L. Novak, T. Schneider, and F. Ait-Chaalal, 2018
"Midwinter suppression of storm tracks in an idealized zonally symmetric setting ",
Journal of the Atmospheric Sciences
TURBULENT CLOSURES AND DIRECT STATISTICAL SIMULATIONS OF GEOPHYSICAL FLOWS<
(with J.B. Marston and T. Schneider)
We are developing approaches to computing geophysical flows statistics directly, rather than through aggregation of direct numerical simulations, as is currently done, for example, in climate models. The research draws on concepts from atmospheric dynamics and theoretical physics. The long-term goal is the development of a new generation of atmosphere models that provide climate statistics directly and that are more efficient than current models in the simulation of deep-time climate and in providing insight into climatic phenomena.
Our approach is to explore how turbulent statistical closures capture atmospheric flows. Besides providing new methods to compute climate, this method might help to build physical laws for climate. For example, a comprehensive theory that would predict the dependence of eddy fluxes with mean fields is currently missing for planetary flows and constitutes an outstanding theoretical challenge.
F. Ait-Chaalal, T. Schneider, B. Meyer and J.B. Marston, 2016
"Cumulant expansions for atmospheric flows ",
New Journal of Physics, Focus on Stochastic Flows and Climate Statistics, Vol. 18, 025019
[download pdf][Official link]
MOMENTUM FLUX IN LARGE-SCALE ATMOSPHERIC FLOWS
(with T. Schneider)
Large-scale baroclinic Rossby waves are essential in setting the general circulation of Earth's atmosphere.
They are generated at mid-latitudes through baroclinic instability, propagate meridionaly and dissipate
before they reach their critical lines in the flank of the jet streams. Propagating Rossby waves transports
(angular) momentum toward where they are generated. Consequently, generation and dissipation of large-scale
eddies at different latitudes causes meridional momentum flux, with convergence at mid-latitudes
and divergence in subtropics and to a lesser extent in polar regions.
Yet it is unclear why the eddy momentum fluxes are concentrated in the upper troposphere. With that question, one of the most basic features of the general circulation of atmospheres remains unexplained.
We address the question of what controls the structure of eddy momentum fluxes with a hierarchy of dry idealized GCMs. We use simplified GCMs in which, for example, nonlinear eddy-eddy interactions (but not eddy–mean flow interactions)
are suppressed, to determine which atmospheric turbulence characteristics are responsible for the structure of eddy momentum fluxes.
F. Ait-Chaalal and T. Schneider, 2015
"Why eddy momentum fluxes are concentrated in the upper troposphere ",
Journal of the Atmospheric Sciences, Vol. 72, 1585-1604
[download pdf][Official link]
Supplemental material: comparing wave breaking in a fully nonlinear simulation, in a simulation where only eddy-mean flow interaction is retained and in a simulation where barotropic eddy-eddy interactions are restored. The videos show potential vorticity on the
320 K isentrope (upper tropical troposphere, lower stratosphere in polar regions):
MIXING OF PASSIVE AND ACTIVE TRACERS IN GEOPHYSICAL FLOWS
This research is motivated by the need to better understand the effect of resolution on the ozone layer chemistry in Chemistry-Climate models.The interest and relevance of this research are also fundamental, since the mixing of chemically active tracers in chaotic and turbulent flows is far from being satisfactorily understood.