Self-Organization of Atmospheric Macroturbulence into Critical States of Weak Nonlinear Eddy-Eddy Interactions

By Tapio Schneider, Christopher C. Walker. 2006

152 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/a1237626c650c7e77b9dd48cbfb287b681cc3943

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Citations in the corpus

WATER VAPOR AND THE DYNAMICS OF CLIMATE CHANGES (2009, background): “In dry atmospheres, an increased static stability means that the latitude at which baroclinic eddy fluxes first become deep enough to reach the upper troposphere moves poleward [Held, 1978; Schneider and Walker, 2006].”
Eddy-Mediated Regime Transitions in the Seasonal Cycle of a Hadley Circulation and Implications for Monsoon Dynamics (2008, methodology): “In all respects other than the radiative-heating formulation , the idealized GCM is the same as that described by Schneider and Walker (2006) and used by Walker and Schneider (2006).”
Parameterization of Mixed Layer Eddies. Part I. Theory and Diagnosis (2008, background): “Eddy mixing length arguments are routinely used to study baroclinic eddy fluxes (Haine and Marshall 1998; Spall 2000; Larichev and Held 1995; Schneider and Walker 2006).”
Eddy Influences on Hadley Circulations: Simulations with an Idealized GCM (2006, methodology): “The simulations with the normative radiative-equilibrium state and with spatially varying thermal relaxation time analyzed here are the same as those whose extratropical macroturbulence and thermal stratification we analyzed in Schneider and Walker (2006).”
Ocean Circulation Kinetic Energy: Reservoirs, Sources, and Sinks (2009, background): “Similar gaps exist in the world oceans, but not in the atmosphere where the first deformation radius is of O(1000) km and the inverse cascade can span a limited wavenumber range (Boer and Shephard, 1983; Schneider and Walker, 2006).”
Formation of Jets and Equatorial Superrotation on Jupiter (2008, background): “Poleward of 20◦, the di- boundary of the integration, N2p = −(ρ̄θ̄)−1 ∂pθ is a static stability measure, and ρ is density (Schneider and Walker 2006).”