Modeling the barotropic response of the global ocean to atmospheric wind and pressure forcing ‐ comparisons with observations

By L. Carrère, F. Lyard. 2003

682 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/7e4c50526472dbb697d8480a7658096d8e89cf62

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In Global and Planetary Change

In Oceanography

Citations in the corpus

Concurrent Simulation of the Eddying General Circulation and Tides in a Global Ocean Model (2010, neutral): “In recent years, it has been shown that achieving accurate surface elevations in forward global barotropic tide models requires the insertion of a parameterization of drag (and energy loss) due to the breaking of internal waves generated by tidal flow over rough topography (Jayne and St. Laurent, 20”
Recent advances in observing mesoscale ocean dynamics with satellite altimetry (2012, background): “Errors are reduced when 10-day averages are made, but also when a high-frequency, low-wavenumber dynamic atmospheric correction is applied, such as MOG2D (Carrere and Lyard, 2003).”
Modeling deformation induced by seasonal variations of continental water in the Himalaya region: Sensitivity to Earth elastic structure (2011, neutral): “5100 2003 2004 2005 2006 2007 2008 2009 2010 2011 2012 −500 −400 −300 −200 −100 0 100 200 300 400 500 Year E qu iv al en t W at er H ei gh t ( m m ) A B and wind on ocean: Mog-2D [Carrère and Lyard, 2003], provided by the European Centre for Medium-Range Weather Forecasts.”
Precision Orbit Determination Standards for the Jason Series of Altimeter Missions (2010, background): “…Klinker et al. 2000), the Toulouse Unstructured Grid Ocean model (T-UGO, or MOG-2D Follow-on), to model the barotropic oceanic mass variations (Carrère and Lyard 2003), and the GLDAS/Noah land-surface model to describe the terrestrial water storage variations Jason-1 and Jason-2 POD…”
The accuracy of surface elevations in forward global barotropic and baroclinic tide models (2004, result): “In agreement with other recent studies of global forward tide models (Jayne and St. Laurent, 2001—hereafter JS; Carrere and Lyard, 2003— hereafter CL; Egbert et al., 2004—hereafter ERB), we argue that topographic drag is a plausible mechanism for mid-ocean tidal dissipation.”
Detection of Continental Hydrology and Glaciology Signals from GRACE: A Review (2008, methodology): “In the process, GRACE coefficients are corrected for atmospheric mass variations and ocean tides using ECMWF and NCEP reanalyses respectively, as well as and global oceanic circulation models such as MOG-2D (Carrère and Lyard 2003).”
EOT11A - Empirical Ocean Tide Model from Multi-Mission Satellite Altimetry (2008, neutral): “…On the radiational anomaly in the global ocean tide with reference to satellite altimetry, Oceanologica Acta, 1994, 17,5,453-459 Carrère, L., and F. Lyard (2003), Modeling the barotropic response of the global ocean to atmospheric wind and pressure forcing—comparisons with observations, Geophys.”
The Impact of Abyssal Mixing Parameterizations in an Ocean General Circulation Model (2009, background): “Other parameterizations in place of equation (4) for the internal wave conversion have been suggested (Carrère and Lyard 2003; Arbic et al. 2004; Egbert et al. 2004), however it was found that any of these schemes gave comparable accuracies in the simulated tidal elevations once they were tuned (Egb”
The GeoForschungsZentrum Potsdam/Groupe de Recherche de Gèodésie Spatiale satellite-only and combined gravity field models: EIGEN-GL04S1 and EIGEN-GL04C (2008, methodology): “…derived at GRGS Toulouse from LAGEOS, GRACE and the combination of both satellites for a time span of mass variations was based on the barotropic MOG2D model (Carrère and Lyard 2003), but the difference when using the baroclinic model OMCT (GFZ RL03) can be neglected (Flechtner et al. 2006).”
Interannual variations of the mass balance of the Antarctica and Greenland ice sheets from GRACE (2006, methodology): “Similarly in the geoid computation process, they account for oceans perturbation using an a priori barotropic oceanmodel (the MOG2D barotropic ocean model, Carrere and Lyard, 2003). As a consequence, the time-variable GRACE geoids analysed in the present study mainly represent signals due to land wa”