Sj. Reid et al., DISTRIBUTION OF OZONE LAMINAE DURING EASOE AND THE POSSIBLE INFLUENCEOF INERTIA-GRAVITY WAVES, Geophysical research letters, 21(13), 1994, pp. 1479-1482
The distribution of laminae in ozone has been determined from the EASO
E ozonesonde archive as a function of potential temperature and potent
ial vorticity. Results confirm previous studies that laminae are absen
t above approximately 450K within the vortex, and are most abundant ne
ar its edge. Observations of inertia-gravity waves in the lower strato
sphere appear to suggest that such waves are not of sufficiently large
amplitude to cause the kinds of laminae that are observed.