The stratospheric ozone layer above Spitsbergen in winter 1989

Details The stratospheric ozone layer above Spitsbergen in winter 1989 The stratospheric ozone layer above Spitsbergen in winter 1989

Mar 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990georl..17..321n&link_type=abstract

Geophysical Research Letters, Supplement (ISSN 0094-8276), vol. 17, March 1990, p. 321-324. Research supported by BMFT.

Computer Science

Sound

12

Optical Radar, Ozonometry, Ozonosphere, Spitsbergen (Norway), Stratospheric Warming, Balloon-Borne Instruments, Ozone Depletion, Winter

Scientific paper

Ozone soundings are performed from Spitzbergen (79 N, 12 E) by an ozone LIDAR and balloon sondes. The development of the ozone layer from January until the end of March 1989 shows no major depletion, but a significant increase in mid-February due to the stratospheric warming. In March, a secondary concentration maximum occurred above the tropopause.

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