Atmospheric forcing of the oceanic semidiurnal tide
- 29 January 2005
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 32 (2)
- https://doi.org/10.1029/2004gl021668
Abstract
No abstract availableKeywords
This publication has 22 references indexed in Scilit:
- The accuracy of surface elevations in forward global barotropic and baroclinic tide modelsDeep Sea Research Part II: Topical Studies in Oceanography, 2004
- Parameterization of ocean self‐attraction and loading in numerical models of the ocean circulationJournal of Geophysical Research: Oceans, 2004
- Semi‐diurnal and diurnal tidal dissipation from TOPEX/Poseidon altimetryGeophysical Research Letters, 2003
- Modeling the barotropic response of the global ocean to atmospheric wind and pressure forcing ‐ comparisons with observationsGeophysical Research Letters, 2003
- Modeling the high‐frequency barotropic response of the ocean to atmospheric disturbances: Sensitivity to forcing, topography, and frictionJournal of Geophysical Research: Oceans, 2001
- Short‐period oceanic circulation: Implications for satellite altimetryGeophysical Research Letters, 2000
- De‐aliasing of global high frequency barotropic motions in altimeter observationsGeophysical Research Letters, 2000
- Nature of global large‐scale sea level variability in relation to atmospheric forcing: A modeling studyJournal of Geophysical Research: Oceans, 1998
- Understanding the relation between wind‐ and pressure‐driven sea level variabilityJournal of Geophysical Research: Oceans, 1994
- Normal Modes of the World Ocean. Part II: Description of Modes in the Period Range 8 to 80 HoursJournal of Physical Oceanography, 1981