P5M.4
Nonhydrostatic mountain waves in flows with directional wind shear
James Doyle, NRL, Monterey, CA; and Q. Jiang
Three research aircraft were deployed to observe modest-amplitude gravity waves over the southwestern French Alps on 13 November 1999 during the Mesoscale Alpine Programme (MAP). Radiosonde ascents and upstream GPS dropsondes deployed by research aircraft indicate the flow was characterized by topographic blocking and stagnation below 2500 m and low-level directional wind shear that extends above mountain top.
The in situ vertical velocity data from the NCAR Electra and backscatter from the downlooking SABL indicated the presence of gravity waves at 5500 m that were characterized by relatively short horizontal wavelengths of approximately 8 km. Backscatter data from the downlooking DIAL lidar onboard the DLR Falcon and in situ vertical velocity data from the aircraft transects indicate that a rapid decrease in the wave amplitude with height was present in the 5.5-6.5 km layer. Factors that may contribute to the rapid decay of wave amplitude include: decrease in the Scorer parameter with height that results in trapped waves, gravity wave breaking in the shear layer, and a directional critical level partially absorbs wave energy.
Numerical simulation results from COAMPS using a horizontal resolution of 556 m are in general agreement with the in situ aircraft and lidar observations. Low-level topographic blocking results in a reduction of the amplitude and dominant horizontal wavelength of the mountain waves. Relative roles of the directional critical level and the wave trapping are explored using linear analytic solutions with a reference state based on composite upstream dropsonde data. Linear theory and nonlinear model results indicate that the absorption of wave energy associated with the directional critical levels has an important impact on the wave characteristics and momentum flux.
Poster Session 5M, Orographic & Coastal Circulation
Thursday, 27 October 2005, 1:15 PM-3:00 PM, Alvarado F and Atria
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