Evaluation of Release-05 GRACE time-variable gravity coefficients over the ocean

Abstract. The latest release of GRACE (Gravity Recovery and Climate Experiment) gravity field coefficients (Release-05, or RL05) are evaluated for ocean applications. Data have been processed using the current methodology for Release-04 (RL04) coefficients, and have been compared to output from two different ocean models. Results indicate that RL05 data from the three Science Data Centers – the Center for Space Research (CSR), GeoForschungsZentrum (GFZ), and Jet Propulsion Laboratory (JPL) – are more consistent among themselves than the previous RL04 data. Moreover, the variance of residuals with the output of an ocean model is 50–60% lower for RL05 data than for RL04 data. A more optimized destriping algorithm is also tested, which improves the results slightly. By comparing the GRACE maps with two different ocean models, we can better estimate the uncertainty in the RL05 maps. We find the standard error to be about 1 cm (equivalent water thickness) in the low- and mid-latitudes, and between 1.5 and 2 cm in the polar and subpolar oceans, which is comparable to estimated uncertainty for the output from the ocean models.

[1]  R. Kwok,et al.  Recent trends in Arctic Ocean mass distribution revealed by GRACE , 2007 .

[2]  R. Steven Nerem,et al.  Preliminary observations of global ocean mass variations with GRACE , 2004 .

[3]  D. Chambers Evaluation of new GRACE time‐variable gravity data over the ocean , 2006 .

[4]  Low-frequency exchange of mass between ocean basins , 2009 .

[5]  A basin‐coherent mode of sub‐monthly variability in Arctic Ocean bottom pressure , 2011 .

[6]  R. Ponte,et al.  Bottom pressure changes around Antarctica and wind‐driven meridional flows , 2009 .

[7]  R. Ponte,et al.  Estimating high frequency ocean bottom pressure variability , 2011 .

[8]  J. Schröter,et al.  Antarctic Circumpolar Current Transport Variability in GRACE Gravity Solutions and Numerical Ocean Model Simulations , 2010 .

[9]  Grzegorz Michalak,et al.  GFZ GRACE Level-2 Processing Standards Document for Level-2 Product Release 0005 : revised edition, January 2013 , 2013 .

[10]  M. Cheng,et al.  Variations in the Earth's oblateness during the past 28 years , 2004 .

[11]  H. Dobslaw,et al.  Short‐term transport variability of the Antarctic Circumpolar Current from satellite gravity observations , 2012 .

[12]  C. Wunsch,et al.  A comparison of model and GRACE estimates of the large‐scale seasonal cycle in ocean bottom pressure , 2007 .

[13]  D. Chambers,et al.  Estimating Geocenter Variations from a Combination of GRACE and Ocean Model Output , 2008 .

[14]  Ichiro Fukumori,et al.  Mechanisms Controlling the Interannual Variation of Mixed Layer Temperature Averaged over the Niño-3 Region , 2007 .

[15]  Uncertainty in ocean mass trends from GRACE , 2010 .

[16]  Jens Schröter,et al.  Measuring ocean mass variability from satellite gravimetry , 2011 .

[17]  Archie Paulson,et al.  FAST TRACK PAPER: Inference of mantle viscosity from GRACE and relative sea level data , 2007 .

[18]  R. Ponte,et al.  High frequency barotropic ocean variability observed by GRACE and satellite altimetry , 2012 .

[19]  V. Zlotnicki,et al.  Subpolar ocean bottom pressure oscillation and its links to the tropical ENSO , 2008 .

[20]  I. Fukumori,et al.  Antarctic Circumpolar Current Transport Variability during 2003–05 from GRACE , 2007 .

[21]  L. Perelman,et al.  A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers , 1997 .

[22]  Tong Lee,et al.  A record‐high ocean bottom pressure in the South Pacific observed by GRACE , 2011 .

[23]  R. Steven Nerem,et al.  Ocean mass from GRACE and glacial isostatic adjustment , 2010 .

[24]  ENSO-correlated fluctuations in ocean bottom pressure and wind-stress curl in the North Pacific , 2011 .

[25]  Don P. Chambers,et al.  A Global Evaluation of Ocean Bottom Pressure from GRACE, OMCT, and Steric-Corrected Altimetry , 2010 .

[26]  J. Willis,et al.  Analysis of large-scale ocean bottom pressure variability in the North Pacific , 2008 .

[27]  Ichiro Fukumori,et al.  A Partitioned Kalman Filter and Smoother , 2002 .

[28]  D. Chambers,et al.  Evaluation of high‐frequency oceanographic signal in GRACE data: Implications for de‐aliasing , 2011 .

[29]  S. Jayne,et al.  A comparison of in situ bottom pressure array measurements with GRACE estimates in the Kuroshio Extension , 2008 .

[30]  F. Bryan,et al.  Time variability of the Earth's gravity field: Hydrological and oceanic effects and their possible detection using GRACE , 1998 .

[31]  S. Swenson,et al.  Post‐processing removal of correlated errors in GRACE data , 2006 .