Diky L A,Golitsyn G S.1968.Calculation of the Rossby wave velocities in the earth's atmosphere.Tellus,20:314-317.Diky, L. A. and Golitsyn, G. S. 1968. Calculation of the Rossby wave velocities in the Earth's atmosphere. Tellus 20, 314-317....
Note also a slight increase in the gravity wave forcing which is also contributing to the vortex breakdown [Scheffler and Pulido, 2015]. Figure 5b shows the calculation of the gravity wave forcing (gray line) as a residual of the other three terms in 7 ( ), and also from the forcing ...
The innovation of this paper starts from a Boussinesq equation, which portrays a Rossby wave with a Beta effect. Then, we obtain the first-order, second-order, and third-order rogue wave solutions with the Hirota bilinear method and symbolic calculation. As far as we know, these have not ...
In this section, we will determine if three leading oceanic mechanisms (Rossby waves, spiciness, and STCs) serve as precursors for TPDV in FOSI via statistical analysis and confirm their influence in the decadal hindcasts. We illustrate the characteristics of the Rossby wave reflection mechanism by...
(5) from a point to the east of the Bahamas, xe, along the baroclinic Rossby wave characteristic $$\begin{array}{*{20}{l}} {\eta \left( {x_{\mathrm{B}},t} \right)} \hfill & = \hfill & {\eta \left( {x_{\mathrm{e}},t + \frac{{x_{\mathrm{B}} - x_{\mathrm{e...
function mode 1 amplitude to topographic Rossby wave's theoretical wave solution on EM14-I2 (circle) and WM96 (triangle). (d) Least-squares fitting of the root-mean-square of vertical velocity to topographic Rossby wave's theoretical wave solution on EM14-I1 (circle) and EM14-I2 (...
The feature of four - wave quasi -resonance dynamics among one mountain wave and three free Rossby waves in the barotropic atmosphere is researched. From a quasigeostrophic barotropic vorticity equation including mountain, in terms of two- time scale,the coupled mode equations of four -wave quasi...