A mean dynamic topography computed over the world ocean from altimetry, in situ measurements, and a geoid model

By Marie-Hélène Rio, F. Hernandez. 2004

517 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/90e3bf939048718557707ddd971ed0e591abe961

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In Global and Planetary Change

In Oceanography

Citations in the corpus

Atlantic meridional overturning circulation and the Southern Hemisphere supergyre (2007, background): “[14] Because of its intermediate depth, the Tasman route has never been invoked before as a major feature for the AMOC in inverse global calculations [Ganachaud and Wunsch, 2000; Sloyan and Rintoul, 2001], and in the mean absolute dynamical topography recently derived [ Rio and Hernandez, 2004; Max”
Mean Dynamic Topography of the Ocean Derived from Satellite and Drifting Buoy Data Using Three Different Techniques (2009, methodology): “The analytical correlation functions between these variables are derived from the geostrophic momentum balance (Rio and Hernandez 2004; Rio et al. 2005).”
The Irminger Gyre: Circulation, convection, and interannual variability (2011, methodology): “Absolute dynamic topography was obtained from a combination of the SSH anomalies and a mean dynamic topography product, which was computed from altimetry, in-situ data, and a geoid model (Rio and Hernandez, 2004).”
Assimilating Along-Track Altimetric Observations through Local Hydrostatic Adjustment in a Global Ocean Variational Assimilation System (2011, methodology): “The large-scale features of the MDT thus computed are in general very similar to those derived from gravimetry and in situ data, like the MDT from Rio and Hernandez (2004), except in some areas such as the Gulf Stream region and especially the Antarctic Circumpolar Current, the former due to the dif”
Simulation of the present-day climate with the climate model INMCM5 (2017, unknown): “2010) and Rio and Hernandez (2004).”
A biologist's guide to assessing ocean currents: a review (2012, methodology): “The mean of the surface geostrophic current was provided by Rio & Hernandez (2004) on a regular 1° × 1° grid.”
To go or not to go with the flow: Environmental influences on whale shark movement patterns (2010, methodology): “These limits were added to a mean dynamic topography grid based on a geoid model (Rio and Hernandez, 2004) and the resulting absolute dynamic topography maps were reprojected into a Mercator equal-area projection and east–west (dz/dx) and north–south (dz/dy) gradients calculated using a filter in…”
State of the climate in 2010 (2011, methodology): “…OSCAR (Ocean Surface Current Analyses–Real time) product, which uses AVISO altimetry, winds, SST, and the Rio05 mean dynamic topography (Rio and Hernandez 2004) to create a 0.33°-resolution surface current maps averaged over the 0 m–30 m layer of the ocean (Bonjean and Lagerloef 2002).”