Abstract
The ozone fluxes and flux convergences within the region between 30 and 0.4 mbar for the Northern Hemisphere are investigated for the period January 1 to March 31, 1979, using Nimbus 7 solar backscatter ultraviolet ozone profiles and the meteorological data derived from NOAA satellites. The results indicate that large contributions to the ozone transport and the transport convergence are due to mean vertical advection and horizontal eddy processes. The contribution from the vertical eddies is insignificant.-from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 5745-5755 |
| Number of pages | 11 |
| Journal | Journal of Geophysical Research Atmospheres |
| Volume | 90 |
| Issue number | D3 |
| DOIs | |
| State | Published - 1985 |
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