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Preindustrial-to-present-day radiative forcing by tropospheric ozone from improved simulations with the GISS chemistry-climate GCM

Publication ,  Journal Article
Shindell, DT; Faluvegi, G; Bell, N
Published in: Atmospheric Chemistry and Physics
January 1, 2003

Improved estimates of the radiative forcing from tropospheric ozone increases since the preindustrial have been calculated with the tropospheric chemistry model used at the Goddard Institute for Space Studies (GISS) within the GISS general circulation model (GCM). The chemistry in this model has been expanded to include simplified representations of peroxyacetylnitrates and non-methane hydrocarbons in addition to background NOx-HO x-Ox-CO-CH4 chemistry. The GCM has improved resolution and physics in the boundary layer, improved resolution near the tropopause, and now contains a full representation of stratospheric dynamics. Simulations of present-day conditions show that this coupled chemistry-climate model is better able to reproduce observed tropospheric ozone, especially in the tropopause region, which is critical to climate forcing. Comparison with preindustrial simulations gives a global annual average radiative forcing due to tropospheric ozone increases of 0.30 W/m2 with standard assumptions for preindustrial emissions. Locally, the forcing reaches more than 0.8 W/m 2 in parts of the northern subtropics during spring and summer, and is more than 0.6W/m2 through nearly all the Northern subtropics and mid-latitudes during summer. An alternative preindustrial simulation with soil NOx emissions reduced by two-thirds and emissions of isoprene, paraffins and alkenes from vegetation increased by 50% gives a forcing of 0.33 W/m2. Given the large uncertainties in preindustrial ozone amounts, the true value may lie well outside this range. © 2003 European Geosciences Union.

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Published In

Atmospheric Chemistry and Physics

DOI

EISSN

1680-7324

ISSN

1680-7316

Publication Date

January 1, 2003

Volume

3

Issue

5

Start / End Page

1675 / 1702

Related Subject Headings

  • Meteorology & Atmospheric Sciences
  • 3702 Climate change science
  • 3701 Atmospheric sciences
  • 0401 Atmospheric Sciences
  • 0201 Astronomical and Space Sciences
 

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ICMJE
MLA
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Shindell, D. T., Faluvegi, G., & Bell, N. (2003). Preindustrial-to-present-day radiative forcing by tropospheric ozone from improved simulations with the GISS chemistry-climate GCM. Atmospheric Chemistry and Physics, 3(5), 1675–1702. https://doi.org/10.5194/acp-3-1675-2003
Shindell, D. T., G. Faluvegi, and N. Bell. “Preindustrial-to-present-day radiative forcing by tropospheric ozone from improved simulations with the GISS chemistry-climate GCM.” Atmospheric Chemistry and Physics 3, no. 5 (January 1, 2003): 1675–1702. https://doi.org/10.5194/acp-3-1675-2003.
Shindell DT, Faluvegi G, Bell N. Preindustrial-to-present-day radiative forcing by tropospheric ozone from improved simulations with the GISS chemistry-climate GCM. Atmospheric Chemistry and Physics. 2003 Jan 1;3(5):1675–702.
Shindell, D. T., et al. “Preindustrial-to-present-day radiative forcing by tropospheric ozone from improved simulations with the GISS chemistry-climate GCM.” Atmospheric Chemistry and Physics, vol. 3, no. 5, Jan. 2003, pp. 1675–702. Scopus, doi:10.5194/acp-3-1675-2003.
Shindell DT, Faluvegi G, Bell N. Preindustrial-to-present-day radiative forcing by tropospheric ozone from improved simulations with the GISS chemistry-climate GCM. Atmospheric Chemistry and Physics. 2003 Jan 1;3(5):1675–1702.

Published In

Atmospheric Chemistry and Physics

DOI

EISSN

1680-7324

ISSN

1680-7316

Publication Date

January 1, 2003

Volume

3

Issue

5

Start / End Page

1675 / 1702

Related Subject Headings

  • Meteorology & Atmospheric Sciences
  • 3702 Climate change science
  • 3701 Atmospheric sciences
  • 0401 Atmospheric Sciences
  • 0201 Astronomical and Space Sciences