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Evidence for in situ generated atmospheric gravity waves associated with astratospheric temperature enhancement (STE) are presented. The signatures oftwo sets of gravity waves are observed by molecular-aerosol lidar inconjunction with the early December 2000 STE event above Sondrestrom,Greenland. The first set of gravity waves shows downward phase progressionwith a vertical wavelength of ~8 km while the second set shows upwardphase progression with a vertical wavelength of ~9 km. With estimatesof the background wind fields from synoptic analyses, the various intrinsicgravity wave parameters of these two wave structures are found. The observedwave features compare well to previous numerical modeling predictions

Observations of in-situ generated gravity waves during a stratospheric temperature enhancement (STE) event