Posts tagged sea ice.

sagansense:

NASA Satellites Show How Our Icy World Is Melting

The melt-off from the world’s ice sheets, ice caps and glaciers over eight years of the past decade would have been enough to cover the United States in about 18 inches (46 centimeters) of water, according to new research based on the most-comprehensive analysis of satellite data yet.

Data, collected for the years 2003 through 2010, indicates that melting ice raised sea levels worldwide by an average of 1.48 millimeters (0.06 inches) each year. The loss of ice from Greenland and Antarctica has already been measured using satellite data, but the new analysis revealed that melting ice elsewhere accounted for about 0.41 mm (0.016 inches) of the annual rise.

Until now, satellite measurements from only selected places were used to extrapolate the overall ice loss outside Greenland and Antarctica.

“The Earth is losing an incredible amount of ice to the oceans annually, and these new results will help us answer important questions in terms of both sea rise and how the planet’s cold regions are responding to global change,” study researcher John Wahr, a professor of physics at the University of Colorado, said in a press release issued by the Boulder campus.

Climate change, spurred by greenhouse gases released into the atmosphere by humans, is believed to be the culprit. Warming raises sea levels not only by melting ice — the aspect examined in this study — but  by causing water to expand.

For the first time, the researchers used the satellite system called GRACE (for “Gravity Recovery and Climate Experiment”) to look at loss of ice by glaciers and ice caps around the world.

GRACE, operated by NASA and Germany, already had been used to study ice sheets on Antarctica, Greenland and other large ice-covered areas.

“But so far the data have not been analyzed simultaneously and consistently for all areas,” Jonathan Bamber, of the Glaciology Centre at the University of Bristol in the United Kingdom, wrote in a commentary published along with the study in the Feb. 9 issue of the journal Nature.

The new data confirmed that most of the melting happened on ice-covered Greenland and Antarctica, where enough ice melted to raise sea levels by 1.06 millimeters (0.042 inches)  per year between January 2003 and December 2010, the study period.

There are more than 160,000 glaciers and ice caps worldwide, but annual changes in mass have been directly measured for only 120 of them, and in most cases only within the last 30 years, according to Bamber.

GRACE consists of two satellites that travel around the Earth together, picking up on changes in the Earth’s gravitational field, which are linked to changes in mass. The researchers devised a way to separate out the changes in mass for ice-covered regions around the globe.  

Their results yielded two surprises: The melt rate for glaciers and ice caps outside Antarctica and Greenland made a smaller contribution to sea-level rise than had been estimated, and the melt rate in the Asian mountains, including the Himalayas, was dramatically lower: 4 billion tons annually versus up to 50 billion. 

In his commentary, Bamber notes that the study period was too brief to capture large fluctuations in melting from some areas, such as in the Gulf of Alaska and the high Asian mountains.

“Nonetheless, Jacob and colleagues have dramatically altered our understanding of recent global (glacier and ice cap) volume changes, and their contribution to sea-level rise,” Bamber wrote, referring to study researcher Thomas Jacob of Colorado-Boulder. “Now we need to work out what this means for estimating their future response.”

(via oldowan)

  May 01, 2012 at 05:01pm

mothernaturenetwork:

Arctic sea ice always grows and shrinks with the seasons, reaching its minimum each summer before expanding again in winter. But thanks to global warming, that minimum itself is now shrinking — and at an unprecedented pace. Here’s a graphical look at how quickly this sea change is happening.

saveplanetearth:

Nature ~ Global warming will open Arctic sea routes but sever the region’s ice roads - May 29, 2011: When it comes to Arctic transportation in the coming decades, melting ice will giveth, and melting ice will taketh away.

Melting Ice Roads Could Cause Northern Countries’ Interiors To Become Wilder @ TreeHugger

Margaret Munro @ Vancouver Sun ~ Climate change will reduce access to northern roadways, study says: But less sea ice will open up shipping routes, although not in Northwest Passage

CBC ~ Climate change to ravage Arctic ice roads

Winter roads that provide an important link to Arctic communities and mines will become increasingly inaccessible as the climate warms over the next 40 years, scientists predict.

In Canada, in particular, we project about 400,000 square kilometres of area that … for climatic reasons, will no longer be suitable for winter roads,” said Scott Stephenson, a graduate student in geography at the University of California, Los Angeles, and lead author of the study published this week in Nature Climate Change. (…)

La Presse ~ Arctique: le réchauffement favorisera le trafic maritime: Le réchauffement climatique va grandement favoriser les transports maritimes dans la région arctique, mais aussi ravager les «routes d’hiver» dont dépendent certaines populations et activités locales à l’intérieur des terres, note une étude publiée dimanche.

(via mission-to-mars-deactivated2011)

mohandasgandhi:

other-stuff:

jonathan-cunningham:

cubicmetaphysics:

No Arctic Sea Ice by the 2030s.

According to Kevin Drum, this means that “On current trends, the Arctic will be entirely ice-free in September by about 2016, and will be ice-free year-round by the early 2030s”. If the ice goes by September 2016 and there are still people denying the globe is warming I honestly don’t know how I’ll react.

..

Scientists have been having panic attacks over this because arctic ice has been melting faster than expected.

(via galdikas)

earth-future:

Arctic Sea-Ice Controls the Release of Mercury

A French-American team, including researchers from CNRS, IRD, the Université Paul Sabatier and the Université de Pau (1), has recently highlighted a new role that sea-ice plays in the mercury cycle in the Arctic. By blocking sunlight, sea-ice could influence the breakdown and transfer into the atmosphere of toxic forms of mercury present in the surface waters of the Arctic Ocean. These results, which suggest that climate plays a key role in the mercury cycle and that the release of mercury into the atmosphere could be accentuated by the melting of Arctic sea-ice, are published in the journal Nature Geoscience (February issue).

Mercury (Hg) is the only heavy metal that is essentially found in gaseous form in the atmosphere. Since the industrial revolution, emissions of anthropogenic Hg resulting from the combustion of fossil fuels have exceeded natural emissions. Both anthropogenic emissions and natural emissions (which mainly stem from the oceans and gases released by volcanoes) reach the Polar Regions under the action of atmospheric currents. In this way, fallout from global atmospheric pollution contributes to depositing mercury in Arctic ecosystems, even though these are far away from major anthropogenic emission sources.

In the Arctic atmosphere, elementary mercury is oxidized into a form that deposits easily in the cryosphere (snow, ice). Then, when the ice melts, this oxidized form can in turn be re-mobilized and transformed, via physicochemical and biological processes, into a toxin: methylmercury (CH3Hg). It is this toxic form that is ingested by living organisms. It accumulates throughout the food chain and can reach concentrations one million times higher than those measured in surface waters at the very top of the chain. Over the last two decades, mercury and methylmercury concentration monitoring programs in different regions of the Arctic have been showing contrasting geographic and temporal trends. What are the reasons for these variations? What processes govern the mercury cycle?

To understand these phenomena better, the researchers focused on murre eggs collected in several Arctic and sub-Arctic locations (Gulf of Alaska, Bering Sea and the Chukchi Sea). Situated at the top of the food chain, these sea birds incorporate the mercury contamination present in the chain and are thus an excellent sentinel species for measuring the impact of this pollutant on marine ecosystems. For instance, the quantity of mercury in their eggs provides an accurate reflection of mercury levels in Arctic ecosystems at a given time. More specifically, the team of scientists measured the isotopic signature (2) of Hg in these eggs and noted that it showed significant geographic variations. The isotopic signature variations of most chemical elements (carbon, nitrogen, etc.) mainly depend on their mass difference (12C, 13C).

Surprisingly, mercury isotopes do not follow the same “rule”: its odd isotopes (199Hg, 201Hg) behave differently to its even isotopes (198Hg, 200Hg, etc). This particularity is an extremely rare phenomenon on Earth (3). For mercury, this anomaly is closely related to sea-ice cover around murre colonies’ egg laying sites. Knowing the important role played by light in the photodegradation of methylmercury, the researchers succeeded in establishing how much of this toxin could be destroyed by sunlight, whether in the presence or in the absence of sea-ice. In this way, they determined that the presence of sea-ice prevents both the photochemical breakdown of methylmercury and that it limits exchanges of mercury between the Arctic Ocean and the atmosphere.

These results suggest that climate plays a key role in the mercury cycle. Accelerated melting of sea-ice over the coming decades will therefore influence the biogeochemical cycle of this pollutant in a significant manner. Analysis of mercury at the isotopic scale now opens new research avenues to better understand the dynamics of this priority pollutant and its impact on the environment.

This work was initiated within the framework of the 4th International Polar Year (2007-2009) and benefited from ARN support.

(1) Laboratoire des Mécanismes et des Transferts en Géologie (CNRS/IRD/Université Paul Sabatier Toulouse 3/Observatoire Midi-Pyrénées) and the Institut des Sciences Analytiques et de Physico-Chimie pour l’Environnement et les Matériaux (CNRS/Université de Pau).

(2) This indicates the proportions of the different isotopes of a specific chemical element. It can vary both geographically and as a function of time (as is the case with carbon), and can thus indirectly indicate various parameters.

(3) This phenomenon, known as mass-independent isotopic fractionation, was discovered in the 20th century for two light elements in the natural environment: oxygen and sulfur.

Journal ReferenceD. Point, J. E. Sonke, R. D. Day, D. G. Roseneau, K. A. Hobson, S. S. Vander Pol, A. J. Moors, R. S. Pugh, O. F. X. Donard, P. R. Becker. Methylmercury photodegradation influenced by sea-ice cover in Arctic marine ecosystemsNature Geoscience, 2011; DOI:10.1038/NGEO1049

Source : ScienceDaily

  February 10, 2011 at 05:20am
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