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Wednesday, July 8, 2009

NASA's JPL ICESat Supplementary Data, Kwok et al.

Sorry readers -- click on the images to see the full image, or click on the link at the end of each figure legend.

New NASA Satellite Survey Reveals Dramatic Arctic Sea Ice Thinning -- 07.07.09
Link here: http://www.nasa.gov/topics/earth/features/icesat-20090707.html

Arctic sea ice thinned dramatically between the winters of 2004 and 2008, with thin seasonal ice replacing thick older ice as the dominant type for the first time on record. The new results, based on data from a NASA Earth-orbiting spacecraft, provide further evidence for the rapid, ongoing transformation of the Arctic's ice cover.

Scientists from NASA and the University of Washington in Seattle conducted the most comprehensive survey to date using observations from NASA's Ice, Cloud and land Elevation Satellite, known as ICESat, to make the first basin-wide estimate of the thickness and volume of the Arctic Ocean's ice cover. Ron Kwok of NASA's Jet Propulsion Laboratory in Pasadena, Calif., led the research team, which published its findings July 7, 2009, in the Journal of Geophysical Research-Oceans.

Below are images related to the release:
http://www.nasa.gov/images/content/324864main_kwokfig1_full.jpg
Figure 1: ICESat measures the distances to the top of the snow cover and to the sea surface. The difference between the two quantities gives the total “freeboard” measurement; that is, the amount of ice above the water line relative to the local sea level. Credit: Courtesy of Norbert Untersteiner, University of Washington. Link to full page image: http://www.nasa.gov/images/content/324864main_kwokfig1_full.jpg

http://www.nasa.gov/images/content/365867main_earth1-20090707-full.jpg
Figure 2: This schematic shows the geometric relationship between freeboard (the amount of ice above the water line), snow depth, and ice thickness. Buoyancy causes a fraction (about 10 percent) of sea ice to stick out above the sea surface. By knowing the density of the ice and applying “Archimedes’ Principle” -- an object immersed in a fluid is buoyed up by a force equal to the weight of the fluid displaced by the object -- the total thickness of the ice can be calculated. Credit: Ron Kwok, NASA/JPL. Link to full page image: http://www.nasa.gov/images/content/365867main_earth1-20090707-full.jpg


http://www.nasa.gov/images/content/365869main_earth2-20090707-full.jpg
Figure 3: ICESat measurements of the distribution of winter sea ice thickness over the Arctic Ocean between 2004 and 2008, along with the corresponding trends in overall, multi-year and first-year winter ice thickness. Credit: Ron Kwok, NASA/JPL. > Larger image

http://www.nasa.gov/images/content/365871main_earth3-20090707-full.jpg
Figure 4: ICESat measurements of winter multi-year ice cover in the Arctic Ocean between 2004 and 2008, along with the corresponding downward trend in overall winter sea ice volume, and switch in dominant ice type from multi-year ice to first-year ice. Credit: Ron Kwok, NASA/JPL. > Larger image

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