Stability of Geostrophic Vortices On a Rotating Sphere
Stability of Geostrophic Vortices On a Rotating Sphere
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In our eReader you can find the full English version of the book. Read Stability of Geostrophic Vortices On a Rotating Sphere Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Stability of Geostrophic Vortices On a Rotating Sphere
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-173- (i) 4 Vortices with Equal Strength y, Equally Spaced on a Circle of Colatitude 9, No Boundary Condition at the Equator . Here we study three cases for the coriolis parameter c = . 7 and one case for the coriolis parameter c = . 5. P P The linear analysis establishes that zero is an eigenvalue of multiplicity two for all values of the parameters. In particular for c = . 1, we find that for 6 _ 49. 6865°. For c = . 5, the configuration studied is in the exponentially ions table region. (a) ...9 = 45°, c = . 7. The configuration is exponentially stable. The experiments were carried out with initial displace- ments eg, , ea, between +1° and + 30°. The results show that all the resulting motions are linear stable motions, even though in some cases, the amplitudes of the resulting oscillations are bounded by 3/2 of the initial disturbance. This is particularly true when the initial displacement is in the longitudinal direction. For initial displacements in the G direction, the circle vortices tend to oscillate about a new position north or south of the equilibrium circle of colatitude depending on the sign of eS-, - This phenomenon has the effect of changing the angular velocity of rotation.
What to read after Stability of Geostrophic Vortices On a Rotating Sphere?
You can find similar books in the "Read Also" column, or choose other free books by Carlos a Leiva to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
-173- (i) 4 Vortices with Equal Strength y, Equally Spaced on a Circle of Colatitude 9, No Boundary Condition at the Equator . Here we study three cases for the coriolis parameter c = . 7 and one case for the coriolis parameter c = . 5. P P The linear analysis establishes that zero is an eigenvalue of multiplicity two for all values of the parameters. In particular for c = . 1, we find that for 6 _ 49. 6865°. For c = . 5, the configuration studied is in the exponentially ions table region. (a) ...9 = 45°, c = . 7. The configuration is exponentially stable. The experiments were carried out with initial displace- ments eg, , ea, between +1° and + 30°. The results show that all the resulting motions are linear stable motions, even though in some cases, the amplitudes of the resulting oscillations are bounded by 3/2 of the initial disturbance. This is particularly true when the initial displacement is in the longitudinal direction. For initial displacements in the G direction, the circle vortices tend to oscillate about a new position north or south of the equilibrium circle of colatitude depending on the sign of eS-, - This phenomenon has the effect of changing the angular velocity of rotation.
What to read after Stability of Geostrophic Vortices On a Rotating Sphere?
You can find similar books in the "Read Also" column, or choose other free books by Carlos a Leiva to read onlineMoreLess
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