Observing the pole tide with satellite altimetry

By Shailen Desai. 2002

241 citations recorded by the source corpus.

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Citations in the corpus

Precision Orbit Determination Standards for the Jason Series of Altimeter Missions (2010, background): “The ocean pole tide, a more recent addition to the IERS standards from Desai (2002), is also included.”
GRACE detects coseismic and postseismic deformation from the Sumatra‐Andaman earthquake (2007, methodology): “based on satellite altimeter data [Desai, 2002].”
Variations of the Earth's figure axis from satellite laser ranging and GRACE (2011, background): “The value of 0.3077 +i0.0036istheanelasticLovenumberusedforthesolidEarth pole tide and g2 + ig2 = 0.705+i0.0036 for the ocean pole tide model [ Desai, 2002 ] in the IERS2003 conventions (thevalue of g2 is updated to be 0.687 in the IERS 2010 convention [Petit and Luzum, 2010]).”
The third realization of the International Celestial Reference Frame by very long baseline interferometry (2020, background): “7.1.4) and the oceans (Desai 2002) were also incorporated in the modeling.”
Deceleration in the Earth's oblateness (2013, methodology): “The ITRF2005 reference frame for tracking stations (specifically, SLRF2005/LPOD2005 [Ries, 2008]), the ocean pole tide [Desai, 2002], the FES2004 ocean (diurnal and semidiurnal) tides [Lyard et al., 2006], and the EGM2008 gravity model [Pavlis et al., 2012] were used in this analysis.”
The GeoForschungsZentrum Potsdam/Groupe de Recherche de Gèodésie Spatiale satellite-only and combined gravity field models: EIGEN-GL04S1 and EIGEN-GL04C (2008, methodology): “EIGEN-GRACE04S also takes into account a model for the self-consistent ocean pole tide (Desai 2002).”