Posted on May 23, 2015 by Bob Berwyn
Study shows widespread, simultaneous ice shelf melting
Satellite data shows sudden shift in ice shelf dynamics along the southern Antarctic Peninsula. @berwyn photo.
FRISCO — Along with studies showing dramatic changes in individual ice shelves in Antarctica, new research shows widespread changes in the region since 2009. Up until then, the Southern Antarctic Peninsula showed no signs of change.
But suddenly, multiple glaciers along a vast coastal expanse, measuring some 750km in length, suddenly started to shed ice into the ocean at a nearly constant rate of 60 cubic kilometers, or about 55 trillion liters of water, each year. This makes the region the second largest contributor to sea level rise in Antarctica and the ice loss shows no sign of waning. Continue reading
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Posted on March 27, 2015 by Bob Berwyn
Troubling signs of a major meltdown continue
Global warming is nibbling away at Antarctica’s ice sheets, which show declines of up to 18 percent in a new analysis of satellite data. bberwyn photo.
*More Summit Voice stories on global warming changes in Antarctica.
FRISCO — In the dry language of science, researchers this week said that some of Antarctica’s floating ice shelves have thinned by as much as 18 percent in just a couple of decades — a finding that provides “new insights on how the Antarctic ice sheet is responding to climate change.”
After analyzing 20 years of satellite data, the new NASA-supported study shows the ice volume decline is accelerating under a thickening blanket of greenhouse gases. Merging data from three overlapping missions, the study was able to show the trend over time rather than just offering a snapshot view of the ice.
“Eighteen percent over the course of 18 years is really a substantial change,” said Paolo. “Overall, we show not only the total ice shelf volume is decreasing, but we see an acceleration in the last decade.” said Scripps graduate student Fernando Paolo. Continue reading
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Posted on March 25, 2015 by Bob Berwyn
Study projects increasing rate of coastal erosion
FRISCO — As sea level rises, Hawaii’s beaches are on track to shrink by 20 to 40 feet during the next few decades, scientists announced in a new study.
“When we modeled future shoreline change with the increased rates of sea level rise projected under the IPCC’s “business as usual” scenario, we found that increased SLR causes an average 16 – 20 feet of additional shoreline retreat by 2050,” said lead author Tiffany Anderson, a post-doctoral researcher at the UHM School of Ocean and Earth Science and Technology. Continue reading
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Posted on March 19, 2015 by Bob Berwyn
Seafloor channels sluicing warm ocean water toward base of East Antarctica’s Totten Glacier
Are Antarctica’s ice sheets near a global warming tipping point? bberwyn photo.
FRISCO — Scientists say they’re a step closer to understanding the extreme thinning of East Antarctica’s largest glacier, which contains enough ice to raise global sea level by about 11 feet.
Ocean gateways are sluicing warm water toward the base of the Totten Glacier near the shoreline, undercutting the icy anchors that slow the advance of the ice toward the sea, according to researchers with the University of Texas at Austin’s Institute for Geophysics, who outline their findings in the March 16 edition of the journal Nature Geoscience.
Similar findings from the region were reported by Australian scientists just a few weeks ago, and another study showed widespread thinning of ice in East Antarctica. Continue reading
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Posted on March 17, 2015 by Bob Berwyn
New ice core analysis shows less of an ‘offset’ than most models currently project
Increasing snowfall in Antarctica will moderate the rate of global sea level rise — but not as much as previously thought. bberwyn photo.
FRISCO — Detailed ice core records from Antarctica show that snowfall over the frozen continent increased about 5 percent for each degree (Celsius) of warming as Earth emerged from the last ice age.
The findings confirm that the increased snowfall will slightly offset sea level rise, as suggested by other research — but not as much as previously thought. That means that some computer models may be underestimating the amount and rate of future sea level rise if they’re based on inaccurate assumptions. Continue reading
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Posted on March 11, 2015 by Bob Berwyn
Will the West Antarctic Ice Sheet slip-slide away as the Southern Ocean warms up? bberwyn photo
A delicate balance
FRISCO — West Antarctica ice sheets are delicately anchored in place along a narrow sliver called the grounding zone, and new research shows that even slight increases in regional ocean and air temperatures are likely to destabilize the ice. The grounding zone is a sloping rock bed that lies below sea level.
In the new study, published this month in the Journal of Glaciology, Caltech scientists said future estimates of sea level rise need to take into account that the ice sheets are more sensitive to temperature perturbations driven by climate change than previously thought.
“Our results show that the stability of the whole ice sheet and our ability to predict its future melting is extremely sensitive to what happens in a very small region right at the grounding line. It is crucial to accurately represent the physics here in numerical models,” said study coauthor Andrew Thompson, an assistant professor of environmental science and engineering at Caltech. Continue reading
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Posted on January 22, 2015 by Bob Berwyn
A meltwater lake on the surface of the Greenland Ice Sheet. Now researchers are tracking where that water goes, and how it may affect ice sheet movement. Photo courtesy Thomas Nylen, National Science Foundation.
Surface meltwater feeds subglacial lakes
FRISCO — Scientists who recently took a close look at the “plumbing” of the Greenland Ice Sheet say that meltwater from the surface is building up lakes beneath the ice and transporting heat to the bottom of the ice sheet.
The research, led by Cornell University Earth and Atmospheric Sciences researcher Michael Willis, includes groundbreaking findings that give new information about atmospheric warming and its affect on the critical zone at the base of the ice. The warmth provided by the water could make the ice sheet move faster and alter how it responds to the changing climate. The research is detailed in a new paper published online by the journal Nature on Jan. 21. Continue reading
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