Preliminary observations of global ocean mass variations with GRACE

By D. Chambers, John M. Wahr, R. S. Nerem. 2004

285 citations recorded by the source corpus.

Subfields: Aerospace Engineering, Astronomy and Astrophysics, Oceanography

View Paper: https://www.semanticscholar.org/paper/192127b733c42e1c14c6fb14537102ea2b8d12bd

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Citations in the corpus

Post‐processing removal of correlated errors in GRACE data (2006, background): “…have exploited this relationship to make estimates of water storage variability, both on land and in the oceans [Swenson and Milly, 2006; Ramillien et al., 2005; Chen et al., 2005; Velicogna and Wahr, 2005; Tamisiea et al., 2005; Chambers et al., 2004; Tapley et al., 2004b; Wahr et al., 2004].”
Interannual variations of the mass balance of the Antarctica and Greenland ice sheets from GRACE (2006, methodology): “…spatio-temporal changes in liquid and solid water mass inside the surface fluid envelopes (e.g., Tapley et al., 2004a,b; Wahr et al., 2004; Chambers et al., 2004; Ramillien et al., 2005; Schmidt et al., 2006), including the ice sheets mass change (Velicogna and Wahr, 2005; Velicogna and…”
Estimating geocenter variations from a combination of GRACE and ocean model output (2008, methodology): “To model the eustatic component of global mean sea level, the monthly transport of water between land and ocean is derived from GRACE measurements [Chambers et al., 2004].”
Contemporary sea level rise. (2010, methodology): “GRACE data averaged over the oceans provide a measure of the ocean mass change (e.g., Chambers et al. 2004).”
Closing the sea level rise budget with altimetry, Argo, and GRACE (2009, background): “steric and mass curves has been noted before [Chambers et al., 2004; Chambers, 2006; Chen et al., 2005; Lombard et al., 2007; Willis et al., 2008].”
Low degree spherical harmonic influences on Gravity Recovery and Climate Experiment (GRACE) water storage estimates (2005, methodology): “Chen et al. [2004] showed that degree-2 variations, DC21, DS21, and DC20, estimated from accurately measured Earth rotational (EOP) data, appear to have better accuracy than those derived from GRACE.”
Approximate decorrelation and non-isotropic smoothing of time-variable GRACE-type gravity field models (2007, background): “At sea, they provide the change in ocean water mass, unlike satellite radar altimetry, which cannot distinguish between steric and non-steric sea-level changes (Chambers et al. 2004).”
Antarctic mass rates from GRACE (2006, background): “Of greatest interest are estimates of terrestrial water storage change [e.g., Wahr et al., 2004; Tapley et al., 2004b], snow/ice sheet mass variation in polar regions [e.g., Velicogna and Wahr, 2005], and oceanic mass change [e.g., Chambers et al., 2004].”
Decorrelated GRACE time-variable gravity solutions by GFZ, and their validation using a hydrological model (2009, methodology): “Using data provided by the gravity recovery and climate experiment (GRACE) twin-satellite mission (Tapley et al. 2004b), scientists from various disciplines have been able, for the first time, to observe directly the redistribution of mass in the world’s ocean (e.g., Chambers et al. 2004 ), the mas”
Reducing leakage error in GRACE-observed long-term ice mass change: a case study in West Antarctica (2015, methodology): “…now over a decade in length, provides a means of measuring and tracking mass movement and redistribution in the Earth climate system on a global basis over many time scales (seasonal, inter-annual, and long-term) (e.g., Chambers et al. 2004; Ramillien et al. 2006; Schrama and Wouters 2011).”
Evaluation of Release-05 GRACE time-variable gravity coefficients over the ocean (2012, methodology): “Interactive Discussion D iscssion P aper | D iscssion P aper | D iscssion P aper | D iscssion P aper | the gravity field that is not due to the recent redistribution of water over the Earth’s surface (Chambers et al., 2010). The GRACE coefficients have correlated errors that map into vertical “strip”
GRACE detects coseismic and postseismic deformation from the Sumatra‐Andaman earthquake (2007, methodology): “…within the Earth system, including terrestrial water storage change [e.g., Tapley et al., 2004b; Wahr et al., 2004; Chen et al., 2005a], non-steric sea level change [e.g., Chambers et al., 2004; Chen et al., 2005b], and polar ice sheet melting [e.g., Velicogna and Wahr, 2006; Chen et al., 2006a].”