PUBLIC INFORMATION OFFICE JET PROPULSION LABORATORY CALIFORNIA INSTITUTE OF TECHNOLOGY NATIONAL AERONAUTICS AND SPACE ADMINISTRATION PASADENA, CALIFORNIA 91109. TELEPHONE (818) 354-5011 http://www.jpl.nasa.gov IMAGE CAPTION P-49411 December 8, 1997 Seasat/NSCAT These three radar images show a comparison of measurements of the Greenland ice sheet made by the Seasat Scatterometer (SASS) with those of the NASA Scatterometer (NSCAT) made after an 18 year time interval. The image on the left was created from data acquired by NSCAT in September 1996, while the image in the middle was generated from Seasat data recorded during the same season in 1978. The image on the right shows the difference between the first two images and thus changes occurring on the ice sheet in the 18 year gap between the two satellite missions. In the right hand difference image, the red and white patches in the center indicate areas of significant change. In particular, they signify shrinkage of the area covered by dry snow, due to the effects of increased summer melting. The dry-snow zone is the high-altitude portion of the Greenland ice cap which normally experiences no summer melting. In the images on the left and in the middle, the red areas are the ice zones which normally experience some melting; the blue areas at the coastlines are exposed rock; the yellow and white areas in central Greenland are the dry snow zone; and the light-blue areas are where annual snow accumulation is at its greatest. The pattern of changes seen in the comparison of the NSCAT and Seasat images are consistent with a 10-year warming trend. An increase of more than 1.0 degree C (33.8 degrees F) took place between 1979 and the present day, except for the summer of 1992 when ash from the Mt. Pinatubo eruption may have temporarily helped to cool the northern hemisphere. #####