Svetlana Y. Erofeeva

TL;DR: In this paper, a relocatable system for generalized inverse (GI) modeling of barotropic ocean tides is described, where the GI penalty functional is minimized using a representer method, which requires repeated solution of the forward and adjoint linearized shallow water equations.

TL;DR: The accuracy of state-of-the-art global barotropic tide models is assessed using bottom pressure data, coastal tide gauges, satellite altimetry, various geodetic data on Antarctic ice shelves, and independent tracked satellite orbit perturbations as discussed by the authors.

TL;DR: In this article, the authors describe high-resolution linear-dynamics and inverse models of Arctic Ocean barotropic tides obtained with the OSU Tidal Inversion Software (OTIS) package.

TL;DR: In this paper, the authors studied the South China Sea (SCS) by assimilating Topex/Poseidon altimetry data into a barotropic ocean tide model for the eight major constituents (M 2 S 2 K 1 O 1 N 2 K 2 P 1 Q 1 ).

TL;DR: In this article, the authors investigated the circulation and water mass transports north of the Denmark Strait using recently collected and historical in situ data along with an idealized numerical model and atmospheric reanalysis fields.