De‐aliasing of global high frequency barotropic motions in altimeter observations
- 15 April 2000
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 27 (8) , 1175-1178
- https://doi.org/10.1029/1999gl011263
Abstract
No abstract availableThis publication has 8 references indexed in Scilit:
- Short‐period oceanic circulation: Implications for satellite altimetryGeophysical Research Letters, 2000
- Regional analysis of the inverted barometer effect over the global ocean using TOPEX/POSEIDON data and model resultsJournal of Geophysical Research: Oceans, 1999
- Time variability of the Earth's gravity field: Hydrological and oceanic effects and their possible detection using GRACEJournal of Geophysical Research, 1998
- Nature of global large‐scale sea level variability in relation to atmospheric forcing: A modeling studyJournal of Geophysical Research: Oceans, 1998
- Representation of Topography by Shaved Cells in a Height Coordinate Ocean ModelMonthly Weather Review, 1997
- Hydrostatic, quasi‐hydrostatic, and nonhydrostatic ocean modelingJournal of Geophysical Research: Oceans, 1997
- Atmospheric loading and the oceanic “inverted barometer” effectReviews of Geophysics, 1997
- Understanding the relation between wind‐ and pressure‐driven sea level variabilityJournal of Geophysical Research: Oceans, 1994