Large-scale Geodynamics Controls Secular Trend of the Total Ozone
Abstract:
We jointly analyzed the global distribution of ozone from TOMS satellite data, the surface of the earth’s core from seismic tomography, and lithospheric plate movements from GPS and concluded the following: (1) There are sources of energy in the solid earth which contribute to the atmospheric ozone; (2) The large-scale geodynamics should be considered among the mechanisms responsible for the global structure of ozonosphere and its evolution with time. We also note similarities in the pattern of ozone caused by sources in the solid earth (“terrestrial ozone”) and the patterns of geomagnetic and gravity fields.
The global morphology of terrestrial ozone suggests a “breakup” in the initial ozone distribution at about the same time as a breakup of Pangea and subsequent spreading of the area of higher ozone content. A restored initial breakup is located in the oceanic region and runs northwest to southeast across Africa. We propose a large-scale geodynamic process: a convective flow in the mantle from the earth’s core surface provokes the breakup of Pangea and the breakup of ozone distribution
