Diagnosing the vertical structure of the eddy diffusivity in real and idealized atmospheres
The Earth's extratropical troposphere is equilibrated by turbulent eddy fluxes of potential temperature and momentum. The equilibrated state has the remarkable characteristic that isentropic slopes leaving the surface in the subtropics reach the tropopause near the Poles. It has been speculated...
Main Authors: | Jansen, Malte Friedrich (Contributor), Ferrari, Raffaele (Contributor) |
---|---|
Other Authors: | Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences (Contributor) |
Format: | Article |
Language: | English |
Published: |
Wiley Blackwell,
2015-10-06T17:47:41Z.
|
Subjects: | |
Online Access: | Get fulltext |
Similar Items
-
The Vertical Structure of the Eddy Diffusivity and the Equilibration of the Extratropical Atmosphere
by: Jansen, Malte Friedrich, et al.
Published: (2013) -
Equilibration of an Atmosphere by Adiabatic Eddy Fluxes
by: Jansen, Malte Friedrich, et al.
Published: (2014) -
The Eddy Diffusivity in Barotropic β-Plane Turbulence
by: Hailu Kong, et al.
Published: (2017-10-01) -
Diagnosing Subgrid Mesoscale Eddy Fluxes With and Without Topography
by: Sina Khani, et al.
Published: (2019-12-01) -
Suppression of Eddy Diffusivity across Jets in the Southern Ocean
by: Ferrari, Raffaele, et al.
Published: (2011)