Premium
Depletion of Arctic ozone in the winter 1990
Author(s) -
Koike M.,
Kondo Y.,
Hayashi M.,
Iwasaka Y.,
Newman P. A.,
Helten M.,
Aimedieu P.
Publication year - 1991
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 - 10.1029/91gl00467
Subject(s) - ozone , mixing ratio , ozone depletion , atmospheric sciences , polar vortex , environmental science , altitude (triangle) , mixing (physics) , arctic , nitric acid , vortex , meteorology , climatology , chemistry , oceanography , physics , geology , inorganic chemistry , geometry , mathematics , quantum mechanics
Ozone mixing ratios were measured by ozonesondes on board balloons launched from Esrange, near Kiruna, Sweden (68°N, 20°E) from January 11 to February 9, 1990. The data obtained prior to a sudden warming on February 7, 1990 show that at potential temperatures between 460 and 640 K, the ozone mixing ratio just inside the polar vortex was systematically smaller than that outside, the largest difference being 29 % at around 525 K. The ozone mixing ratio at 525 K inside the vortex decreased at a rate of about 1.5 % per day between January 26 and February 4. The temperatures simultaneously observed were quite often low enough to allow for formation of nitric acid trihydrate (NAT) particles around this altitude. Depletion of ozone due to highly perturbed chemical conditions in late January and early February is strongly suggested.