planetary wave वाक्य
उदाहरण वाक्य
मोबाइल
- His Thesis was a study of " Planetary Waves ."
- At this point planetary waves may no longer penetrate into the stratosphere ).
- Thus the polar night jet weakens and simultaneously becomes distorted by the growing planetary waves.
- Mixing occurs with unstable planetary waves that are characteristic of the middle and upper stratosphere in winter.
- Each large meander, or wave, within the jet stream is known as a Rossby wave ( planetary wave ).
- Lindzen's work on atmospheric tides led him to the study of planetary waves and the general circulation of atmospheres.
- In " Planetary waves on beta planes ", he developed a Bretherton appeared, which Lindzen read with great interest.
- Propagation of El Ni�o effect through planetary waves may have warmed the polar region and delayed the onset of the northern hemisphere glaciation.
- Equatorial Rossby waves can also adjust to equilibrium under gravity in the tropics; because the planetary waves have frequencies much lower than gravity waves.
- Rossby waves, named after Carl-Gustaf Arvid Rossby are important in planetary atmospheres and oceans and are also known as it planetary waves.
- Early and late polar breakup episodes have occurred, due to variations in the stratospheric flow structure and upward spreading of planetary waves from the troposphere.
- Scientists are connecting a delay in the Arctic vortex breakup with a reduction of planetary wave activities, few stratospheric sudden warming events, and depletion of ozone.
- Examination of the climatology data over the same period of time indicates that these wild planetary wave meanderings are not a normal aspect of our regional climate patterns.
- :The location of a volcano strongly influences the geographic distribution of atmospheric heating and the development of planetary waves that affect air circulation ( especially in the northern hemisphere ).
- More recent work has shown that most teleconnections from the tropics to the extratropics can be understood to surprising accuracy by the propagation of linear, planetary waves upon a 3-dimensional seasonally-varying basic state.
- The second stage is one where quasi-geostrophic adjustment takes place by means of planetary waves; this process can be comparable to the wave field adjusting to the mass field ( due to the wavelengths being larger than the Rossby deformation radius.
- When this occurs, the vortex rings become more unstable and prone to shifting by planetary waves . The planetary wave activity in both hemispheres varies year-to-year, producing a corresponding response in the strength and temperature of the polar vortex.
- When this occurs, the vortex rings become more unstable and prone to shifting by planetary waves . The planetary wave activity in both hemispheres varies year-to-year, producing a corresponding response in the strength and temperature of the polar vortex.
- Thus, the phase and group speeds are equal in magnitude but opposite in direction ( phase speed is westward and group velocity is eastward ); note that is often useful to use potential vorticity as a tracer for these planetary waves, due to its invertibility ( especially in the quasi-geostrophic framework ).
- In 2005-2006 he showed that processes based on the nonlinear nature of the atmospheric dynamics could probably address the question What caused the southern hemisphere to exhibit very strong planetary waves in 2002 ? This evidence is based on his new finding that the fluctuations of the total ozone content and temperature exhibit long-range correlations.
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