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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 17, issue 1
Ann. Geophys., 17, 115–121, 1999
https://doi.org/10.1007/s00585-999-0115-4
© European Geosciences Union 1999
Ann. Geophys., 17, 115–121, 1999
https://doi.org/10.1007/s00585-999-0115-4
© European Geosciences Union 1999

  31 Jan 1999

31 Jan 1999

Inertia-gravity waves in the troposphere and lower stratosphere associated with a jet stream exit region

L. Thomas, R. M. Worthington, and A. J. McDonald L. Thomas et al.
  • Department of Physics, University of Wales, Aberystwyth, Ceredigion SY23 3BZ, UK

Abstract. Radar measurements at Aberystwyth (52.4° N, 4.1° W) of winds at tropospheric and lower stratospheric heights are shown for 12-13 March 1994 in a region of highly curved flow, downstream of the jet maximum. The perturbations of horizontal velocity have comparable amplitudes in the troposphere and lower stratosphere with downward and upward phase propagation, respectively, in these two height regions. The sense of rotation with increasing height in hodographs of horizontal perturbation velocity derived for hourly intervals show downwards propagation of energy in the troposphere and upward propagation in the lower stratosphere with vertical wavelengths of 1.7 to 2.3 km. The results indicate inertia-gravity waves propagating in a direction similar to that of the jet stream but at smaller velocities. Some of the features observed contrast with those of previous observations of inertia-gravity waves propagating transverse to the jet stream. The interpretation of the hodographs to derive wave parameters has taken account of the vertical shear of the background wind transverse to the direction of wave propagation.

Key words. Meteorology and atmospheric dynamics (mesoscale meteorology; middle atmosphere dynamics; waves and tides)

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