Internal gravity waves in a saturated moist neutral atmosphere

AMS Citation:
Muraki, D. J., and R. Rotunno, 2013: Internal gravity waves in a saturated moist neutral atmosphere. Journal of the Atmospheric Sciences, 70, 3693-3709, doi:10.1175/JAS-D-13-051.1.
Date:2013-12-01
Resource Type:article
Title:Internal gravity waves in a saturated moist neutral atmosphere
Abstract: This work is motivated by an unusual feature associated with the start-up of a moist nearly neutral atmospheric flow over a mountain ridge that was previously observed in a full-physics numerical model. In that study, the upstream propagation of a wave of subsidence precluded the establishment of upward-displaced and saturated flow that might be expected upstream of the topography. This phenomenon was hypothesized to be a consequence of the peculiar property of saturated moist neutral flow: an upward air parcel displacement produces zero buoyancy, while a downward displacement desaturates the air parcel and produces a positive buoyancy anomaly. In the present study, this hypothesis is confirmed within numerical solutions to a reduced system of equations that incorporates the saturated-atmosphere property in a particularly simple manner. The relatively uncomplicated nature of these solutions motivates the numerical solution of a further simplified initial-value problem for both nonhydrostatic and hydrostatic flow. Exact analytic solutions are developed for the latter hydrostatic case, which explains the upstream-propagating wave of subsidence as a shock phenomenon.
Subject(s):Conditional instability, Gravity waves, Mesoscale processes, Nonlinear dynamics, Orographic effects, Differential equations
Peer Review:Refereed
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OpenSky citable URL: ark:/85065/d78g8mm0
Publisher's Version: 10.1175/JAS-D-13-051.1
Author(s):
  • David Muraki
  • Richard Rotunno - NCAR/UCAR
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