously thought, according to new research from Durham University.
A team from the Department of Geography used declassified spy satellite imagery to create the first long-term record of changes in the terminus of outlet glaciers — where they meet the sea — along 5,400km of the East Antarctic Ice Sheet’s coastline. The imagery covered almost half a century from 1963 to 2012.
Using measurements from 175 glaciers, the researchers were able to show that the glaciers underwent rapid and synchronised periods of advance and retreat which coincided with cooling and warming.
The researchers said this suggested that large parts of the ice sheet, which reaches thicknesses of more than 4km, could be more susceptible to changes in air temperatures and sea-ice than was originally believed.
Current scientific opinion suggests that glaciers in East Antarctica are at less risk from climate change than areas such as Greenland or West Antarctica due to its extremely cold temperatures which can fall below minus 30°C at the coast, and much colder further inland.
But the Durham team said there was now an urgent need to understand the vulnerability of the East Antarctic Ice Sheet, which holds the vast majority of the world’s ice and enough to raise global sea levels by over 50m.
Dr Chris Stokes, in Durham’s Department of Geography, said: “We know that these large glaciers undergo cycles of advance and retreat that are triggered by large icebergs breaking off at the terminus, but this can happen independently from climate change.
“It was a big surprise therefore to see rapid and synchronous changes in advance and retreat, but it made perfect sense when we looked at the climate and sea-ice data.
“When it was warm and the sea-ice decreased, most glaciers retreated, but when it was cooler and the sea ice increased, the glaciers advanced. [Note: Antarctic sea ice is currently near record high levels]
“In many ways, these measurements of terminus change are like canaries in a mine — they don’t give us all the information we would like, but they are worth taking notice of.”
The researchers found that despite large fluctuations in terminus positions between glaciers — linked to their size — three significant patterns emerged:
- In the 1970s and 80s, temperatures were rising and most glaciers retreated;
- During the 1990s, temperatures decreased and most glaciers advanced;
- And the 2000s saw temperatures increase and then decrease, leading to a more even mix of retreat and advance.
Trends in temperature and glacier change were statistically significant along the East Antarctic Ice Sheet’s warmer Pacific Coast, but no significant changes were found along the much cooler Ross Sea Coast, which might be expected if climate is driving the changes, the Durham researchers said.