Energy Flux and Wavelet Diagnostics of Secondary Mountain Waves

In recent years aircraft data from mountain waves have been primarily analyzed using velocity and temperature power spectrum and momentum flux estimation Herein it is argued that energy flux wavelets (i e pressure velocity wavelet cross spectra) provide a more powerful tool for locating and classifying different types of mountain waves In the first part of the paper pressure velocity cross spectra using various linear mountain wave solutions are shown to be capable of disentangling collocated waves with different propagation directions and wavelength A field of group velocity vectors can also be determined In the second part the energy flux wavelet technique is applied to five cases of mountain waves entering the stratosphere from the Terrain Induced Rotor Experiment (T REX) in 2006 Perturbation pressure along the flight track is determined using aircraft static pressure corrected hydrostatically with GPS altitude In four of the cases collocated long up propagating and short down propagating waves are seen in the stratosphere These waves have strong but opposite p'w' cospectra In one of these cases a patch of turbulence is col located with the up and down waves In two other cases trapped waves riding on the tropopause inversion layer (TIL) are seen These trapped waves have p w quadrature spectia that reverse sign across the tropopause These newly discovered wave types may arise from secondary wave generation (i e a nonlinear transfer of energy from the long vertically propagating waves to shorter modes)