Atmospheric Rossby waves are the result of conservation of potential vorticity and are influenced by the Coriolis force and pressure gradient.
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One can identify a terrestrial Rossby wave as its phase velocity, marked by its wave crest, always has a westward component.
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However, the collected set of Rossby waves may appear to move in either direction with what is known as its group velocity.
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Rossby waves "'move along the thermocline : the boundary between the warm upper layer and the cold deeper part of the ocean.
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Rossby waves, named after Carl-Gustaf Arvid Rossby are important in planetary atmospheres and oceans and are also known as it planetary waves.
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In the northern hemisphere the jet stream was very disturbed, resulting in a Rossby wave pattern of high and low pressure regions.
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Therefore, the physical mechanism responsible for the propagation of these equatorial Rossby waves is none other than the conservation of potential vorticity:
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Rossby waves have been suggested as an important mechanism to account for the heating of the ocean on Europa, a moon of Jupiter.
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When these frontal storms along the Rossby waves turned north-eastward, they hit southwest England, Wales, north England and Scotland and across to Scandinavia.
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Five pulses of the MJO and Equatorial Rossby waves ( ER ) were responsible for most of the cyclone activity during the season.
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