Based on chemical transport model studies, the RF from the increase in
stratospheric water vapour due to oxidation of CH4 is estimated to be +0.07 [± 0.05] W m — 2, with a low level of scientific understanding.
Not exact matches
Recent studies have shown a doubling of
stratospheric water vapour, likely from increasing atmospheric heights
due to global warming, overshooting thunderstorm tops from stronger tropical cyclones and mesoscale convective systems etc...
The difference is in the residence time, mainly
due to the lack of
water vapour: the
stratospheric injection of SO2 by the Pinatubo did last 2 - 3 years before the reflecting drops were large enough to fall out of the atmosphere.
Future climate change may cause either an increase or a decrease in background tropospheric ozone,
due to the competing effects of higher
water vapour and higher
stratospheric input; increases in regional ozone pollution are expected
due to higher temperatures and weaker circulation.