Abstract
In situ observations of small-scale dynamics and compositional structure in the tropopause region are presented. The measurements were made aboard the Grob "Egrett" high-altitude research aircraft above Aberystwyth, Wales, in the summer of 2000. The observations presented here show evidence of mixing of ozone and water vapor in a patch of intense turbulence just above the tropopause. This turbulence is shown to be the result of wind shear above a tropospheric jet stream. The value of the vertical eddy diffusion coefficient in this turbulence is estimated to be 0.9 m2 s-1. It is also shown that wavelike perturbations superimposed on the overall tracer structure can be accounted for by a gravity wave.
Original language | English |
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Article number | 4084 |
Number of pages | 6 |
Journal | Journal of Geophysical Research: Atmospheres |
Volume | 107 |
Issue number | D10 |
DOIs | |
Publication status | Published - 27 May 2002 |
Keywords
- Aircraft measurements
- Atmospheric chemistry
- Jet stream
- Kelvin-Helmholtz instability
- Tropopausal turbulence
- Wave breaking