New evidence for ozone depletion in the upper stratosphere

Mathematics – Logic

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

9

Atmospheric Composition And Structure: Evolution Of The Atmosphere, Atmospheric Composition And Structure: Middle Atmosphere-Composition And Chemistry, Atmospheric Composition And Structure: General Or Miscellaneous, Meteorology And Atmospheric Dynamics: Climatology

Scientific paper

Differential absorption lidar measurements at the Meteorological Observatory Hohenpeissenberg between 1987 and 1993 show a statistically significant ozone decrease between 32 and 42 km, peaking at about -1.7% per year at 39 km altitude. This depletion is higher than reported by SAGE II or SBUV, yet the Hohenpeissenberg data agree very well with the results from Umkehr measurements. The observed ozone trend is in the upper range of predictions from photochemical models (-0.5 to -1.5 % per year), whereas SBUV and SAGE II results are close to the lower end of the simulations. The agreement with photochemical models indicates that the depletion is most likely caused by catalytic ozone destruction through anthropogenic chlorine.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

New evidence for ozone depletion in the upper stratosphere does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with New evidence for ozone depletion in the upper stratosphere, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and New evidence for ozone depletion in the upper stratosphere will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1024073

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.