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  • 1
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    In:  Phys. Earth Plan. Int., Luxembourg, Conseil de l'Europe, vol. 102, no. 1-2, pp. 33-50, pp. B05S07, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1997
    Keywords: Anisotropy ; earth mantle ; Rheology ; Gravimetry, Gravitation ; Isostasy ; PEPI
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  • 2
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    In:  Geophys. J. Int., Luxembourg, Conseil de l'Europe, vol. 120, no. 1-2, pp. 287-311, pp. B05S07, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1995
    Keywords: Earth tides ; Rheology ; Layers ; Inelastic ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; GJI
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  • 3
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    In:  J. Geophys. Res., Leipzig, Akad. Nauk SSSR, vol. 85, no. B1, pp. 6471-6477, pp. B01308, (ISSN: 1340-4202)
    Publication Date: 1980
    Keywords: Earthquake ; Inelastic ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Finite Element Method ; JGR
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  • 4
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    In:  Eos, Trans., Am. Geophys. Un., Luxembourg, Conseil de l'Europe, vol. 81, no. 37, pp. 421, 426 & 427, pp. L12309, (ISSN: 1340-4202)
    Publication Date: 2000
    Keywords: Gravimetry, Gravitation ; Geodesy ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; climate ; glaciers
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  • 5
    Publication Date: 2011-11-04
    Description: Models are routinely used to remove the effects of global ocean tides from GRACE data during processing to reduce temporal aliasing into monthly GRACE solutions. These models have typically been derived using data from satellite altimeters such as TOPEX/Poseidon. Therefore the Arctic ocean components of tide models are not constrained by altimetry data, potentially resulting in errors that are likely to alias into monthly GRACE gravity fields at all latitudes. Seven years of GRACE inter-satellite accelerations are inverted to solve for corrections to the amplitude and phase of major solar and lunar ocean tides at latitudes north of 50°N using a mascon approach. The tide model originally applied to our data was FES2004, truncated to maximum degree lmax = 90. Simulations are performed to verify that our inversion algorithm works as designed. Uncertainty estimates are derived from tidal solutions on land, and by subtracting two independent solutions that each use 3.5 years of data. Features above the noise floor in the M2, K1, S2, and O1 solutions likely represent errors in FES2004. Errors due to truncating the spherical harmonic expansion of FES2004 are too small, and errors in the land mask model (needed to transform sea surface heights into mass) only affect coastal areas and do not produce similar relative amplitudes for any examined tides. In the oceans north of 50°N, these residuals tend to reduce the FES2004 amplitudes for M2, K1, S2, and O1. Reductions in the variance of accelerations not used in our inversion suggest that our results can be used to improve GRACE processing.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 6
    Publication Date: 2011-07-13
    Description: We use temporal gravity variations from GRACE to investigate changes in a 34-year time series of Earth's oblateness (J2) observed by satellite laser ranging (SLR). We use 2002–2010 GRACE data to compute the effects of Greenland and Antarctic ice mass variations on J2 (2.0 and 1.7 × 10−11/year respectively). Their combined effect on the J2 trend during the GRACE mission is 3.7 × 10−11/year, which agrees well with the GIA-corrected SLR J2 trend over the same time period. The results suggest that at least since 2002, ice loss from Greenland and Antarctica has been the dominant contributor to the current GIA-corrected J2 trend, which apparently began sometime in the 1990s.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 7
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 2006-03-04
    Description: Using measurements of time-variable gravity from the Gravity Recovery and Climate Experiment satellites, we determined mass variations of the Antarctic ice sheet during 2002-2005. We found that the mass of the ice sheet decreased significantly, at a rate of 152 +/- 80 cubic kilometers of ice per year, which is equivalent to 0.4 +/- 0.2 millimeters of global sea-level rise per year. Most of this mass loss came from the West Antarctic Ice Sheet.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Velicogna, Isabella -- Wahr, John -- New York, N.Y. -- Science. 2006 Mar 24;311(5768):1754-6. Epub 2006 Mar 2.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉University of Colorado, Cooperative Institute for Research in Environmental Sciences and Department of Physics, University Campus Box 390, Boulder, CO 80309-0390, USA. isabella@colorado.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/16513944" 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
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  • 8
    Publication Date: 2012-12-01
    Description: We combined an ensemble of satellite altimetry, interferometry, and gravimetry data sets using common geographical regions, time intervals, and models of surface mass balance and glacial isostatic adjustment to estimate the mass balance of Earth's polar ice sheets. We find that there is good agreement between different satellite methods--especially in Greenland and West Antarctica--and that combining satellite data sets leads to greater certainty. Between 1992 and 2011, the ice sheets of Greenland, East Antarctica, West Antarctica, and the Antarctic Peninsula changed in mass by -142 +/- 49, +14 +/- 43, -65 +/- 26, and -20 +/- 14 gigatonnes year(-1), respectively. Since 1992, the polar ice sheets have contributed, on average, 0.59 +/- 0.20 millimeter year(-1) to the rate of global sea-level rise.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Shepherd, Andrew -- Ivins, Erik R -- A, Geruo -- Barletta, Valentina R -- Bentley, Mike J -- Bettadpur, Srinivas -- Briggs, Kate H -- Bromwich, David H -- Forsberg, Rene -- Galin, Natalia -- Horwath, Martin -- Jacobs, Stan -- Joughin, Ian -- King, Matt A -- Lenaerts, Jan T M -- Li, Jilu -- Ligtenberg, Stefan R M -- Luckman, Adrian -- Luthcke, Scott B -- McMillan, Malcolm -- Meister, Rakia -- Milne, Glenn -- Mouginot, Jeremie -- Muir, Alan -- Nicolas, Julien P -- Paden, John -- Payne, Antony J -- Pritchard, Hamish -- Rignot, Eric -- Rott, Helmut -- Sorensen, Louise Sandberg -- Scambos, Ted A -- Scheuchl, Bernd -- Schrama, Ernst J O -- Smith, Ben -- Sundal, Aud V -- van Angelen, Jan H -- van de Berg, Willem J -- van den Broeke, Michiel R -- Vaughan, David G -- Velicogna, Isabella -- Wahr, John -- Whitehouse, Pippa L -- Wingham, Duncan J -- Yi, Donghui -- Young, Duncan -- Zwally, H Jay -- New York, N.Y. -- Science. 2012 Nov 30;338(6111):1183-9. doi: 10.1126/science.1228102.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK. ashepherd@leeds.ac.uk〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23197528" target="_blank"〉PubMed〈/a〉
    Keywords: Antarctic Regions ; *Climate Change ; Geographic Information Systems ; Greenland ; *Ice Cover
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 9
    Publication Date: 2013-05-21
    Description: Glaciers distinct from the Greenland and Antarctic Ice Sheets are losing large amounts of water to the world's oceans. However, estimates of their contribution to sea level rise disagree. We provide a consensus estimate by standardizing existing, and creating new, mass-budget estimates from satellite gravimetry and altimetry and from local glaciological records. In many regions, local measurements are more negative than satellite-based estimates. All regions lost mass during 2003-2009, with the largest losses from Arctic Canada, Alaska, coastal Greenland, the southern Andes, and high-mountain Asia, but there was little loss from glaciers in Antarctica. Over this period, the global mass budget was -259 +/- 28 gigatons per year, equivalent to the combined loss from both ice sheets and accounting for 29 +/- 13% of the observed sea level rise.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Gardner, Alex S -- Moholdt, Geir -- Cogley, J Graham -- Wouters, Bert -- Arendt, Anthony A -- Wahr, John -- Berthier, Etienne -- Hock, Regine -- Pfeffer, W Tad -- Kaser, Georg -- Ligtenberg, Stefan R M -- Bolch, Tobias -- Sharp, Martin J -- Hagen, Jon Ove -- van den Broeke, Michiel R -- Paul, Frank -- New York, N.Y. -- Science. 2013 May 17;340(6134):852-7. doi: 10.1126/science.1234532.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Graduate School of Geography, Clark University, Worcester, MA 01610, USA. agardner@clarku.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23687045" target="_blank"〉PubMed〈/a〉
    Keywords: Arctic Regions ; Greenland ; *Ice Cover ; *Seawater
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 10
    Publication Date: 2012-02-10
    Description: Glaciers and ice caps (GICs) are important contributors to present-day global mean sea level rise. Most previous global mass balance estimates for GICs rely on extrapolation of sparse mass balance measurements representing only a small fraction of the GIC area, leaving their overall contribution to sea level rise unclear. Here we show that GICs, excluding the Greenland and Antarctic peripheral GICs, lost mass at a rate of 148 +/- 30 Gt yr(-1) from January 2003 to December 2010, contributing 0.41 +/- 0.08 mm yr(-1) to sea level rise. Our results are based on a global, simultaneous inversion of monthly GRACE-derived satellite gravity fields, from which we calculate the mass change over all ice-covered regions greater in area than 100 km(2). The GIC rate for 2003-2010 is about 30 per cent smaller than the previous mass balance estimate that most closely matches our study period. The high mountains of Asia, in particular, show a mass loss of only 4 +/- 20 Gt yr(-1) for 2003-2010, compared with 47-55 Gt yr(-1) in previously published estimates. For completeness, we also estimate that the Greenland and Antarctic ice sheets, including their peripheral GICs, contributed 1.06 +/- 0.19 mm yr(-1) to sea level rise over the same time period. The total contribution to sea level rise from all ice-covered regions is thus 1.48 +/- 0.26 mm (-1), which agrees well with independent estimates of sea level rise originating from land ice loss and other terrestrial sources.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Jacob, Thomas -- Wahr, John -- Pfeffer, W Tad -- Swenson, Sean -- England -- Nature. 2012 Feb 8;482(7386):514-8. doi: 10.1038/nature10847.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Physics and Cooperative Institute for Environmental Studies, University of Colorado at Boulder, Boulder, Colorado 80309, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/22318519" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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