Variations of mesospheric equatorial ozone as observed by the Solar Maximum Mission

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

4

Equatorial Atmosphere, Mesosphere, Ozonometry, Solar Maximum Mission, Solar Terrestrial Interactions, Annual Variations, Atmospheric Chemistry, Secular Variations, Solar Flux, Sunset

Scientific paper

Tropical lower mesospheric ozone concentrations determined from UV sunset occultations demonstrate latitude dependent variations from 1985 through 1988. The annual and semiannual ozone behavior is caused primarily by equatorial temperature waves. Secular changes are the result of variations in mesospheric temperature, solar flux, and trace constituents which are involved in the ozone chemistry. The variation with latitude of the observed ozone trends between 1985 and 1989 is different from predictions of some models which simulate stratospheric and lower mesospheric ozone behavior over a sunspot cycle. This is the result of differences between the actual temperature structure of the atmosphere and that adopted in the models.

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

Variations of mesospheric equatorial ozone as observed by the Solar Maximum Mission 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 Variations of mesospheric equatorial ozone as observed by the Solar Maximum Mission, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Variations of mesospheric equatorial ozone as observed by the Solar Maximum Mission will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1887394

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