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Mountain waves (Mountain-induced clouds). Hydraulic jump or rotor clouds in the Owens Valley Looking south on east side of Sierras; photo by glider.

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Presentation on theme: "Mountain waves (Mountain-induced clouds). Hydraulic jump or rotor clouds in the Owens Valley Looking south on east side of Sierras; photo by glider."— Presentation transcript:

1 Mountain waves (Mountain-induced clouds)

2

3 Hydraulic jump or rotor clouds in the Owens Valley Looking south on east side of Sierras; photo by glider pilot Robert Symons

4 Lenticular clouds http://www.photolib.noaa.gov/historic/nws/wea00108.htm

5 Lenticular clouds over Lake Tahoe (photo by RGF)

6 Lenticular clouds http://www.photolib.noaa.gov/historic/nws/wea00010.htm

7 Lenticular/cap/banner clouds over Mt. Rainier http://www.phototripusa.com/images/rwarfield/rw_3843_12.html

8 Lee waves forced by the Appalachians 13 April 2007

9 Lee waves downwind of Rockies 17 March 2005

10 Lee waves in Nevada 17 March 2005

11 Lee waves on Mars http://www.solarviews.com/raw/mars/leewave.gif

12 Background on gravity waves and pendulum equations

13 An oscillating parcel in a stable environment z’ = parcel vertical displacement N = Brunt-Vaisalla frequency Assumed solution: wavy in time… Result: where

14 Environmental response to oscillating parcels Assumed solution wavy in time & space where

15 Gravity wave frequency equation Two waves - opposite directions Period shorter in more stable environment Horizontal phase speeds Still proportional to N

16 DTDM animation input_strfcn_isolated_nowind.txt

17 Phase line tilt with height Westward wave tilts westward with height; Eastward wave tilts eastward Tilt implies vertical propagation

18 Adding a mean flow (constant w/ height) Owing to mean flow, one wave speeds up, one slows down Mountain waves are horizontally stationary gravity waves

19 Mountain wave analysis Adiabatic, Boussinesq, inviscid –But linearize about a mean state with wind, as well as vertical shear and even curvature shear, so –Assume locally steady state

20 Mountain wave equation l 2 = Scorer parameter

21 Cases to be examined Sinusoidal terrain –l 2 constant with height – flow with constant stability and mean wind –l 2 variable with height Isolated mountain Conditions for wave trapping leading to lenticular clouds

22 l 2 < k 2 Narrow mountain Waves decay w/ z l 2 > k 2 Wide mountain Waves preserved w/ z, mimic mountain shape Sinusoidal mountain

23 Isolated ridge Narrow mountain wide mountain l 2 < k 2 l 2 > k 2

24 More stable layer below - trapped lee waves & lenticular/lee wave clouds


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