Melting ice in Arctic and Antarctica

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  • #3533

    Worrisome signs re ice melting at both poles.

    From Nat Geo:

    Quote:
    An "alarming rate" of melting in the Antarctic Peninsula has finally snapped the ice bridge that held the Wilkins Ice Shelf in place, experts say.

    The 25-mile-long (40-kilometer-long) ribbon of sea ice that secured the Jamaica-size ice shelf (which is just out of view in the above pictures) to Antarctica had been "hanging by a thread" since August 2008 (above, top, in November 2008 in a European Space Agency satellite image).

    On Saturday, April 4, the bridge broke at its weakest point (bottom)—at about 1,640 feet (500 meters) wide—and shattered into hundreds of small icebergs. The ice shelf, which is now exposed to the open ocean, is more vulnerable to breaking up, experts say.

    "We've been watching it all summer, waiting for it to go, and bang—now it's gone," David Vaughan, a glaciologist for the British Antarctic Survey, told National Geographic News.

    "It's the culmination of yet another ice shelf retreat that's been driven by [warming] climate," Vaughan said.

    The Antarctic Peninsula has warmed 3 degrees Celsius (5.4 degrees Fahrenheit) since the 1950s, he said—"something that people should take note of."

    Jamaica-Size Ice Shelf Breaks Free

    and from BBC:

    Quote:
    Arctic ice reached a larger maximum area this winter than in the last few years, scientists say, but the long-term trend still shows it declining.

    The 30-year trend shows the maximum annual sea-ice cover, usually seen in March, is shrinking by 2.7% per decade.

    Only 10% of the cover consists of relatively durable ice that has formed over more than two years, a record low.

    Scientists from the US National Snow and Ice Data Center (NSIDC), say the thin ice is prone to summer melting.

    "Thickness is important, especially in the winter, because it is the best overall indicator of the health of the ice cover," said NSIDC scientist Walt Meier.

    "As the ice cover in the Arctic grows thinner, it grows more vulnerable to melting in the summer."

    In the 1980s, thick multi-year ice made up 30-40% of the cover, the scientists say.

    The summer minimum area is changing much faster than the winter maxima, shrinking by about 0.7% per year. Last year UK researchers showed that the ice has also markedly thinned in recent years.

    #4638

    WWF release:

    Warming in the Arctic could lead to flooding affecting one quarter of the world’s population, substantial increases in greenhouse gas emissions from massive carbon pools, and extreme global weather changes, according to a new WWF report.

    The Arctic Climate Feedbacks: Global Implications report, released today, outlines dire global consequences of a warming Arctic that are far worse than previous projections. The unprecedented peer-reviewed report brings together top climate scientists who have assessed the current science on arctic warming.

    "What they found was a truly sobering picture,’ said Dr Martin Sommerkorn, senior climate change advisor for WWF’s Arctic programme. ‘What this report says is that a warming Arctic is much more than a local problem, it’s a global problem.

    "Simply put, if we do not keep the Arctic cold enough, people across the world will suffer the effects."

    The report shows that numerous arctic climate feedbacks – negative effects prompted by the impacts of warming — will make global climate change more severe than indicated by other recent projections, including those of the Intergovernmental Panel on Climate Change’s 2007 assessment.

    The dramatic loss of sea ice resulting from the Arctic warming at about twice the rate of the rest of the world will influence atmospheric circulation and weather in the Arctic and beyond. This is projected to change temperature and precipitation patterns in Europe and North America, affecting agriculture, forestry and water supplies.

    In addition, the Arctic’s frozen soils and wetlands store twice as much carbon as is held in the atmosphere. As warming in the Arctic continues, soils will increasingly thaw and release carbon into the atmosphere as carbon dioxide and methane, at significantly increased rates. Levels of atmospheric methane, a particularly potent greenhouse gas, have been increasing for the past two years, and it is suggested that the increase comes from warming arctic tundra.

    In a first-of-its kind assessment incorporating the fate of the ice sheets of Greenland and West Antarctica into global sea level projections, the WWF report concludes that sea- levels will very likely rise by more than one meter by 2100 — more than twice the amount given in the Intergovernmental Panel on Climate Change’s 2007 assessment that had excluded the contribution of ice sheets from their projection. The associated flooding of coastal regions will affect more than a quarter of the world’s population.

    "This report shows that it is urgently necessary to rein in greenhouse gas emissions while we still can," Sommerkorn said. "If we allow the Arctic to get too warm, it is doubtful whether we will be able to keep these feedbacks under control.

    Warming Arctic’s global impacts outstrip predictions

    #4683

    Press release from US Geological Survey:

    Quote:
    Ice shelves are retreating in the southern section of the Antarctic Peninsula due to climate change.This could result in glacier retreat and sea-level rise if warming continues, threatening coastal communities and low-lying islands worldwide.

    Research by the U.S. Geological Survey is the first to document that every ice front in the southern part of the Antarctic Peninsula has been retreating overall from 1947 to 2009, with the most dramatic changes occurring since 1990. The USGS previously documented that the majority of ice fronts on the entire Peninsula have also retreated during the late 20th century and into the early 21st century. 

    The ice shelves are attached to the continent and already floating, holding in place the Antarctic ice sheet that covers about 98 percent of the Antarctic continent. As the ice shelves break off, it is easier for outlet glaciers and ice streams from the ice sheet to flow into the sea. The transition of that ice from land to the ocean is what raises sea level.

    “This research is part of a larger ongoing USGS project that is for the first time studying the entire Antarctic coastline in detail, and this is important because the Antarctic ice sheet contains 91 percent of Earth’s glacier ice,” said USGS scientist Jane Ferrigno. “The loss of ice shelves is evidence of the effects of global warming. We need to be alert and continually understand and observe how our climate system is changing.”

    The Peninsula is one of Antarctica’s most rapidly changing areas because it is farthest away from the South Pole, and its ice shelf loss may be a forecast of changes in other parts of Antarctica and the world if warming continues.

    Retreat along the southern part of the Peninsula is of particular interest because that area has the Peninsula’s coolest temperatures, demonstrating that global warming is affecting the entire length of the Peninsula.

    The Antarctic Peninsula’s southern section as described in this study contains five major ice shelves:  Wilkins, George VI, Bach, Stange and the southern portion of Larsen Ice Shelf. The ice lost since 1998 from the Wilkins Ice Shelf alone totals more than 4,000 square kilometers, an area larger than the state of Rhode Island.

    The USGS is working collaboratively on this project with the British Antarctic Survey, with the assistance of the Scott Polar Research Institute and Germany’s Bundesamt fűr Kartographie und Geodäsie. The research is also part of the USGS Glacier Studies Project, which is monitoring and describing glacier extent and change over the whole planet using satellite imagery.

    The report, “Coastal-Change and Glaciological Map of the Palmer Land Area, Antarctica: 1947—2009” and its accompanying map is available online.

    The other completed reports in the Coastal Change and Glaciological Maps of Antarctica series can be viewed online.

    Ice Shelves Disappearing on Antarctic Peninsula

    Glacier Retreat and Sea Level Rise are Possible Consequences

    #4818

    From the Guardian:

    Quote:
    Arctic sea ice has melted to a level not recorded since satellite observations started in 1972 – and almost certainly not experienced for at least 8,000 years, say polar scientists.

    Daily satellite sea-ice maps released by Bremen university physicists show that with a week's more melt expected this year, the floating ice in the Arctic covered an area of 4.24 million square kilometres on 8 September. The previous one-day minimum was 4.27m sq km on 17 September 2007.

    Arctic temperatures have risen more than twice as fast as the global average over the past half century.

    Separate, less reliable, research suggests that Arctic ice is in a downward spiral, declining in area but also thinning. Using records of air, wind and sea temperature, scientists from the Polar Science Centre of the University of Washington, Seattle, announced last week that the Arctic sea-ice volume reached its lowest ever level in 2010 and was on course to set more records this year.

    Further evidence of dramatic change in the Arctic came last week from Alan Hubbard, a Welsh glaciologist at Aberystwyth University, who has been studying the Petermann glacier in northern Greenland for several years.

    The glacier, which covers about 6% of the icecap, is 186 miles (300km) long and up to 3,280ft (1km) high. In August last year, a 100 square-mile (260 sq km) block of ice calved from the glacier. Photographs show that by July this year it had melted and disappeared.

    "I was gobsmacked. It [was] like looking into the Grand Canyon full of ice and coming back two years later to find it full of water," said Hubbard.

    Arctic sea ice is melting at its fastest pace in almost 40 years

    The Northwest Passage was, again, free of ice this summer and the polar region could be unfrozen in just 30 years

     

     

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