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Effect of quadric shear basic zonal flows and topography on baroclinic instability Cover

Effect of quadric shear basic zonal flows and topography on baroclinic instability

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Volume 72 (2020): Issue 1
By: ,  ,   and    
Open Access
|Jan 2020
Figures & tables

Figures & Tables

Fig. 1.

Spatial structure of unstable modes in the presence of these meridional topographic slopes.

Fig. 2.

Spatial structure of unstable modes in the presence of a zonal topographic slope: sx=1×10−3.

Fig. 3.

Spatial structure of unstable modes in the presence of a zonal topographic slope: sx=5×10−3.

Fig. 4.

Spatial structure of unstable modes in the presence of a zonal topographic slope: sx=1×10−2.

DOI: https://doi.org/10.1080/16000870.2020.1843330 | Journal eISSN: 3035-9554
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Language: English
Page range: 1843330 - 1843330
Published on: Jan 1, 2020
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
Keywords:
topographic slope,
basic zonal flows,
quadric shear,
baroclinic instability,
β plane approximation

© 2020 Xiujie Zhang, Hongxin Zhang, Yuying Yang, Jian Song, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.

Volume 72 (2020): Issue 1
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