rossby wave वाक्य
उदाहरण वाक्य
मोबाइल
- Each large meander, or wave, within the jet stream is known as a Rossby wave ( planetary wave ).
- Satellite observations have revealed the stately progression of Rossby waves across all the ocean basins, particularly at low-and mid-latitudes.
- Usually the shorter Rossby waves have an eastward group velocity and the longer ones have a westward group velocity.
- Wavenumbers 1 6 are called long waves and often synonymous in meteorological literature with the mid-latitude planetary Rossby waves.
- At shortest periods are the equatorial gravity waves while the longest periods are associated with the equatorial Rossby waves.
- Internal waves are usually distinguished from Rossby waves, which are influenced by the change of Coriolis frequency with latitude.
- The terms " barotropic " and " baroclinic ", are used to distinguish the vertical structure of Rossby waves.
- In addition, long distance links that are associated with Rossby waves are the most dominant links in the climate network.
- In the atmosphere it gives rise to large-scale patterns like Rossby waves and determines the basic circulation patterns of storms.
- This blocking pattern causes Rossby waves with zonal wavenumber 1 and / or 2 to grow to unusually large amplitudes.
- Atmospheric Rossby waves are the result of conservation of potential vorticity and are influenced by the Coriolis force and pressure gradient.
- One can identify a terrestrial Rossby wave as its phase velocity, marked by its wave crest, always has a westward component.
- However, the collected set of Rossby waves may appear to move in either direction with what is known as its group velocity.
- Rossby waves "'move along the thermocline : the boundary between the warm upper layer and the cold deeper part of the ocean.
- Rossby waves, named after Carl-Gustaf Arvid Rossby are important in planetary atmospheres and oceans and are also known as it planetary waves.
- In the northern hemisphere the jet stream was very disturbed, resulting in a Rossby wave pattern of high and low pressure regions.
- Therefore, the physical mechanism responsible for the propagation of these equatorial Rossby waves is none other than the conservation of potential vorticity:
- Rossby waves have been suggested as an important mechanism to account for the heating of the ocean on Europa, a moon of Jupiter.
- When these frontal storms along the Rossby waves turned north-eastward, they hit southwest England, Wales, north England and Scotland and across to Scandinavia.
- 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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