Global sea level change signatures observed by GRACE satellite gravimetry
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Ki-Weon Seo | Jianli Chen | Taehwan Jeon | Jianli Chen | K. Seo | C. Wilson | Kookhyoun Youm | Clark R Wilson | T. Jeon | Kookhyoun Youm
[1] Richard M. Bingley,et al. Sea level: measuring the bounding surfaces of the ocean , 2014, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.
[2] Srinivas Bettadpur,et al. High‐resolution CSR GRACE RL05 mascons , 2016 .
[3] Byron D. Tapley,et al. Contribution of ice sheet and mountain glacier melt to recent sea level rise , 2013 .
[4] Don P. Chambers,et al. Evaluation of Release-05 GRACE time-variable gravity coefficients over the ocean , 2012 .
[5] J. Wahr,et al. Computations of the viscoelastic response of a 3-D compressible Earth to surface loading: an application to Glacial Isostatic Adjustment in Antarctica and Canada , 2012 .
[6] Jianli Chen,et al. Ice and groundwater effects on long term polar motion (1979–2010) , 2017 .
[7] Pavel Ditmar,et al. Optimizing estimates of annual variations and trends in geocenter motion and J2 from a combination of GRACE data and geophysical models , 2016 .
[8] Srinivas Bettadpur,et al. The pole tide and its effect on GRACE time‐variable gravity measurements: Implications for estimates of surface mass variations , 2015 .
[9] Eric Rignot,et al. Improved representation of East Antarctic surface mass balance in a regional atmospheric climate model , 2014 .
[10] M. Watkins,et al. Quantifying and reducing leakage errors in the JPL RL05M GRACE mascon solution , 2016 .
[11] H. Dieng,et al. New estimate of the current rate of sea level rise from a sea level budget approach , 2017 .
[12] Kimio Hanawa,et al. Observations: Oceanic Climate Change and Sea Level , 2007 .
[13] Isabella Velicogna,et al. Time‐variable gravity observations of ice sheet mass balance: Precision and limitations of the GRACE satellite data , 2013 .
[14] W. Peltier,et al. Space-geodetic and water level gauge constraints on continental uplift and tilting over North America: regional convergence of the ICE-6G_C (VM5a/VM6) models , 2017 .
[15] Guillaume Ramillien,et al. Sea level budget over 2003-2008: A reevaluation from GRACE space gravimetry, satellite altimetry and Argo , 2009 .
[16] K. Seo,et al. Correlated error reduction in GRACE data over Greenland using extended empirical orthogonal functions , 2017 .
[17] W. R. Peltier,et al. Closure of the budget of global sea level rise over the GRACE era: the importance and magnitudes of the required corrections for global glacial isostatic adjustment , 2009 .
[18] J. Kusche,et al. A new unified approach to determine geocentre motion using space geodetic and GRACE gravity data , 2016 .
[19] D. Chambers,et al. Ocean bottom pressure seasonal cycles and decadal trends from GRACE Release-05: Ocean circulation implications , 2013 .
[20] M. Watkins,et al. Improved methods for observing Earth's time variable mass distribution with GRACE using spherical cap mascons , 2015 .
[21] W. Landman. Climate change 2007: the physical science basis , 2010 .
[22] Duane E. Waliser,et al. Gravity Recovery and Climate Experiment (GRACE) alias error from ocean tides , 2008 .
[23] Armin Köhl,et al. Evaluation of the GECCO2 ocean synthesis: transports of volume, heat and freshwater in the Atlantic , 2015 .
[24] W. Peltier. GLOBAL GLACIAL ISOSTASY AND THE SURFACE OF THE ICE-AGE EARTH: The ICE-5G (VM2) Model and GRACE , 2004 .
[25] A. Cazenave,et al. Sea level budget over 2005–2013: missing contributions and data errors , 2015 .
[26] Archie Paulson,et al. FAST TRACK PAPER: Inference of mantle viscosity from GRACE and relative sea level data , 2007 .
[27] J. Kusche,et al. Passive‐ocean radial basis function approach to improve temporal gravity recovery from GRACE observations , 2017 .
[28] M. Cheng,et al. Deceleration in the Earth's oblateness , 2013 .
[29] Shin-Chan Han,et al. Broadscale postseismic gravity change following the 2011 Tohoku-Oki earthquake and implication for deformation by viscoelastic relaxation and afterslip , 2014, Geophysical research letters.
[30] J. Thepaut,et al. The ERA‐Interim reanalysis: configuration and performance of the data assimilation system , 2011 .
[31] W. Peltier,et al. GRACE era secular trends in Earth rotation parameters: A global scale impact of the global warming process? , 2011 .
[32] Duane E. Waliser,et al. GRACE's spatial aliasing error , 2006 .
[33] J. Willis,et al. Deep-ocean contribution to sea level and energy budget not detectable over the past decade , 2014 .
[34] Jens Schröter,et al. Revisiting the contemporary sea-level budget on global and regional scales , 2016, Proceedings of the National Academy of Sciences.
[35] A. Cazenave,et al. The Sea Level Budget Since 2003: Inference on the Deep Ocean Heat Content , 2015, Surveys in Geophysics.
[36] P. Tregoning,et al. Journal of Geophysical Research: Solid Earth An assessment of the ICE6G_C(VM5a) glacial isostatic adjustment model , 2016 .
[37] W. Tad Pfeffer,et al. Recent contributions of glaciers and ice caps to sea level rise , 2012, Nature.
[38] F. Bryan,et al. Time variability of the Earth's gravity field: Hydrological and oceanic effects and their possible detection using GRACE , 1998 .
[39] J. Mitrovica,et al. Bias in GRACE estimates of ice mass change due to accompanying sea-level change , 2013, Journal of Geodesy.
[40] Low degree gravity changes from GRACE, Earth rotation, geophysical models, and satellite laser ranging , 2008 .
[41] Peter U. Clark,et al. The Sea-Level Fingerprint of West Antarctic Collapse , 2009, Science.
[42] I. Velicogna,et al. Detection of sea level fingerprints derived from GRACE gravity data , 2017 .
[43] D. Chambers,et al. Estimating Geocenter Variations from a Combination of GRACE and Ocean Model Output , 2008 .
[44] Isabella Velicogna,et al. Regional acceleration in ice mass loss from Greenland and Antarctica using GRACE time‐variable gravity data , 2014 .
[45] M. Tamisiea,et al. Recent mass balance of polar ice sheets inferred from patterns of global sea-level change , 2001, Nature.
[46] W. Peltier,et al. Space geodesy constrains ice age terminal deglaciation: The global ICE‐6G_C (VM5a) model , 2015 .