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Mass loss of the Greenland ice sheet from GRACE time-variable gravity measurements

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Abstract

The Gravity Recovery and Climate Experiment (GRACE) satellite data is used to estimate the rate of ice mass variability over Greenland. To do this, monthly GRACE level 2 Release-04 (RL04) data from three different processing centers, Center for Space Research (CSR), German Research Center for Geosciences (GFZ) and Jet Propulsion Laboratories (JPL) were used during the period April 2002 to February 2010. It should be noted that some months are missing for all three data sets. Results of computations provide a mass decrease of −163 ± 20 Gigaton per year (Gt/yr) based on CSR-RL04 data, −161 ± 21 Gt/yr based on GFZ-RL04 data and −84 ± 26 Gt/yr based on JPL RL04.1. The results are derived by the application of a non-isotropic filter whose degree of smoothing corresponds to a Gaussian filter with a radius of 340 km. Striping effects in the GRACE data, C20 effect, and leakage effects are taken into the consideration in the computations. There is some significant spread of the results among different processing centers of GRACE solutions; however, estimates achieved in this study are in agreement with the results obtained from alternative GRACE solutions.

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References

  • Akaike H., 1973. Information theory and an extension of maximum likelihood principle. In: Petrov B.N. and Csáki F. (Eds.), 2nd International Symposium on Information Theory. Akadémiai Kaidó, Budapest, Hungary, 267–281.

    Google Scholar 

  • Baur O., Kuhn M. and Featherstone W.E., 2009a. GRACE-derived ice-mass variations over Greenland by accounting for leakage effects. J. Geophys. Res., 114, B06407, DOI: 10.1029/2008JB006239.

    Article  Google Scholar 

  • Baur O., Kuhn M. and Featherstone W.E., 2009b. GRACE-Derived Linear and Non-Linear Secular Mass Variations over Greenland. Publication No. 213, The Institute for Geoscience Research (TIGeR), Curtin University of Technology, Australia.

    Google Scholar 

  • Bettadpur S., 2007. CSR Level-2 Processing Standards Document for Product Release 04. Report GRACE 327-742. Center for Space Research, University of Texas at Austin, Austin, TX.

    Google Scholar 

  • Chambers D.P., 2007. Effects of ice melting on GRACE observations of ocean mass trends. Geophys. Res. Lett., 34, L05610, DOI: 10.1029/2006GL029171.

    Article  Google Scholar 

  • Chambers D.P., 2009. Calculating trends from GRACE in the presence of large changes in continental ice storage and ocean mass. Geophys. J. Int., 176, 415–419, DOI: 10.1111/j.1365-246X.2008.04012.x.

    Article  Google Scholar 

  • Chen J.L., Wilson C.R. and Tapley B.D., 2006. Satellite gravity measurements confirm accelerated melting of Greenland ice sheet. Science, 313, 1958–1960, DOI: 10.1029/science.1129007.

    Article  Google Scholar 

  • Chen J.L., Wilson C.R., Famiglietti J.S. and Rodell M., 2005. Spatial sensitivity of the Gravity Recovery and Climate Experiment (GRACE) time-variable gravity observations. J. Geophys. Res., 110, B08408, DOI: 10.1029/2004JB003536.

    Article  Google Scholar 

  • Hanna E.P., Cappelen X., Fettweis P., Huybrechts P., Luckman A. and Ribergaard M., 2009. Hydrologic response of the Greenland ice sheet: The role of oceanographic warming. Hydrol. Process., 23, 7–30, DOI: 10.1002/hyp.7090.

    Article  Google Scholar 

  • Kusche J., 2007. Approximate decorrelation and non-isotropic smoothing of time-variable GRACE-type gravity fields. J. Geodesy, 81, 733–749.

    Article  Google Scholar 

  • Kusche J., Schmidt R., Petrovic S. and Rietbroek R., 2009. Decorrelated GRACE time-variable gravity solutions by GFZ, and their validation using a hydrological model. J. Geodesy, 83, 903–913.

    Article  Google Scholar 

  • Luthcke S.B., Zwally H.J., Abdalati W., Rowlands D.D., Ray R.D., Nerem R.S., Lemoine F.G., McCarthy J.J. and Chinn D.S., 2006. Recent Greenland ice mass loss by drainage system from satellite gravity observations. Science, 314, 1286–1289, DOI: 10.1126/Science.1130776.

    Article  Google Scholar 

  • Ramillien G., Lombard A., Cazenave A., Ivins E.R., Llubes M., Remy F. and Biancale R., 2006. Interannual variations of the mass balance of the Antarctica and Greenland ice sheets from GRACE. Glob. Planet. Change, 53, 198–208, DOI: 10.1016/j.gloplacha.

    Article  Google Scholar 

  • Rodell M., Houser P.R., Jambor U., Gottschalck J., Mitchell K., Meng C.-J., Arsenault K., Cosgrove B., Radakovich J., Bosilovich M., Entin J.K., Walker J.P., Lohmann D. and Toll D., 2004a. The global land data assimilation system. Bull. Amer. Meteorol. Soc., 85, 381–394.

    Article  Google Scholar 

  • Rodell M., Famiglietti J.S., Chen J.L., Seneviratne S.I., Viterbo P., Holl S. and Wilson C.R., 2004b. Basin scale estimates of evapotranspiration using GRACE and other observations. Geophys. Res. Lett., 31, L20504, DOI: 10.1029/2004GL020873.

    Article  Google Scholar 

  • Sandberg Sørensen L.S. and Forsberg R., 2010. Greenland ice sheet mass loss from GRACE monthly models. In: Mertikas S.P. (Ed.), Gravity, Geoid and Earth Observation. International Association of Geodesy Symposia 135, 527–532, Springer-Verlag, Berlin, Heidelberg, Germany, DOI: 10.1007/978-3-642-10634-7_70.

    Chapter  Google Scholar 

  • Solomon S., Qin D., Manning M., Chen Z., Marquis M., Averyt K.B., Tignor M. and Miller H.L., 2007. Climate Change 2007 — The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the IPCC. Cambridge University Press, Cambridge, U.K.

    Google Scholar 

  • Swenson S. and Wahr J, 2002. Methods for inferring regional surface-mass anomalies from Gravity Recovery and Climate Experiment (GRACE) measurements time-variable gravity. J. Geophys. Res., 107, B92193, DOI:10.1029/2001JB000576.

    Google Scholar 

  • Swenson S., Wahr J. and Milly P.C.D., 2003. Estimated accuracies of regional water storage variations inferred from the Gravity Recovery and Climate Experiment (GRACE). Water Resour. Res., 39, 1223, DOI: 10.1029/2002WR001808.

    Article  Google Scholar 

  • Tapley B.D., Bettadpur S., Watkins M.M. and Reigber C., 2004a. The Gravity Recovery and Climate Experiment: Mission overview and early results. Geophys. Res. Lett., 31, L09607, DOI: 10.1029/2004GL019920.

    Article  Google Scholar 

  • Tapley B.D., Bettadpur S., Ries J.C., Thompson P.F. and Watkins M.M., 2004b. GRACE measurements of mass variability in the Earth system. Science, 305, 503–505.

    Article  Google Scholar 

  • Velicogna I., 2009. Increasing rates of ice mass loss from the Greenland and Antarctic ice sheets revealed by GRACE. Geophys. Res. Lett., 36, L19503, DOI: 10.1029/2009GL040222.

    Article  Google Scholar 

  • Veliconga I. and Wahr J., 2005. Greenland mass balance from GRACE. Geophys. Res. Lett., 32, L18505, DOI: 10.1029/2005GL023955.

    Article  Google Scholar 

  • Velicogna I. and Wahr J., 2006a. Acceleration of Greenland ice mass loss in spring 2004. Nature, 443, 329–331.

    Article  Google Scholar 

  • Velicogna I. and Wahr J., 2006b. Measurements of time-variable gravity show mass loss in Antarctica. Science, 311, 1754–1756, DOI: 10.1126/science. 1123785.

    Article  Google Scholar 

  • Wahr J., Molenaar M. and Bryan F., 1998. Time variability of the Earth’s gravity field: Hydrological and oceanic effects and their possible detection using GRACE. J. Geophys. Res., 103(B12), 30205–30229.

    Article  Google Scholar 

  • Wahr J., Swenson S., Zlotnicki V. and Velicogana I., 2004. Time-variable gravity from GRACE: First results. Geophys. Res. Lett., 31, L11501, DOI: 10.1029/2004GL019779.

    Article  Google Scholar 

  • Wouters B., Chambers D.P. and Schrama E.J.O., 2008. GRACE observes small-scale mass loss in Greenland. Geophys. Res. Lett., 35, L20501, DOI: 10.1029/2008GL034816.

    Article  Google Scholar 

  • Yamamoto K., Fukuda Y., Doi K. and Motoyama H., 2008. Interpretation of the GRACE-derived mass trend in Enderby Land, Antarctica. Polar Sci., 2, 267–276, DOI: 10.1016 /j.polar.2008.10.001.

    Article  Google Scholar 

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Authors and Affiliations

  1. Division of Geomatics, Norwegian University of Science and Technology, N-7491, Trondheim, Norway

    Gholamreza Joodaki & Hossein Nahavandchi

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  1. Gholamreza Joodaki
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  2. Hossein Nahavandchi
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Correspondence to Gholamreza Joodaki.

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Joodaki, G., Nahavandchi, H. Mass loss of the Greenland ice sheet from GRACE time-variable gravity measurements. Stud Geophys Geod 56, 197–214 (2012). https://doi.org/10.1007/s11200-010-0091-x

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  • DOI: https://doi.org/10.1007/s11200-010-0091-x

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