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    Antarctic elevation change from 1992 to 1996 (1998)
    American Association for the Advancement of Science (AAAS)
    Details
    Publication Date: 1998-10-17
    Description: Satellite radar altimeter measurements show that the average elevation of the Antarctic Ice Sheet interior fell by 0.9 +/- 0.5 centimeters per year from 1992 to 1996. If the variability of snowfall observed in Antarctic ice cores is allowed for, the mass imbalance of the interior this century is only -0.06 +/- 0.08 of the mean mass accumulation rate.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Wingham -- Ridout -- Scharroo -- Arthern -- Shum -- New York, N.Y. -- Science. 1998 Oct 16;282(5388):456-8.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉D. J. Wingham, A. J. Ridout, R. J. Arthern, Department of Space and Climate Physics, University College London, 17-19 Gordon Street, London WC1H 0AH, UK. R. Scharroo, Delft Institute for Earth-Oriented Space Research, Delft University of Technology.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/9774268" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
    Published by American Association for the Advancement of Science (AAAS)
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    Crustal dilatation observed by GRACE after the 2004 Sumatra-Andaman earthquake (2006)
    American Association for the Advancement of Science (AAAS)
    Details
    Publication Date: 2006-08-05
    Description: We report the detection of an earthquake by a space-based measurement. The Gravity Recovery and Climate Experiment (GRACE) satellites observed a +/-15-microgalileo gravity change induced by the great December 2004 Sumatra-Andaman earthquake. Coseismic deformation produces sudden changes in the gravity field by vertical displacement of Earth's layered density structure and by changing the densities of the crust and mantle. GRACE's sensitivity to the long spatial wavelength of gravity changes resulted in roughly equal contributions of vertical displacement and dilatation effects in the gravity measurements. The GRACE observations provide evidence of crustal dilatation resulting from an undersea earthquake.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Han, Shin-Chan -- Shum, C K -- Bevis, Michael -- Ji, Chen -- Kuo, Chung-Yen -- New York, N.Y. -- Science. 2006 Aug 4;313(5787):658-62.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Geodetic Science, Department of Geological Sciences, Ohio State University, 275 Mendenhall Laboratory, 125 South Oval Mall, Columbus, OH 43210-1398, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/16888136" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
    Published by American Association for the Advancement of Science (AAAS)
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