Canadian Glaciers Now Major Contributor to Sea Level Change, UCI Study Shows

Nine times more ice is melting annually due to warmer temperatures

Article ID: 669468

Released: 14-Feb-2017 2:15 PM EST

Source Newsroom: University of California, Irvine

  • Credit: NASA / John Sonntag

    Canada’s glaciers and ice caps are now a major contributor to sea level change, a new UCI study shows. Ten times more ice is melting annually due to warmer temperatures. Seen here is the edge of the Barnes Ice Cap in May 2015.

  • Credit: UCI

Newswise — Irvine, Calif., Feb. 14, 2017 — Ice loss from Canada’s Arctic glaciers has transformed them into a major contributor to sea level change, new research by University of California, Irvine glaciologists has found.

From 2005 to 2015, surface melt off ice caps and glaciers of the Queen Elizabeth Islands grew by an astonishing 900 percent, from an average of three gigatons to 30 gigatons per year, according to results published today in the journal Environmental Research Letters.

“In the past decade, as air temperatures have warmed, surface melt has increased dramatically,” said lead author Romain Millan, an Earth system science doctoral student.

The team found that in the past decade, overall ice mass declined markedly, turning the region into a major contributor to sea level change. Canada holds 25 percent of all Arctic ice, second only to Greenland.

The study provides the first long-term analysis of ice flow to the ocean, from 1991 to 2015.

The Canadian ice cap has glaciers on the move into the Arctic Ocean, Baffin Bay and Nares Strait. The researchers used satellite data and a regional climate model to tally the “balance” of total gain and loss each year, and the reasons why. Because of the huge number of glaciers terminating in area marine basins, they expected that discharge into the sea caused by tide water hitting approaching glacier fronts would be the primary cause.

In fact, they determined that until 2005, the ice loss was caused about equally by two factors: calving icebergs from glacier fronts into the ocean accounted for 52 percent, and melting on glacier surfaces exposed to air contributed 48 percent. But since then, as atmospheric temperatures have steadily climbed, surface melt now accounts for 90 percent.

Millan said that in recent years ice discharge was only a major component in a few basins, and that even rapid, short term increases from these ice fields only had a minor impact on the long-term trend.

Millan added, “We identified meltwater runoff as the major contributor to these ice fields’ mass loss in recent years. With the ongoing, sustained and rapid warming of the high Arctic, the mass loss of the Queen Elizabeth Islands area is likely to continue to increase significantly in coming decades.”

Fellow authors are UCI professor of Earth system science Eric Rignot and UCI assistant research scientist Jeremie Mouginot. NASA provided funding.

About the University of California, Irvine: Founded in 1965, UCI is the youngest member of the prestigious Association of American Universities. The campus has produced three Nobel laureates and is known for its academic achievement, premier research, innovation and anteater mascot. Led by Chancellor Howard Gillman, UCI has more than 30,000 students and offers 192 degree programs. It’s located in one of the world’s safest and most economically vibrant communities and is Orange County’s second-largest employer, contributing $5 billion annually to the local economy. For more on UCI, visit www.uci.edu.

Media access: Radio programs/stations may, for a fee, use an on-campus ISDN line to interview UCI faculty and experts, subject to availability and university approval. For more UCI news, visit news.uci.edu. Additional resources for journalists may be found at communications.uci.edu/for-journalists.

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