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A balanced state consistent with planetary-scale motion for quasi-geostrophic dynamics Cover

A balanced state consistent with planetary-scale motion for quasi-geostrophic dynamics

By:  and    
Open Access
|Jan 2020

Figures & Tables

Fig. 1.

The velocity, temperature and forcing associated with the pressure field, P=(Γ+AsinωX) Yz. The vertical and horizontal structure of P is shown in three representative vertical levels (a). The horizontal wind vector fields with streamlines in lower level (z = 0.1) and high level (z = 1.0) are shown in (b) and (c), respectively. The horizontal structures of the driving forcing QL are shown in the three vertical levels in (d). The meridional and vertical velocity with the forcing QL in Yz plane is shown in (e) and (f), where two different X values are chosen as X=1.0 (e) and X = 0 (f) and the colour represents the forcing QL.

Fig. 2.

Same as in Fig. 1 with the different pressure field P=ΓYz+Aeγzsin(ωX).

Language: English
Page range: 1697164 - 1697164
Published on: Jan 1, 2020
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 2020 Woosok Moon, James Y-K. Cho, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.