Not exact matches
Tropospheric ozone — a greenhouse gas and the kind that affects the air we breathe — can increase in
concentration because of atmospheric conditions, or can result from human activities.
«We use 1280 years of control simulation, with constant preindustrial forcings including constant specified CO2, and a five - member ensemble of historical simulations from 1850 — 2005 including prescribed historical greenhouse gas
concentrations, SO2 and other aerosol - precursor emissions, land use changes, solar irradiance changes,
tropospheric and stratospheric
ozone changes, and volcanic aerosol (ALL), following the recommended CMIP5 specifications.
The change in total solar irradiance over recent 11 - year sunspot cycles amounts to < 0.1 %, but greater changes at ultraviolet wavelengths may have substantial impacts on stratospheric
ozone concentrations, thereby altering both stratospheric and
tropospheric circulation patterns... This model prediction is supported by paleoclimatic proxy reconstructions over the past millennium.
However, the use of this term is not uniform when discussing stabilisation targets as some authors define carbon dioxide equivalent
concentrations as the net forcing of all anthropogenic radiative forcing agents including greenhouse gases,
tropospheric ozone, and aerosols but not natural forcings.
While others have looked at how changes in climate and in carbon dioxide
concentrations may affect vegetation, Reilly and colleagues added to that mix changes in
tropospheric ozone.
--
ozone is a strong driver of stratospheric temperature variations and
ozone concentrations are not constant — the variation of the stratospheric temperature is different on different altitudes — in the 60 - 80 the
tropospheric temperatures went down but the stratospheric temperatures didn't go up.
Methane enhances its own lifetime through changes in the OH
concentration: it leads to changes in
tropospheric ozone, enhances stratospheric water vapour levels, and produces CO2.