The stationary response to large-scale orography in a general circulation model and a linear model
Journal Article
·
· Journal of the Atmospheric Sciences; (United States)
- Geophysical Fluid Dynamics Laboratory/NOAA, Princeton, NJ (United States)
Stationary waves generated over orography in a linear model and a general circulation model (GCM) are compared to examine how the atmosphere's response is established for small mountains and how linear theory breaks down over large orographic features. Both models have nine vertical levels and are low-resolution (R15) spectral models. The linear model solves the stationary linear primitive equations. The GCM's control integration uses zonally uniform and hemispherically symmetric boundary conditions, with a global swamp surface. Five experiments are performed by perturbing the GCM with Gaussian mountains of various heights introduced in midlatitudes. The stationary wave model is linearized about zonal mean fields from the GCM climatology. The linear model's response to a Gaussian mountain at 45[degrees]N latitude is dominated by a single wave train radiating toward the southeast. For mountain heights between 0.7 an 2 km, the GCM's stationary waves are similar to the linear model response to orography, although amplitudes increase less rapidly than linearly with mountain height. For larger mountains, closed isentropes and distinctly nonlinear flow occur along the surface of the mountain and a large poleward-radiating wave train develops. The development of closed isentropes, and the breakdown of linear theory, can be predicted whenever the slope of the surface exceeds the slope of the isentropes in the unperturbed (no mountain) basic state. 19 refs., 29 figs.
- OSTI ID:
- 5583742
- Journal Information:
- Journal of the Atmospheric Sciences; (United States), Journal Name: Journal of the Atmospheric Sciences; (United States) Journal Issue: 6 Vol. 49:6; ISSN 0022-4928; ISSN JAHSAK
- Country of Publication:
- United States
- Language:
- English
Similar Records
Mechanisms of low-frequency variability in a simple model with orography
GCM response of northern winter stationary waves and storm tracks to increasing amounts of carbon dioxide
Linear simulation of the stationary eddies in a general circulation model. Part I. The no-mountain model
Journal Article
·
Sun Mar 14 23:00:00 EST 1993
· Journal of the Atmospheric Sciences; (United States)
·
OSTI ID:6438375
GCM response of northern winter stationary waves and storm tracks to increasing amounts of carbon dioxide
Journal Article
·
Fri Oct 01 00:00:00 EDT 1993
· Journal of Climate; (United States)
·
OSTI ID:5584118
Linear simulation of the stationary eddies in a general circulation model. Part I. The no-mountain model
Journal Article
·
Sun Nov 30 23:00:00 EST 1986
· J. Atmos. Sci.; (United States)
·
OSTI ID:6130851
Related Subjects
54 ENVIRONMENTAL SCIENCES
540110*
ATMOSPHERIC CIRCULATION
BOUNDARY CONDITIONS
COMPARATIVE EVALUATIONS
DIFFERENTIAL EQUATIONS
DISTURBANCES
EQUATIONS
EVALUATION
FLUID FLOW
FUNCTIONS
GAUSS FUNCTION
GENERAL CIRCULATION MODELS
MATHEMATICAL MODELS
METEOROLOGY
MOUNTAINS
PARTIAL DIFFERENTIAL EQUATIONS
STATISTICAL MODELS
TIME DEPENDENCE
VORTEX FLOW
WAVE EQUATIONS
540110*
ATMOSPHERIC CIRCULATION
BOUNDARY CONDITIONS
COMPARATIVE EVALUATIONS
DIFFERENTIAL EQUATIONS
DISTURBANCES
EQUATIONS
EVALUATION
FLUID FLOW
FUNCTIONS
GAUSS FUNCTION
GENERAL CIRCULATION MODELS
MATHEMATICAL MODELS
METEOROLOGY
MOUNTAINS
PARTIAL DIFFERENTIAL EQUATIONS
STATISTICAL MODELS
TIME DEPENDENCE
VORTEX FLOW
WAVE EQUATIONS