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How much could be gained from ocean-data assimilation if ENSO were a simple stochastic oscillator?
Assimilation of sub-surface ocean data is one of the factors that have contributed to the increas...
G Burgers | Conference: Third WMO international symposium on assimilation | Organisation: WMO (Geneva 2000) | Place: Quebec City | First page: 0 | Last page: 0
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Tropical disturbances in a GCM
We have analyzed the tropical disturbances in a 11-layer atmospheric general circulation model (G...
RJ Haarsma, JFB Mitchell, CA Senior | Status: published | Journal: Clim. Dyn. | Volume: 8 | Year: 1993 | First page: 247 | Last page: 257
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Bifurcations in a low-order model with self-interaction
For finite the equivalent depth, the shallow-water equations (SWE) exhibit instabilities based on...
RJ Haarsma, JD Opsteegh | Status: published | Journal: Tellus | Volume: 43A | Year: 1991 | First page: 266 | Last page: 276
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Global ocean mean wave period data: validation and description
A global comparison of altimeter and ERA-40 mean wave period data is performed for the first time...
S Caires, A Sterl, CP Gommemginger | Status: published | Journal: J. Geophys. Res. | Volume: 110 | Year: 2005 | First page: 0 | Last page: 0 | doi: 10.1029/2004JC002631
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Applications of continuation methods in physical oceanography
In this paper, continuation methods are used to study fundamental problems in physical oceanograp...
CA Katsman, HA Dijkstra, MJ Schmeits | Conference: Continuation methods in Fluid Dynamics. ERCOFTAC/ | Organisation: Notes on Numerical Fluid mecha | First page: 155 | Last page: 166
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