Sunday, November 17, 2013

Could volcanoes be causing Antarctic ice loss?

AFP - Accelerating ice loss from the Antarctic ice sheet could be due in part to active volcanoes under the frozen continent's eastern part, a study said on Sunday.
From 2002 to 2011, the average annual rate of Antarctic icesheet loss increased from about 30 billion tonnes to about 147 billion tonnes, the UN's panel of climate scientists reported in September.
The icesheet is a mass of glacial land ice -- one such sheet covers most of Greenland and the other Antarctica, and together they contain most of the freshwater on Earth.
The sheets are constantly moving, slowly flowing downhill and seawards under their own weight. Portions that extend out over the water are called ice shelf.

Previous research has blamed warmer seas swirling in a circular fashion around Antarctica for the quicker pace of icesheet loss from the southernmost continent.
These waters erode ice shelves, went the theory. And as more of the shelves disappeared, the quicker the sheet would flow and lose ice to the sea.
But in a new paper in the journal Nature Geoscience geologists led by Amanda Lough at Washington University in St. Louis, Missouri, suggested that, in West Antarctica, the faster flow may be also be due to volcanoes.
These heat the underside of the ice, causing melting that lubricates the flow, they suggested.
Evidence for this comes from recently deployed sensors that recorded two "swarms" of seismic activity under Mary Byrd Land, a highland region of West Antarctica, in 2010 and 2011.
Using ice-penetrating radar, the team found an intriguing elliptically-shaped deposit, measuring about 1,000 square kilometres (386 square miles) in the area, at a depth of 1,400 metres (4,550 feet).
  • The deposit is believed to be volcanic ash, spewed out by an enormous eruption some 8,000 years ago -- an estimate reached on the assumption it has since been covered by ice accumulating at the rate of 12.5 centimetres (five inches) a year.
"Together, these observations provide strong evidence for ongoing magmatic activity and demonstrate that volcanism continues to migrate southwards."
Several volcanoes were known to exist in West Antarctica, but none were thought to be active.
"Eruptions at this site are unlikely to penetrate the 1.2 to two-km (0.75-1.2-mile) -thick overlying ice, but would generate large volumes of melt water that could significantly affect ice stream flow," said the study.

1 comment:

  1. Volcanoes still active under Antarctic ice, study confirms...

    Deep under the ice sheet covering Antarctica, volcanic fire still rages, a new study shows. The movement of magma, which may signal an upcoming eruption, was spotted by tell-tale signs of ‘tremor swarms’ in the west of the frigid continent.

    Antarctica features a number of volcanoes elevating above its surface, the most active and well-known being Mound Erebus. Hence there have long been suspicions that some volcanic activity is occurring under the ice as well. This is indeed so, confirms a study published on Sunday last week in the journal Nature Geoscience, and it may have an effect on global climate change.

    The authors of the paper studied the so-called Executive Committee Range, a series of volcanoes in Antarctica’s Marie Byrd Land, a desolate region in the west of the continent. They lie in more or less a straight line with volcanoes becoming progressively younger further to the south. The oldest in the chain, Whitney Peak, is estimated to be 13.2 to 12.7 million years old, while the youngest, Mount Waesche, formed about 1 million years ago.

    Amanda Lough of Washington University in St Louis, Missouri, along with her colleagues, found that magma is still stirring under the Executive Committee Range thanks to seismic data gathered stations, installed on the ice between 2007 and 2010.

    The station’s purpose is studying of the interaction between ice and the Earth’s crust. But among the data Lough found a series of unusual tremors, most of them occurring during two ‘seismic swarms’ in the first two months of 2010 and in March 2011.

    The quakes were 25 to 40km deep, which meant they were not produced by the movement of ice. They also had a fairly low frequency, between 2 and 4 Hertz, suggesting they were not caused by an earthquake produced by tectonic plates grinding against each other.

    Finally, the 1,370 tremors were centered on a point 55km south of Mount Waesche, the spot where volcanic activity should be now if the linear trend of Executive Committee Range continued.

    While the exact nature of the quakes could not be identified for certain, they are consistent with magma movements recorded in volcanic areas of Alaska’s Aleutian Islands, the Pacific Northeast, Hawaii and Mt. Pinatubo in the Philippines, the study says. Those sometimes indicate an upcoming eruption.

    Researchers cross-checked the seismic data with results of geomagnetic and radar mapping of the area. A slightly higher magnetic field suggested that there was a bump in the crust, a sign of magmatic activity under it. There are also indications of a layer of volcanic ash embedded in the ice, with its depth putting it about 8,000 years in the past. The team believes that the ash came from an eruption of Mount Waesche.

    There is no sign that any eruptions occurred since then, and if they did, it would have to be a big one to melt the 1km thick ice sheet covering the location. But the head coming from a volcano could affect the movement of the ice by lubricating it. Scientists however are not sure how big an impact it would cause on the climate.


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Δημοσιεύτηκε από Geo Kok στις Πέμπτη, 11 Φεβρουαρίου 2021
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Δημοσιεύτηκε από Geo Kok στις Πέμπτη, 11 Φεβρουαρίου 2021
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