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IARC scientists document warm water surging into Arctic
September 27, 2006
Scientists at the University of Alaska Fairbanks International Arctic Research Center this fall documented that recent surges of warm water from the North Atlantic Ocean continue to pulse into the Arctic Ocean and are moving toward Alaska and the Canadian Basin. Scientists made the observations this fall during an oceanographic cruise aboard the Russian icebreaker Kapitan Dranitsyn as part of the Nansen and Amundsen Basins Observational Systems program. Information gathered by the NABOS program, as well as from other international programs, has shown that, during the last decade, the movement of warm water into the Arctic Ocean has increased. And the readings from this fall's cruise show unprecedented warmth in some areas. "The large area of the Arctic Ocean promises to become much warmer," said Igor Polyakov, NABOS principal investigator and a research professor at IARC. The readings come from observational moorings, which are instrument-bearing buoys that are anchored to the ocean floor and float below the surface of the ocean. These instruments first detected a surge of anomalous warm water, at mid-ocean depths of about 150 to 800 meters below the surface, in February of 2004 on the continental slope of the Laptev Sea, Polyakov said. "What we found this year was one of our eastern moorings also showed a warming signal." That finding indicates that the warm water is moving further and further into the Arctic, he said, which could increase the overall temperature of the Arctic Ocean. While the causes of the influx of warm water will require further study, the observations from the NABOS project suggest that the Arctic Ocean is moving toward a warmer state, a change that could have global implications. Ocean temperature in the Arctic is important because it may affect the amount of sea ice in the region. Scientists believe that arctic sea ice cover plays a major role in the global climate, as ice reflects more of the sun's heat than open water. The NABOS project is funded by the National Oceanic and Atmospheric Administration and the National Science Foundation and is a collaboration among six nations. It is one of many UAF projects that will contribute to the international efforts of the upcoming International Polar Year. IPY is a two-year event, slated to begin in March 2007, which will focus research efforts and public attention on the Earth's polar regions. UAF is among a handful of institutions worldwide that is ideally situated to participate in IPY research, education and outreach. University of Alaska Fairbanks Related Arctic Ocean Current Events and Arctic Ocean News ArticlesSunlit Snow Triggers Atmospheric Cleaning, Ozone Depletion in the ArcticNational Science Foundation-funded researchers at Purdue University have discovered that sunlit snow is the major source of atmospheric bromine in the Arctic, the key to unique chemical reactions that purge pollutants and destroy ozone. Pioneering study calculates Arctic Ocean nutrient budgetThe first study of its kind to calculate the amount of nutrients entering and leaving the Arctic Ocean has been carried out by scientists based at the National Oceanography Centre, Southampton. 2013 Wintertime Arctic Sea Ice Maximum Fifth Lowest on RecordLast September, at the end of the northern hemisphere summer, the Arctic Ocean's icy cover shrank to its lowest extent on record, continuing a long-term trend and diminishing to about half the size of the average summertime extent from 1979 to 2000. Amplified greenhouse effect shaping North into SouthAn international team of 21 authors from 17 institutions in seven countries has just published a study in the journal Natural Climate Change showing that, as the cover of snow and ice in the northern latitudes has diminished in recent years, the temperature over the northern land mass has increased at different rates during the four seasons, causing a reduction in temperature and vegetation seasonality in this area. Amplified Greenhouse Effect Shifts North's Growing SeasonsVegetation growth at Earth's northern latitudes increasingly resembles lusher latitudes to the south, according to a NASA-funded study based on a 30-year record of land surface and newly improved satellite data sets. Melt ponds cause the Artic sea ice to melt more rapidly The Arctic sea ice has not only declined over the past decade but has also become distinctly thinner and younger. Mathematics and weather and climate researchHow does mathematics improve our understanding of weather and climate? Can mathematicians determine whether an extreme meteorological event is an anomaly or part of a general trend? Mercury releases contaminate ocean fish: Dartmouth-led effort publishes major findingsIn new research published in a special issue of the journal Environmental Research and in "Sources to Seafood: Mercury Pollution in the Marine Environment"- a companion report by the Dartmouth-led Coastal and Marine Mercury Ecosystem Research Collaborative (C-MERC), scientists report that mercury released into the air and then deposited into oceans contaminates seafood commonly eaten by people in the U.S. and globally. Ocean currents play a role in predicting extent of Arctic sea ice Each winter, wide swaths of the Arctic Ocean freeze to form sheets of sea ice that spread over millions of square miles. This ice acts as a massive sun visor for the Earth, reflecting solar radiation and shielding the planet from excessive warming. Why Antarctic sea ice cover has increased under the effects of climate changeThe first direct evidence that marked changes to Antarctic sea ice drift have occurred over the last 20 years, in response to changing winds, is published this week in the journal Nature Geoscience. Scientists from NERC's British Antarctic Survey (BAS) and NASA's Jet Propulsion Laboratory (JPL), Pasadena California explain why, unlike the dramatic losses reported in the Arctic, the Antarctic sea ice cover has increased under the effects of climate change. More Arctic Ocean Current Events and Arctic Ocean News Articles

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