Regional to Global Evolution of Impacts of Parameterized Mountain-Wave Drag in the Lower Stratosphere

• Published in: Journal of climate 2020-04, Vol.33 (8), p.3093-3106
• Main Author: Kruse, Christopher G.
• Format: Article
• Language: English
• Subjects: Advection; Atmosphere; Atmospheric circulation; Atmospheric gravity waves; Climate; Climate models; Computational fluid dynamics; Diffusion; Drag; Evolution; General circulation; General circulation models; Gravitational waves; Gravity waves; Horizontal advection; Horizontal diffusion; Lower stratosphere; Mountains; North Pole; Northern Hemisphere; Polar caps; Potential vorticity; Simulation; Southern Hemisphere; Stratosphere; Survival; Two dimensional models; Vorticity; Wave drag; Winter
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/JCLI-D-19-0076.1

Mountain ranges are regional features on Earth, as are the regions of mountain-wave drag (MWD) exerted by dissipating atmospheric gravity waves generated by flow over them. However, these regional drags have significant global- or zonal-mean impacts on Earth’s atmospheric general circulation (e.g., slowing of the polar night jet). The objective of this work is to understand the regional to global evolution of these impacts. The approach is to track the evolution of MWD-generated potential vorticity (PV) over the winter using the Whole Atmosphere Community Climate Model (WACCM). Within an ensemble of winter-long runs with and without MWD, lower-stratospheric PV is generated over mountains and advected downstream, generating large-scale PV banners. These PV banners are diffused but survive this diffusion and are reinforced over downstream mountain ranges, accumulating into zonal-mean or global features within WACCM. A simple 2D model representing sources, advection, and diffusion of “passive PV” recreates the salient features in the WACCM results, suggesting the winter-long evolution of MWD-generated PV can be crudely understood in terms of horizontal advection and diffusion within a global vortex. In the Northern Hemisphere, cyclonic, equatorward PV banners accumulate zonally into a single zonally symmetric positive PV anomaly. The anticyclonic, poleward PV banners also accumulate into a zonally symmetric feature, but then diffuse over the North Pole into a negative PV polar cap. In the Southern Hemisphere, the same processes are at work, though the different geographic configuration of mountain ranges leads to different patterns of impacts.