A Quantitative Scaling Theory for Meridional Heat Transport in Planetary Atmospheres and Oceans
Author:
Affiliation:
1. Université Paris‐Saclay CNRS CEA, Service de Physique de l’Etat Condensé Gif‐sur‐Yvette France
2. Massachusetts Institute of Technology Cambridge MA USA
Funder
H2020 European Research Council
Division of Atmospheric and Geospace Sciences
Publisher
American Geophysical Union (AGU)
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020AV000362
Reference53 articles.
1. Baroclinically Unstable Geostrophic Turbulence in the Limits of Strong and Weak Bottom Ekman Friction: Application to Midocean Eddies
2. Effects of Mean Flow Direction on Energy, Isotropy, and Coherence of Baroclinically Unstable Beta-Plane Geostrophic Turbulence
3. On Quadratic Bottom Drag, Geostrophic Turbulence, and Oceanic Mesoscale Eddies
4. A GCM Investigation into the Nature of Baroclinic Adjustment
5. Inverse energy cascade in stationary two-dimensional homogeneous turbulence
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