Rossby Waves

Some articles on rossby waves, waves, wave:

Rossby Wave - Oceanic Waves
... Oceanic Rossby waves are thought to communicate climatic changes due to variability in forcing, due to both the wind and buoyancy ... Both barotropic and baroclinic waves cause variations of the sea surface height, although the length of the waves made them difficult to detect until the advent of ... by the NASA/CNES TOPEX/Poseidon satellite confirmed the existence of oceanic Rossby waves ...
Equatorial Waves - Connection To El Nino Southern Oscillation
... Kelvin waves have been connected to El Nino (beginning in the Northern Hemisphere winter months) in recent years in terms of precursors to this ... oscillation (MJO) can trigger oceanic Kelvin waves throughout its 30–60 day cycle or the latent heat of condensation can be released (from intense convection) resulting in ... the east, thereby exciting a Kelvin wave, which in this sense can be thought of as a warm-water anomaly that travels under the ocean’s surface at a depth of about 150 meters ...
Atmosphere Of Jupiter - Dynamics - Shallow Models
... Its existence is connected to production of Rossby waves ... reach a certain size, the energy begins to flow into Rossby waves instead of larger structures, and the inverse cascade stops ... the spherical rapidly rotating planet the dispersion relation of the Rossby waves is anisotropic, the Rhines scale in the direction parallel to the equator is ...
Rossby Wave
... Atmospheric Rossby waves are giant meanders in high-altitude winds that are a major influence on weather ... They are not to be confused with oceanic Rossby waves, which move along the thermocline that is, the boundary between the warm upper layer of the ocean and the cold deeper part of the ocean ... Rossby waves are a subset of inertial waves ...
Indonesian Throughflow
... westerly winds in the eastern Indian Ocean force equatorial downwelling Kelvin waves (eastward moving, eastward flow) that propagate through the Indonesian ... Global-scale, ocean waves such as equatorial/coastal Kelvin and Rossby waves drive interannual variation of the ITF with an amplitude of roughly +/-3 Sv ... winds from El Nino force westward moving-equatorial Rossby waves and eastward currents that hit eastern New Guinea and propagate around the west coast as coastal Kelvin ...

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