Alien species could damage Antarctic ecosystems

By Monica Heger, OurAmazingPlanet

Alien species, like the chironomid midge, can thrive in icy Antarctic climates and could damage the environment if they were to expand.

A tiny fly not native to Antarctica has proven it can not only withstand the icy polar climate, but thrive within it. This insect invader is just one of many foreign species that have reached several islands around Antarctica, with possible consequences for the native flora and fauna.

Scientists with the British Antarctic Survey (BAS) have discovered that a species of fly originally from South Georgia, the chironomid midge, has flourished since its accidental introduction to Signy Island in the Antarctic in the 1960s. It has expanded to more than 650 feet (200 meters) away from its original site, and in some areas is more numerous than any of the native insects.

“There’s a risk of the flies becoming persistent and then turning into something invasive and damaging,” said Peter Convey, a terrestrial ecologist with the BAS, who, along with study author Kevin Hughes, environmental research and monitoring manager at the BAS, presented research on invasive species in Antarctica at the International Polar Year science conference in Oslo last week.

The fly likely traveled unnoticed on the backs of plants that were brought to Antarctica for research purposes, Convey said. It was discovered in the 1980s, but didn’t seem to be causing any harm. Then in the 1990s and early 2000s, its populations exploded, Convey said.

“There’s been a lot more recognition that alien species are a threat to ecosystems and more likely to become established,” he told OurAmazingPlanet.

The flies are decomposers, breaking down waste and recycling it back into the soil. While their function is actually beneficial, Convey said that the fact that they’ve become so numerous could be problematic. At their densest — over 400,000 larvae per square meter (about 11 square feet) — the flies make up more biomass than all other arthropods. Convey and his team are now studying the effects the fly is having on the rest of the ecosystem.

This study and other recent research on invasive species in the Antarctic should serve as a warning, said Yves Frenot, director of the French Polar Institute.

“Due to significant climate change and an increase in the number of visitors [to Antarctica], the risk of introduction and establishment of non-native species is extremely high,” he told OurAmazingPlanet.

Already, there are around 200 non-native species on the sub-Antarctic islands including mice, rats, sheep, cats, beetles and aphids. Ground beetles in particular have been extremely invasive, preying on the native insects.

“On the islands where you see them, you get very big drops, sometimes extinctions, of local insects,” Convey said.

[Ed- Apols for full quote]

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Antarctica’s enigmatic Gamburtsev Subglacial Mountains revealed

By Adele Rackley for Planet Earth Online

The newest images of the Gamburtsev Subglacial Mountains (GSM) were presented at the International Polar Year conference in Oslo this week, showing the features of this enigmatic mountain range in unprecedented detail.

Scientists from the British Antarctic Survey (BAS) were part of the seven-nation Antarctica’s Gamburtsev Province project (AGAP), one of the most ambitious Antarctic missions of the International Polar Year.

The team used sophisticated radar, magnetic and gravity sensors to complete an airborne survey of 20% of this previously unexplored and incredibly inhospitable area.

The GSM was the birthplace of the vast East Antarctic Ice Sheet (EAIS), which now covers the main peaks to a depth of up to 3km. The EAIS covers 10 million km2 so understanding how this remote region is likely to respond to climate change and contribute to sea-level rise is very important.

First identified by Soviet scientists in 1958, the GSM lie under the highest part of the EAIS, known as Dome A. The survey images clearly show the high-relief, alpine-style landscape of the GSM and the network of valleys branching across them. The profiles show that the valleys were carved by fluvial (river) as well as glacial activity.

‘It’s likely that the valleys were initially eroded by rivers, which points to the fact that the mountains were there long before the ice began to form, about 35 million years ago,’ says Dr Kathryn Rose of BAS. ‘As temperatures fell, glaciers formed on the highest peaks and followed the path of the existing drainage system,’ she adds.

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Researchers snap signs of illegal fishing

By Mark Horstman for ABC News Australia

Scientists investigating deep sea life in a supposedly pristine area of the Southern Ocean near eastern Antarctica have been shocked to find what they believe is evidence of illegal fishing there.

The scientists were using an experimental “benthic trawl” net fitted with cameras to get their first look at an unexplored undersea plateau within Australian Antarctic Territory, known as Bruce Rise.

But the first photos of the sea floor from about 1500 metres depth were not what the team expected to see.

“We were expecting reasonably complex rocky reefs, perhaps more coral reefs like were observed further to the east … however, we didn’t find anything like that – it was mud,” said project leader Andrew Constable, from the Australian Antarctic Division in Hobart.

“But what was really interesting as well is that on that mud were a whole bunch of long straight furrows. And we repeatedly encountered those.”

Dr Constable believes the furrows are marks gouged by bottom longlines set to catch patagonian toothfish – all the more surprising because that area of Bruce Rise is closed to fishing.

“We were very surprised, firstly that we observed them, but secondly, we couldn’t believe the number of them. The intensity of fishing in the area was certainly beyond what we would expect,” he said.

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Arctic explorers take first-ever water samples at north pole

Adam Vaughan for The Guardian

Catlin Arctic survey drills ‘hole in the pole’ to collect water samples that will be used to measure ocean acidification

Arctic explorers have taken the first-ever samples of ocean water at the north pole after a gruelling two-and–a-half month expedition across the polar ice.

Headed by former bank manager Ann Daniels, the Catlin Arctic survey team achieved what last year’s expedition – led by polar explorer Pen Hadow – failed to do: reach the north pole and take water samples to measure the impact of a changing climate.

Pen Hadow, the survey’s director and last year’s expedition leader, said: “It’s not possible to imagine what this team has had to do to pull off this extreme survey. I consider them to be the world’s toughest to have done this.”

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Greenland glacier slide speeds 220 percent in summer

Meantime… at the other end of the world Maria Golovnina reports for Reuters

(Reuters) – A glacier in Greenland slides up to 220 percent faster toward the sea in summer than in winter and global warming could mean a wider acceleration that would raise sea levels, according to a study published Sunday.

A group of experts led by Ian Bartholomew at Edinburgh University in Scotland said the variability was much stronger than earlier observations of glacier movement in Greenland.

The study, published in the journal Nature Geoscience, is a new piece of a puzzle to understand the world’s second biggest ice sheet behind Antarctica. Greenland has enough ice to raise world sea levels by about 7 meters (23 ft) if it all melted.

The study said GPS satellite measurements of the glacier in south-west Greenland, up to 35 km (22 miles) inland and at altitudes of up to 1,095 meters (3,592 ft), showed that the ice in some places slid at 300 meters per year at peak summer rates.

“Our measurements reveal substantial increases in ice velocity during summer, up to 220 percent above winter background values,” it said.

The scientists said that the summer slide might be linked to melt water seeping under the ice. It did not speculate if the change in speed between summer and winter was part of natural shifts or was influenced by a changing climate.

But they wrote: “In a warming climate, with longer and more intense summer melt seasons, we would expect that water will reach the bed farther inland and a larger portion of the ice sheet will experience summer velocity changes.”

The United Nations panel of climate experts said in 2007 that global warming was unequivocal and that it was more than 90 percent certain that most warming in the past half century was caused by human activities led by the burning of fossil fuels.

The U.N. panel has come under fire this year after officials said its latest report in 2007 exaggerated the pace of melt of Himalayan glaciers by saying they might all disappear by 2035.

More than 250 members of the U.S. National Academy of Sciences Thursday defended climate change research against “political assaults,” and said that any delay in tackling global warming heightens the risk of a planet-wide catastrophe.

[Ed-Apols for full quote]

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How does ice flow? – Scientists from the Alfred Wegener Institute present first results of a new measurement method in Antarctica

Alfred Wegener Institute

Bremerhaven, 5 Mai 2010. Currently the yearly General Assembly of the European Geological Union takes place in Vienna, Austria. Dr. Olaf Eisen from the German Alfred Wegener Institute presents results from an environmentally friendly measurement method that he and his colleagues used on an Antarctic ice-shelf for the first time in early 2010. It supplies data that are input to models for the ice mass balance and thus permit better forecasting of future changes in the sea level.

The quality of scientific models depends to a decisive degree on the available database. Therefore members of a young investigators group supported by the German Research Foundation (DFG) now applied a special geophysical measurement method, vibroseismics, for data collection in the Antarctic for the first time. “By means of vibroseismic measurements, we would like to find out more about the structure of the ice and thus about the flow characteristics of the Antarctic ice sheet,” explains Dr. Olaf Eisen from the Alfred Wegener Institute for Polar and Marine Research in the Helmholtz Association. He is head of the LIMPICS young investigators group (Linking micro-physical properties to macro features in ice sheets with geophysical techniques).

Eisen now presents first results from geophysical measurement campaign in the Antarctic on the international conference. The objective of the expedition was to determine the internal structure of an ice sheet from its surface by means of geophysical methods. The cooperation partners are the Universities of Bergen (Norway), Swansea (Wales, UK), Innsbruck (Austria) and Heidelberg (Germany) and the Commission for Glaciology of the Bavarian Academy of Sciences and Humanities. For test purposes vibroseismics was used along with proven explosive seismic methods for the first time on an ice sheet.

One of the problems involved in the application of seismic methods on ice sheets is the very porous firn layer, which may be 50 to 100 metres thick. Explosive seismics involves drilling a hole, approximately 10 to 20 metres deep, into the firn to achieve a better coupling between the explosive charge and the surrounding firn or ice. Drilling takes a lot of time and permits only slow progress along the seismic profiles. Vibroseismics entails the generation of seismic waves directly on the surface. For this purpose the vibrator pad of a 16-ton vibroseis truck of the University of Bergen is pressed onto the precompressed firn and set into operation at a defined vibration rate. In contrast to explosive seismic methods, the excited seismic signal is known and can be repeatedly generated as frequently as desired, leading in the end to improved data quality. However, the loss of seismic energy in the porous firn is a disadvantage. Therefore, the scientists compare the explosive seismic and vibroseismic methods quantitatively and in this way want determine how much energy is propagating from the surface through the ice and reflected back to the surface. First data analyses show that vibroseismics is coequal to the classic explosive seismics concerning the amplitude of the waves sent into deeper snow and ice layers. An explicit advantage is the lower effort and thus less time and energy the scientists spend to measure seismic profiles now.

Yngve Kristoffersen, professor of geophysics at the University of Bergen, who provides the vibroseismic equipment, explains: “The successful pilot study opens up a new era for efficient and more environmentally friendly methods for obtaining seismic information on the internal structure of the ice and the bedrock underneath it. This would extend our knowledge about how the ice sheet moves across the bedrock and about the geological structure of the rock under the ice.” Furthermore, in the coming years this method will be applied during pre-site surveys of future geological drill sites under ice shelves, which will contribute to a better understanding of climate history.

Notes for editors:

Your contact is Dr Olaf Eisen from the Alfred Wegener Institute (phone: +49 471 4831-1969; e-mail: Olaf.Eisen(at)awi.de). Your contact in the Communication and Media Department of the Alfred Wegener Institute is Folke Mehrtens (phone: +49 471 4831-2007; e-mail: Folke.Mehrtens(at)awi.de).

The Alfred Wegener Institute conducts research in the Arctic, Antarctic and oceans of the high and mid latitudes. It coordinates polar research in Germany and provides major infrastructure to the international scientific community, such as the research icebreaker Polarstern and stations in the Arctic and Antarctic. The Alfred Wegener Institute is one of the sixteen research centres of the Helmholtz Association, the largest scientific organisation in Germany.

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Unlocking Secrets from the Ice In a Rapidly Warming Region

Yale Environment 360

Earlier this year, climatologist Ellen Mosley-Thompson led an expedition to drill into glacial ice on the Antarctic Peninsula, one of the world’s fastest-warming regions. In an interview with Yale Environment 360, Mosley-Thompson explains what the Antarctic ice cores may reveal and describes what it’s like working in the world’s swiftly melting ice zones.

Ellen Mosley-Thompson and her husband, Lonnie Thompson, are two of the world’s most respected climatologists and glaciologists, traveling around the globe to bore holes in shrinking glaciers and ice sheets. Mosley-Thompson works mainly at the poles, in Greenland and Antarctica, while her husband has done more ice corings of low-latitude glaciers — in the Andes, Africa, and the Himalayas — than any other person alive. Their work, taken together, paints a sobering portrait of the rapid retreat of most of the world’s glaciers and ice caps in the face of the buildup of planet-warming greenhouse gases.

Several months ago, during the Antarctic summer, Mosley-Thompson — the director of the Byrd Polar Research Center at Ohio State University — returned to Antarctica for the ninth time to head a six-person expedition to the Bruce Plateau on the Antarctic Peninsula. The peninsula has warmed faster than almost any other place on Earth, with winter temperatures increasing by 11 degrees F over the past 60 years and year-round temperatures rising by 5 degrees F. As a result, sea ice now covers the western Antarctic Peninsula three months less a year than three decades ago, 90 percent of glaciers along the western Antarctic Peninsula are in retreat, and large floating ice shelves are crumbling.

The most famous of those ice shelves is the Larsen B, a slab of ice — once the size of Connecticut — that disintegrated spectacularly in 2002 in the Weddell Sea. Mosley-Thompson’s expedition was part of a larger study to research the collapse of the Larsen A & B ice shelves and to place this major event in the context of previous eras of climate change.

Working for 42 days in frigid temperatures at 6,500 feet, Mosley-Thompson and her team encountered numerous hardships and difficulties, including the loss of ice drills. Thanks to the ingenuity and engineering skills of her team members, the group finally succeeded in drilling 1,462 feet to the bedrock atop the Bruce Plateau. When the ice cores return to Ohio State in June, Mosley-Thompson and her colleagues hope to analyze the ice to track the history of climate change for thousands of years, perhaps to the last glacial period and beyond.

But even before she analyzes her latest drilling samples, Mosley-Thompson tells Yale Environment 360 senior editor Fen Montaigne, one thing is clear: the retreat of the world’s glaciers, coupled with evidence from other Antarctic ice cores showing atmospheric concentrations of CO2 at their highest levels in more than 800,000 years, “tells us very clearly that we have a serious problem.”

Link to Interview Here…

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Eric Borjeson, cinematographer for Disneynature’s ‘Oceans,’ talks about swimming with sharks

BY ISSIE LAPOWSKY DAILY NEWS STAFF WRITER

There’s deep-sea diving, and then there’s being surrounded by a gang of sharks.

Eric Borjeson prefers the latter.

“You just have to think of a shark as a beautiful animal that doesn’t want to harm you and is just living its life.”

Easy for him to say. The 46-year-old Swede, a pro diver turned cinematographer, spent the last five years under-water filming Disneynature’s documentary “Oceans,” which opened Wednesday. With four other divers, he shuttled between Cape Town and Antarctica, in search of some of the world’s scariest sea life.

“The vision was clear from the beginning,” Borjeson says. “The producers wanted us to be with the animals, not just look at them.”

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What did I do over 2009 at Mawson Station?

A 10 min. documentary.

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Thanks Saint Onion!

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A kite’s eye view for Antarctic conservationists

By Pauline Askin for Reuters Life!

CAPE DENISON, Antarctica (Reuters Life!) – The high winds and freezing conditions of Antarctica can be perilous, but for some it’s the perfect opportunity to fly a kite, in the name of conservation.

The kite is an aerial photography device providing a birds’ eye view of the icy, windy plateau that is home to the historic huts built by Australian explorer Sir Douglas Mawson and his team during their 1911-14 Australian Antarctic Expedition to Cape Denison in East Antarctica.

The vicious wind, which screams down the plateau, blew at more than 140 km/h (nearly 90 mph) for 12 hours in 1913, nearly killing Mawson and his men, and has been ravaging the Oregon and Baltic Pine huts ever since.

This year, ten members of the Mawson’s Huts Foundation are trying to repair some of the damage during their six-week stay in one of the world’s most hostile environments, carrying on restoration work termed Project Blizzard that began in 1985.

“This is a unique conservation job in the respect that we are in Antarctica and have to deal with unusual things like ice levels and strong winds. There are no other place in the world exposed to that kind of wind,” Marty Passingham, senior heritage carpenter, told Reuters.

Read the punchline. It’s worth it.

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