Efficient Inverse Modeling of Barotropic Ocean Tides

By Gary D. Egbert, S. Erofeeva. 2002

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In Oceanography

Citations in the corpus

Accuracy assessment of global barotropic ocean tide models (2014, methodology): “EOT11a output was used between 74◦N and 84◦S as a constraint. A direct optimization method was used for finding the minimum of a cost function containing dynamical residual smoothing terms, which are the first and the second derivatives of the model residuals. Thus, the model does not smooth control”
The accuracy of surface elevations in forward global barotropic and baroclinic tide models (2004, background): “2 solution (Egbert and Erofeeva, 2002) compare well with Antarctic tidegauge data (Laurie Padman, Gary Egbert, and Lana Erofeeva, personal communication 2004).”
The third realization of the International Celestial Reference Frame by very long baseline interferometry (2020, methodology): “Ocean loading displacements were obtained from the TPXO.7.2 model (Egbert & Erofeeva 2002), supplemented with the FES99 model (Lefèvre et al. 2002) for the long-period Ssa tide, while those due to atmospheric pressure loading (both tidal and non-tidal) come from the APLO model (Petrov & Boy 2004).”
Energetics of M2 Barotropic-to-Baroclinic Tidal Conversion at the Hawaiian Islands (2008, methodology): “2 inverse model (Egbert 1997; Egbert and Ray 2001; Egbert and Erofeeva 2002).”
Three‐dimensional, nonhydrostatic numerical simulation of nonlinear internal wave generation and propagation in the South China Sea (2011, methodology): “Superimposed over this are the predicted barotropic currents (averaged over the entire depth) from SUNTANS and OTIS [Egbert and Erofeeva, 2002].”
Profiling risk and sustainability in coastal deltas of the world (2015, background): “org Methods Figures S1-S4 Tables S1-S3 References (34-52)”
Eddy‐driven recirculation of Atlantic Water in Fram Strait (2016, methodology): “Tidal forcing is added along the open boundaries from the global TPXO tidal model [Egbert and Erofeeva, 2002].”
A barotropic inverse tidal model for the Arctic Ocean (2004, positive): “by direct matrix factorization for 8 harmonics: M2 ,S 2 ,N 2, K2 ,K 1 ,O 1 ,P 1, and Q1; see Egbert and Erofeeva [2002] (hereinafter denoted E&E).”