Why Eddy Momentum Fluxes are Concentrated in the Upper Troposphere
Farid Ait-Chaalal, Tapio Schneider

TL;DR
This study uses an idealized GCM to investigate why Earth's extratropical eddy momentum flux is concentrated in the upper troposphere, highlighting the roles of nonlinear eddy interactions and wave absorption processes.
Contribution
It demonstrates that nonlinear eddy-eddy interactions and wave absorption in the surf zone are key to EMF concentration, independent of surface drag or linear wave propagation.
Findings
EMF concentration is not due to surface drag.
Linear wave propagation is not the primary cause.
Nonlinear interactions in the surf zone are essential for EMF concentration.
Abstract
The extratropical eddy momentum flux (EMF) is controlled by generation, propagation, and dissipation of large-scale eddies and is concentrated in Earth's upper troposphere. An idealized GCM is used to investigate how this EMF structure arises. In simulations in which the poles are heated more strongly than the equator, EMF is concentrated near the surface, demonstrating that surface drag generally is not responsible for the upper-tropospheric EMF concentration. Although Earth's upper troposphere favors linear wave propagation, quasi-linear simulations in which nonlinear eddy-eddy interactions are suppressed demonstrate that this is likewise not primarily responsible for the upper-tropospheric EMF concentration. The quasi-linear simulations reveal the essential role of nonlinear eddy-eddy interactions in the surf zone in the upper troposphere, where wave activity absorption away from the…
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