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Ozone and aerosol observed by lidar in the Canadian Arctic during the winter of 1995/96
Author(s) -
Donovan D. P.,
Bird J. C.,
Whiteway J. A.,
Duck T. J.,
Pal S. R.,
Carswell A. I.,
Sandilands J. W.,
Kaminski J. W.
Publication year - 1996
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/96gl03230
Subject(s) - ozone , lidar , stratosphere , atmospheric sciences , aerosol , environmental science , climatology , ozone depletion , ozone layer , arctic , potential vorticity , the arctic , mixing ratio , meteorology , vorticity , oceanography , geology , vortex , geography , remote sensing
Lidar observations of stratospheric ozone made at Eureka (80.0°N, 86.42°W) during the 95/96 winter show substantial declines in ozone mixing ratios. Reductions in ozone levels of up to 40% between the 410 K and 580 K isentropic levels were observed between mid‐January and mid‐March. The correlation of the ozone data with potential vorticity and concurrent lidar observations of stratospheric aerosol is consistent with the claim that significant chemical depletion did occur.

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