Trajectories of trace constituents in a strong flow around the polar vortex during the development of a midwinter warming

Details Trajectories of trace constituents in a strong flow around the polar vortex during the development of a midwinter warming Trajectories of trace constituents in a strong flow around the polar vortex during the development of a midwinter warming

Jan 1993

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993adspr..13..343p&link_type=abstract

Advances in Space Research, Volume 13, Issue 1, p. 343-350.

Computer Science

Scientific paper

Trajectories are computed for different heights in a stratospheric winter vortex, displaced from the pole by a developing warming.
It is shown that horizontal mixing and height-dependent vertical motions at the edge of the vortex will cause notches in originally undisturbed profiles of source gases.
During the CHEOPS-campaigns over Northern Scandinavia such profiles were measured and are compared with the computed backward trajectories.

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