Much work is being done on improving the realism of such effects — particularly
through ozone chemistry (which enhances the signal), and aerosol pathways (which don't appear to have much of a global effect i.e. Dunne et al. (2016)-RRB-.
Not exact matches
Through extensive modeling of stratospheric
chemistry, the team found that calcite, a constituent of limestone, could counter
ozone loss by neutralizing emissions - borne acids in the atmosphere, while also reflecting light and cooling the planet.
The balance of oxygen isotopes within
ozone are strikingly weird with enrichment of heavy isotopes
through a physical chemical phenomenon first described by co-author Mark Thiemens, a professor of
chemistry at UC San Diego, and colleagues 25 years ago.
This in turn has been linked to solar UV /
ozone chemistry translated
through atmospheric pathways to polar surface pressure.