Open AccessEffects of stratosphere‐troposphere chemistry coupling on tropospheric ozone
Author(s) -
Tian Wenshou,
Chipperfield Martyn P.,
Stevenson David S.,
Damoah Richard,
Dhomse Sandip,
Dudhia Anu,
Pumphrey Hugh,
Bernath Peter
Publication year - 2010
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2009jd013515
Subject(s) - stratosphere , troposphere , atmospheric sciences , ozone , tropospheric ozone , atmospheric chemistry , ozone layer , environmental science , atmospheric sounding , total ozone mapping spectrometer , climatology , meteorology , geology , physics
A new, computationally efficient coupled stratosphere‐troposphere chemistry‐climate model (S/T‐CCM) has been developed based on three well‐documented components: a 64‐level general circulation model from the UK Met Office Unified Model, the tropospheric chemistry transport model (STOCHEM), and the UMSLIMCAT stratospheric chemistry module. This newly developed S/T‐CCM has been evaluated with various observations, and it shows good performance in simulating important chemical species and their interdependence in both the troposphere and stratosphere. The modeled total column ozone agrees well with Total Ozone Mapping Spectrometer observations. Modeled ozone profiles in the upper troposphere and lower stratosphere are significantly improved compared to runs with the stratospheric chemistry and tropospheric chemistry models alone, and they are in good agreement with Michelson Interferometer for Passive Atmospheric Sounding satellite ozone profiles. The observed CO tape recorder is also successfully captured by the new CCM, and ozone‐CO correlations are in accordance with Atmospheric Chemistry Experiment observations. However, because of limitations in vertical resolution, intrusion of CO‐rich air in the stratosphere from the mesosphere could not be simulated in the current version of S/T‐CCM. Additionally, the simulated stratosphere‐to‐troposphere ozone flux, which controls upper tropospheric OH and O 3 concentrations, is found to be more realistic in the new coupled model compared to STOCHEM.