Students on Ice Blog

Educational Expeditions to Antarctica and the Arctic

Archive for July, 2009

SOI Launches Arctic Youth Expedition 2009 Website

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Between July 29th and August 13th parents, students, educators and polar enthusiasts can visit the www.studentsonice.com/arctic2009 Students on Ice Arctic Youth Expedition 2009 website to share all of our expedition moments. We will be posting photos, journal entries and expedition updates on a daily basis! Please note, that occasionally, due to our ship’s position, it may be impossible to send images. Our webmaster back at SOI Head Office will report any expedition developments on the site. But please remember we are in one of the most remote places in the world and flexibility is the key!

The Arctic is an amazing window to our world, and a cornerstone of our global ecosystem. We hope our student expeditioners will return home as ambassadors and leaders for the planet, with new perspective, levels of inspiration and motivation for the future.

Please enjoy your journey with us!

For those interested in joining us on an upcoming Students on Ice Arctic or Antarctic expedition, please visit our main website or contact our office.

In the expedition spirit,

Geoff Green
Executive Director and Expedition Leader,
Students on Ice

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Global warming impacts animation: Arctic

The impacts of global warming will be particularly dramatic for the Arctic and Antarctica. In this animation, we look more closely at the consequences for the Arctic.

Signs of ancient Arctic sea ice: At least 47.5 million years ago

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These 3-micrometer-wide needle-shaped fossils of marine algae from the genus Synedropsis indicate that sea ice first formed in the Arctic Ocean at least 47.5 million years ago. (Credit: C. Stickley/University of Tromsø, Richard Pearce/National Oceanographic Centre, Southampton)

Signs of ancient sea ice
Fossils of certain marine algae suggest floating ice debuted in the Arctic at least 47.5 million years ago

by Sid Perkins

Science News (July 15, 2009) — Fossils of ice-dependent algae reveal that Arctic sea ice, which is today very much an endangered species, formed at least 47.5 million years ago, about 1.5 million years earlier than previously recognized.

Sediments on the bottom of the Arctic Ocean often contain pebbles and mineral grains carried to sea by icebergs or by ice that formed in shallow water along the coast. Previous analyses of such ice-rafted debris, such as physical studies of the shape and surface texture of those bits of rock, suggest that sea ice first graced the Arctic Ocean, at least seasonally, about 46 million years ago, says Catherine Stickley, a micropaleontologist at the University of Tromsø in Norway. However, new analyses of fossils in the sediments push back the date ice first appeared, Stickley and her colleagues report in the July 16 Nature.

The researchers examined sediments drilled from a site on a submarine ridge about 250 kilometers from the North Pole, where waters today are about 1,300 meters deep. The critical clue betraying the presence of ancient sea ice — fossils of marine algae whose modern cousins depend on sea ice as habitat — are found in sediments deposited about 47.5 million years ago, says Stickley. Remains of those needle-shaped microorganisms, part of the Synedropsis genus, make up as much as 61 percent of the fossils in those sediments.

The team’s findings provide new details about the timing and pace of global cooling that was occurring during an era when atmospheric concentrations of carbon dioxide were declining, Stickley notes.

For more information, visit
http://www.sciencenews.org/view/generic/id/45561/title/Signs_of_ancient_sea_ice_

Runaway spurt of global warming turned Earth into a hothouse

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Close up of a melting glacier. A runaway spurt of global warming 55 million years ago turned Earth into a hothouse but how this happened remains worryingly unclear, scientists said. (AFP/File/Jorge Vinueza)

Mystery mechanism drove global warming 55 million years ago

AFP PARIS (July 13, 2009) — A runaway spurt of global warming 55 million years ago turned Earth into a hothouse but how this happened remains worryingly unclear, scientists said on Monday.

Previous research into this period, called the Palaeocene-Eocene Thermal Maximum, or PETM, estimates the planet’s surface temperature blasted upwards by between five and nine degrees Celsius (nine and 16.2 degrees Fahrenheit) in just a few thousand years.

The Arctic Ocean warmed to 23 C (73 F), or about the temperature of a lukewarm bath.

How PETM happened is unclear but climatologists are eager to find out, as this could shed light on aspects of global warming today.

What seems clear is that a huge amount of heat-trapping “greenhouse” gases — natural, as opposed to man-made — were disgorged in a very short time.

The theorised sources include volcanic activity and the sudden release of methane hydrates in the ocean.

A trio of Earth scientists, led by Richard Zeebe of the University of Hawaii, try to account for the carbon that was spewed out during PETM.

They believe that levels of atmospheric carbon dioxide (CO2) rose by 70 percent during PETM’s main phase to reach 1,700 parts per million (ppm), attaining a concentration of between four and five times that of today.

But all this CO2 can only account for between one and 3.5 C (1.8-6.3 F) of PETM’s warming if the models for climate sensitivity are right, the team found.

There must have been some other factor that stoked temperatures higher.

Even though there are big differences between Earth’s geology and ice cover then and now, the findings are relevant as they highlight the risk of hidden mechanisms that add dramatically to warming, says the paper.

Some of these so-called “positive feedbacks” are already known.

For instance, when a patch of Arctic sea ice melts, this exposes the uncovered sea to sunlight, depriving it of a bright, reflective layer.

That causes the sea to warm, which leads to the loss of more ice, which in turn helps the sea to warm, and so on.

But these “feedbacks” are poorly understood and some scientists believe there could be others still to be identified.

“Our results imply a fundamental gap in our understanding about the amplitude of global warming associated with large and abrupt climate perturbations,” warns Zeebe’s team.

“This gap needs to be filled to confidently predict future climate change.”

After the big warm-up, the planet eventually cooled around 100,000 years later, but not before there had been a mass extinction, paving the way to the biodiversity that is familiar to us today.

Man-made global warming, driven mainly by the burning of oil, gas and coal, has amounted to around 0.8 C (1.12 F) over the past century.

Last week in L’Aquila, Italy, the Group of Eight (G8) industrialised countries and other economies that together account for 80 percent of greenhouse-gas emissions pledged to try to limit overall warming to 2 C (3.6 F) over pre-industrial times.

SOI celebrates anniversary of Isabella Bay / Niginganiq agreement

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On August 6, Students on Ice plans to visit the hamlet of Clyde River, Nunavut, as part of the Students on Ice – International Polar Year Arctic Youth Expedition 2009. Celebrating the establishment of Niginganiq National Wildlife Area with Clyde River residents and expedition partners, the expedition later plans to travel to Isabella Bay on August 8. (Photo by Lee Narraway)

Inuit to celebrate anniversary of bowhead sanctuary agreement

CBC News (July 22, 2009) — The federal government has not finalized the creation of a bowhead whale sanctuary off the Baffin Island coast, so Inuit are planning a party next month to nudge the government on the issue.

Inuit land-claims organization Nunavut Tunngavik Inc. (NTI) will hold a party Aug. 6 in the hamlet of Clyde River near the site of the future Niginganiq National Wildlife Area.

The party will mark one year since the federal government signed an Inuit impact and benefits agreement (IIBA) for the 336,200-hectare Niginganiq site.

Located in Isabella Bay, on the northeast coast of Baffin Island, the Niginganiq National Wildlife Area will protect the essential feeding and resting grounds for thousands of bowhead whales.

One year later, the sanctuary has yet to become a reality since the government still has to give it the official stamp of approval.

Election could delay progress

Nunavut Tunngavik president Paul Kaludjak told CBC News that it has been a long wait — one that could get even longer if a federal election is called this fall, he said.

“It’s always on the table. You take it as it comes, and if they call an election, so be it,” he said Tuesday.

“It will be another hurdle that we have to wait for. We look forward to it getting passed through Parliament and going forward with it.”

The Aug. 6 celebration is a way to let people know that the national wildlife area is important for both NTI and the people of Clyde River, Kaludjak said.

‘We always try to be patient’

He admitted the celebration is partly meant to put pressure on Ottawa to make the sanctuary official.

“We always try to be patient, and I know there’s value in terms of the IIBA being positive for the Inuit side, where we see benefits long term,” he said.

In Clyde River, Joannasie Aapak of the local bowhead committee told CBC News the Niginganiq National Wildlife Area will attract tourists and much-needed jobs to the hamlet of about 820.

More than a 100 students and educators travelling on a ship with the Students on Ice program will join the Aug. 6 celebration.

Kaludjak says federal politicians and senior staff are also on NTI’s invitation list.

The World Wildlife Fund estimates about 1,500 to 2,000 whales inhabit the Niginganiq area during the late summer and fall feeding periods.

Clyde River residents have been seeking protection for the area since 1998.

For more information, visit
http://www.cbc.ca/canada/north/story/2009/07/22/nti-bowhead-sanctuary.html

CALL FOR SUBMISSIONS: 2009 IPY Film Festival

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2009 INTERNATIONAL POLAR YEAR FILM FESTIVAL – CALL FOR SUBMISSIONS

The Canadian Film Institute, working in partnership with the International Polar Year, is seeking entries for the International Polar Year Film Festival. The International Polar Year is an event with over 60 countries involved in an intense program of scientific research focused on the Arctic and Antarctic. This special film festival will bring together an international selection of works exploring the issues and activities of the International Polar Year. Ranging from educational works (documentaries, industrial films) to fiction films, the Festival will celebrate the rich diversity of the polar region, as well as examine the many challenges it faces in the 21st Century.

The Canadian Film Institute, committed to programming a dynamic and diverse selection of works related to the representation of the Arctic, welcomes submissions from all film and video practices, including science and research.

The IPY Film Festival will take place from September 28-30, 2009 in the Auditorium of Library and Archives Canada in Ottawa, Ontario, Canada.

Submissions must be sent in a playable DVD or video format (NTSC). Send submissions as soon as possible, as the process of selection is already underway. If possible, please include a director’s biography, filmography, a film still, contact information, and any other relevant information.

Send submissions to:

CANADIAN FILM INSTITUTE
2 Daly Avenue | Suite 120
Ottawa | Ontario | Canada
K1N 6E2
Tel: 613.232.6727
Fax: 613.232.6315
info@cfi-icf.ca

Contact Scott Birdwise of the Canadian Film Institute at birdwise@cfi-icf.ca for further information.

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CFC Replacements Intensify Climate Concerns

The Rise of ‘Super’ Greenhouse Gases

The chemicals that replaced ozone-depleting substances in refrigerators, air conditioners and insulating foam have been found to possess heat-trapping power hundreds or thousands of times that of carbon dioxide. And scientists say the problem is growing: If the world doesn’t decrease these emissions, they could undermine any progress made in reducing other greenhouse gases.

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SOURCE: Proceedings of the National Academy of Sciences
(GRAPHIC: Patterson Clark – The Washington Post)

Chemicals That Eased One Woe Worsen Another

by David A. Fahrenthold

Washington Post (July 20, 2009) — This is not the funny kind of irony: Scientists say the chemicals that helped solve the last global environmental crisis — the hole in the ozone layer — are making the current one worse.

The chemicals, called hydrofluorocarbons (HFCs), were introduced widely in the 1990s to replace ozone-depleting gases used in air conditioners, refrigerators and insulating foam.

They worked: The earth’s protective shield seems to be recovering.

But researchers say what’s good for ozone is bad for climate change. In the atmosphere, these replacement chemicals act like “super” greenhouse gases, with a heat-trapping power that can be 4,470 times that of carbon dioxide.

Now, scientists say, the world must find replacements for the replacements — or these super-emissions could cancel out other efforts to stop global warming.

“Whatever targets you thought you were going to make,” said David Fahey, a physicist at the National Oceanic and Atmospheric Administration, “it will be undermined by the fact that you have . . . additional emissions that you hadn’t planned on.”

The colorless, odorless replacement chemicals enter the atmosphere in tiny amounts, often leaking out of refrigerators and air conditioners, or escaping when those machines break and are improperly dumped. They now account for about 2 percent of the climate-warming power of U.S. emissions, according to the Environmental Protection Agency.

That is still far less than carbon dioxide, which is produced by burning fossil fuels and accounts for about 85 percent of the problem. And it is less than the roughly 10 percent of warming from methane, which comes from sources including farm animals and decomposing trash.

But in recent weeks, these obscure gases have been given a higher profile in the carbon-dominated debate on climate change.

Last month, a group of scientists published a paper projecting that, if unchecked, the emissions would rise rapidly over the next 40 years. By 2050, they found, the amount of super greenhouse gases in the atmosphere might be equal to six or more years’ worth of carbon dioxide emissions.

And last week, diplomats met in Geneva to discuss ideas for a worldwide reduction in HFCs.

“You have this moment when you could nip this problem in the bud and avoid this very large growth of a dangerous chemical,” said David Doniger, policy director at the Natural Resources Defense Council’s climate center, from Geneva. “Now, in the next couple of years, is when you have to do this.”

The roots of the problem go back to the 1970s, when scientists theorized that chemicals called chlorofluorocarbons (CFCs) were slowly eroding stratospheric ozone. That was a dangerous thing, since the ozone layer protects the planet from harmful UV radiation.

In 1987, governments signed the Montreal Protocol, agreeing to reduce CFCs. Since then, this agreement has been a kind of bureaucratic miracle: Ninety-six percent of ozone-depleting substances have been phased out, according to the United Nations.

The United Nations says there is still a hole in the ozone above the South Pole, but global ozone levels are expected to return to their pre-1980 level by about 2050.

“If this were a soccer team . . . it’s won every single game,” said Durwood Zaelke, president of the Institute for Governance and Sustainable Development. “That’s astounding in the international environmental field.”

It worked because chemists engineered substitutes for CFCs, new gases without the propensity to chemically unlock ozone molecules. The replacements could still chill cold cuts and Chevrolets — in refrigerators and under car hoods, they are compressed and uncompressed in a process that sucks heat out of passing air.

But the chemicals’ strong bonds also cause them to act as heat sponges in Earth’s atmosphere, absorbing energy from the sun and keeping it from being reflected out into space. In the “blanket” created by heat-trapping gases, that makes them especially heavy strands.

“Pound for pound, they’re much more powerful than CO2, you know — hundreds or thousands of times more powerful,” said NOAA physicist Fahey.

Exactly how powerful depends on the makeup of the gases. One, common in fridges and auto air conditioners, lasts 12 to 14 years in the atmosphere and has 1,430 times the global warming impact of carbon dioxide. Another has a 52-year life and 4,470 times the power.

According to the recent paper, there will soon be many more of them, as developing countries become more prosperous and their people buy vehicles and air conditioners.

Even if the world makes significant progress in reducing carbon dioxide and methane — still a big if, since recent negotiations on the topic have produced little — the scientists said the growth in HFCs could undo a significant part of their work.

Internationally, the gases are still supposed to be dealt with in the same vast and balky negotiations that will reduce carbon dioxide. So they will probably be on the table when diplomats gather in Copenhagen in December to create a successor to the Kyoto Protocol of 1997.

But many environmental groups, including the nonprofit Environmental Investigation Agency, say they would like to see the gases regulated using the Montreal Protocol, because the framework succeeded in dealing with other pollutants.

“The climate problem is not one global problem. It’s a package of global problems,” said Zaelke, of the Institute for Governance and Sustainable Development. “You can reach in and pull out a piece.”

Sens. John F. Kerry (D-Mass.) and Barbara Boxer (D-Calif.), who chair two powerful committees, urged this approach in a letter to President Obama in April. Last week, an official said the administration was still deciding what approach to support.

A bigger question: What will replace these chemicals? Experts say that some substitutes, with less global warming impact, can be made with new HFCs or by using ammonia or butane. But others are needed. “We don’t know all of them yet,” said Mack McFarland, global environmental manager for DuPont Fluoroproducts, a division of Delaware-based DuPont.

Global warming impacting Greenlanders’ daily lives

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Greenlandic fisherman Johannes Heilmann poses for a photo in front of the shipping harbor of Nuuk fjord. From his trawler that motors along the Nuuk fjord, Heilmann has watched helplessly in recent years as climate change takes its toll on Greenland. Global warming is occurring twice as fast in the Arctic as in the rest of the world. (AFP/File/Slim Allagui)

Global warming impacting Greenlanders’ daily lives

AFP NUUK (July 9, 2009) — From his trawler that motors along the Nuuk fjord, fisherman Johannes Heilmann has watched helplessly in recent years as climate change takes its toll on Greenland.

Global warming is occurring twice as fast in the Arctic as in the rest of the world.

Heilmann, in his 60s with a craggy, rugged face from years of work in the outdoors, says he and his colleagues can no longer take their dogsleds out to the edge of the ice floes to fish because the ice isn’t thick enough to carry the weight.

And yet the freezing waters with large chunks of ice are too difficult to navigate in their small fishing boats, making fishing near impossible.

“We can’t use the sleds any more, the ice isn’t thick enough,” laments Heilmann, saying he now has to rely on bird hunting, and sometimes seal hunting, while waiting for the summer months to go fishing.

At Ilulissat, more than 200 kilometres (125 miles) north of the Arctic Circle, Emil Osterman tells local daily Sermitsiaq how “in 1968, when I was 13, we went fishing in December in the fjord and the ice was several metres thick.”

Now, more than 40 years on, the ice at the very same location at the same time of year “is only 30 centimetres thick.”

The head of Nuuk’s fishing and hunting association, Leif Fontaine, explains how climate warming is also affecting the region’s shrimp industry — Greenland’s main export and biggest industrial sector.

“When the water gets warmer, the shrimp become rarer as they move further north,” he says.

“And the melting ice is worrying, especially for the residents of isolated villages in the north and the east who only have sleds and no boats to hunt, fish and survive,” he adds.

That has forced some hunters to let their sleddogs starve to death, since they can’t provide them with the seals and fish they need to eat.

Polar bears that roam the ice also have an increasingly difficult time finding food, especially seals, as the ice floes melt. As a result they end up approaching villages in search of nourishment, presenting a danger to the locals and themselves.

In Nuuk, residents like Nana Pedersen and Sofus Moeller, two recent high school graduates, are worried about the changes to the climate.

They recall a snowstorm that took place on June 20 — rare even for Greenland.

Moeller says he is “worried” about the changes, but admits that he doesn’t think about it every day.

“I don’t know if it’s warmer than before, since winter after all lasts until May here,” he says.

But at the new Arctic research centre in Nuuk, director Soeren Rysgaard has no doubts that climate change is having an impact.

“It’s very visible in the Arctic.”

Fishermen who pull up fewer fish in their nets or who can no longer fish in certain areas because the ice is too thin are those most affected right now, he says.

But the speaker of the local parliament, Josef Motzfeldt, notes that global warming has also brought “some good.”

A growing number of tourists have come to Greenland to see how climate change is causing the North Atlantic island’s enormous glaciers to melt, and new species never before found in Greenland are turning up, such as sea urchins and squid.

In southern Greenland, the longer summers are benefiting vegetable farmers, who are experiencing some of their most lucrative times.

“Trees are growing and the fields are full of potatoes, lettuce, carrots and cabbage” to be sold at the local market, explains Anders Iversen, who heads a plant nursery near Qaqotorq in the south.

Temperatures are warmer now, with the mercury sometimes rising above 20 degrees Celsius (68 Fahrenheit) in summer, he says.

“If global warming continues, we will be able to grow even more kinds of vegetables during a longer season,” he adds.

The farmers’ hopes could soon be confirmed by new worrying observations in Greenland’s far north.

The Arctic Sunrise, a ship belonging to environmental group Greenpeace, has recently arrived at the Petermann glacier, one of the region’s biggest glaciers that is in the process of breaking up, where experts will study its developments.

For Greenpeace, the shrinking of the glacier is a clear sign that global warming is no longer “a theory, but a harsh reality.”

Arctic climate under greenhouse conditions in the late Cretaceous

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Fossil diatom algae of Cretaceous age from the Alpha Ridge of the Arctic Ocean. (Credit: Image courtesy of National Oceanography Centre, Southampton, UK)

Arctic Climate Under Greenhouse Conditions In The Late Cretaceous

Science Daily (July 17, 2009) — New evidence for ice-free summers with intermittent winter sea ice in the Arctic Ocean during the Late Cretaceous – a period of greenhouse conditions – gives a glimpse of how the Arctic is likely to respond to future global warming.

Records of past environmental change in the Arctic should help predict its future behaviour. The Late Cretaceous, the period between 100 and 65 million years ago leading up to the extinction of the dinosaurs, is crucial in this regard because levels of carbon dioxide (CO2) were high, driving greenhouse conditions. But scientists have disagreed about the climate at this time, with some arguing for low Arctic late Cretaceous winter temperatures (when sunlight is absent during the Polar night) as against more recent suggestions of a somewhat milder 15°C mean annual temperature.

Writing in Nature, Dr Andrew Davies and Professor Alan Kemp of the University of Southampton’s School of Ocean and Earth Science based at the National Oceanography Centre, Southampton, along with Dr Jennifer Pike of Cardiff University take this debate a step forward by presenting the first seasonally resolved Cretaceous sedimentary record from the Alpha Ridge of the Arctic Ocean.

The scientists analysed the remains of diatoms – tiny free-floating plant-like organisms – preserved in late Cretaceous marine sediments. In modern oceans, diatoms play a dominant role in the ‘biological carbon pump’ by which carbon dioxide is drawn down from the atmosphere through photosynthesis and a proportion of it exported to the deep ocean. Unfortunately, the role of diatoms in the Cretaceous oceans has until now been unclear, in part because they are often poorly preserved in sediments.

But the researchers struck lucky. “With remarkable serendipity,” they explain, ” successive US and Canadian expeditions that occupied floating ice islands above the Alpha Ridge of the Arctic Ocean, recovered cores containing shallow buried upper Cretaceous diatom ooze with superbly preserved diatoms.” This has allowed them to conduct a detailed study of the diatom fossils using sophisticated electron microscopy techniques. In the modern ocean, scientists use floating sediment traps to collect and study settling material. These electron microscope techniques that have been pioneered by Professor Kemp’s group at Southampton have unlocked a ‘palaeo-sediment trap’ to reveal information about Late Cretaceous environmental conditions.

They find that the most informative sediment core samples display a regular alternation of microscopically thin layers composed of two distinctly different diatom assemblages, reflecting seasonal changes. Their analysis clearly demonstrates that seasonal blooming of diatoms was not related to the upwelling of nutrients, as has been previously suggested. Rather, production occurred within a stratified water column, indicative of ice-free summers. These summer blooms comprised specially adapted species resembling those of the modern North Pacific Subtropical Gyre, or preserved in relatively recent organically rich Mediterranean sediments called ’sapropels’.

The sheer number of diatoms found in the Late Cretaceous sediment cores indicates exceptional abundances equalling modern values for the most productive areas of the Southern Ocean. “This Cretaceous production, dominated by diatoms adapted to stratified conditions of the polar summer may also be a pointer to future trends in the modern ocean,” say the researchers: “With increasing CO2 levels and global warming giving rise to increased ocean stratification, this style of (marine biological) production may become of increasing importance.”

However, thin accumulations of earthborn sediment within the diatom ooze are consistent with the presence of intermittent sea ice in the winter, a finding that supports “a wide body of evidence for low Arctic late Cretaceous winter temperatures rather than recent suggestions of a 15?C mean annual temperature at this time.” The size distribution of clay and sand grains in the sediment points to the formation of sea ice in shallow coastal seas during autumn storms but suggests the absence of larger drop-stones suggests that the winters, although cold, were not cold enough to support thick glacial ice or large areas of anchored ice.

Commenting on the findings, Professor Kemp said: “Although seasonally-resolved records are rarely preserved, our research shows that they can provide a unique window into past Earth system behaviour on timescales immediately comparable and relevant to those of modern concern.”

Davies, A., Kemp, A. S. & Pike, J. Late Cretaceous seasonal ocean variability from the Arctic. Nature 460, 254-258 (9 July 2009).

http://www.nature.com/nature/journal/v460/n7252/full/nature08141.html

The research was supported by the Natural Environment Research Council.

High-res photos could provide detailed info about sea ice

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Recently declassified high-resolution satellite photos, such as this one from the Canadian Fram Strait, could provide scientists with more detailed information about Arctic sea ice melting. (Credit: Global Fiducials Library/USGS)

ARCTIC IMAGES DECLASSIFIED
High-resolution photos could provide detailed information about changes in sea ice

by Jenny Lauren Lee

Science News (July 15, 2009) — Hundreds of high-resolution satellite photos of the Arctic sea ice taken during the past 10 years should be immediately declassified and released to the scientific research community, the National Research Council reported on July 15. Shortly after, the United States Geological Survey made about a thousand of the images available to the public through the Global Fiducials Library.

“Most people from the scientific community are not aware that these images have been collected,” says Stephanie Pfirman, chair of the NRC committee that wrote the report. “They’ll be very excited to see these results.”

The photos could help scientists study the rapid changes taking place in the Arctic, the committee members say. Current research efforts that might benefit include studies of polar bear habitats, of the movement of ice floes and of the formation and evolution of melt ponds — bodies of water that form on ice sheets and accelerate their melting.

“There are a lot of processes that we still don’t have a good handle on,” such as why Arctic ice is melting faster than models predict it should, says geographer Mark Serreze of the University of Colorado at Boulder. High-resolution satellite imagery is “just the sort of thing we need” to answer these questions, he says.

The satellite project began in the mid-1990s when environmental scientists teamed up with members of the intelligence community to create a program that would see whether “classified assets”, which might include aircraft or satellites, could collect data useful for scientific purposes. Called Medea, the program approved the use of pre-existing satellites to take pictures beginning in 1999 at one-meter resolution of four Arctic sites. Two additional locations were added in 2005. The only catch was that the photographs could not be released until a committee had determined that they were scientifically useful.

For more information, visit
http://www.sciencenews.org/view/generic/id/45557/title/Arctic_images_declassified

About Me

    About

    STUDENTS ON ICE is an award-winning organization offering unique learning expeditions to the Antarctic and the Arctic.

    Our mandate is to provide students from around the world with inspiring educational opportunities at the ends of our earth, and in doing so, help them foster a new understanding and respect for our planet.