Sentences with phrase «tropospheric ozone chemistry»

This is important for the light that it shines on tropospheric ozone chemistry («bad ozone») which is a contributing factor to global warming (albeit one which is about only about 20 % as important as CO2).

Not exact matches

Ozone climatology: Some chemistry / aerosol models will run with interactive stratospheric chemistry while others will prescribe ozone in the stratosphere and only run with detailed tropospheric chemiOzone climatology: Some chemistry / aerosol models will run with interactive stratospheric chemistry while others will prescribe ozone in the stratosphere and only run with detailed tropospheric chemiozone in the stratosphere and only run with detailed tropospheric chemistry.
There is considerable interest in a sun and NAM (and SAM) connections via UV / ozone chemistry and modulating Earth system flows — especially equator to pole stratospheric and tropospheric pathways.
In terms of atmospheric chemistry, a strong consensus was reached for the first time that science could predict the changes in tropospheric ozone in response to scenarios for CH4 and the indirect greenhouse gases (CO, NOx, VOC) and that a quantitative GWP for CO could be reported.
Further, within my field, atmospheric chemistry, we are very much focused on the other forcings; aerosol and tropospheric ozone, for instance.
Mickley, L.J., P.P. Murti, D.J. Jacob, J.A. Logan, D.M. Koch, and D. Rind, 1999: Radiative forcing from tropospheric ozone calculated with a unified chemistry - climate model.
Shindell, D.T., G. Faluvegi, and N. Bell, 2003: Preindustrial - to - present - day radiative forcing by tropospheric ozone from improved simulations with the GISS chemistry - climate GCM.
In contrast, predictions made by the chemistry - climate models indicate that, as a consequence of ozone recovery — a factor largely ignored by IPCC models — the tropospheric winds in the Southern Hemisphere may actually decelerate in the high latitudes and move toward the equator, potentially reversing the direction of climate change in that hemisphere.
a b c d e f g h i j k l m n o p q r s t u v w x y z