Difference between revisions of "Tropospheric Chemistry with Isoprene"
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(Created page with "=Tropospheric Chemistry with Isoprene - TropIsop= thumb|left|Telford ''et al'' ACP '''10''' 7117 (2010)[[Image:Pinatubo_c5h8_2.png|thumb|right|Telf…") |
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=Tropospheric Chemistry with Isoprene - TropIsop= |
=Tropospheric Chemistry with Isoprene - TropIsop= |
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− | [[Image:Pinatubo_c5h8_1.png|thumb|left|Telford ''et al'' ACP '''10''' 7117 (2010)]][[Image:Pinatubo_c5h8_2.png|thumb|right|Telford ''et al'' ACP '''10''' 7117 (2010)]] |
+ | [[Image:Pinatubo_c5h8_1.png|thumb|left|Difference in tropospheric column of isoprene caused by changes to emissions between 1990 and 1992 caused by the eruption of Mt. Pinatubo. This study was performed by nudging the model to ERA-40 re-analysis. Telford ''et al'' ACP '''10''' 7117 (2010)]][[Image:Pinatubo_c5h8_2.png|thumb|right|Difference in tropospheric column of OH caused by changes to emissions between 1990 and 1992 caused by the eruption of Mt. Pinatubo. This study was performed by nudging the model to ERA-40 re-analysis. Telford ''et al'' ACP '''10''' 7117 (2010)]] |
''55 species, 48 advected tracers, 164 reactions'' |
''55 species, 48 advected tracers, 164 reactions'' |
Latest revision as of 15:54, 12 August 2010
Tropospheric Chemistry with Isoprene - TropIsop
55 species, 48 advected tracers, 164 reactions
The addition of the Mainz Isoprene Mechanism to the Standard Tropospheric Chemistry scheme allows for more detailed studies of land-surface-climate interactions and this scheme can be run at decadal to centennial time scales. The scheme has 129 gas-phase reactions with 35 photolysis reactions and has emissions into 9 species, with isoprene oxidation considered. Emissions of isoprene are scaled to be diurnally varying.