The influence of ozone precursor emissions from four world regions on tropospheric composition and radiative climate forcing
Ozone (Oâ) precursor emissions influence regional and global climate and air quality through changes in tropospheric Oâ and oxidants, which also influence methane (CHâ) and sulfate aerosols (SOâ²â»). We examine changes in the tropospheric composition of Oâ, CHâ, SOâ²⻠and global net radiative forcing (RF) for 20% reductions in global CHâ burden and in anthropogenic Oâ precursor emissions (NOx, NMVOC, and CO) from four regions (East Asia, Europe and Northern Africa, North America, and South Asia) using the Task Force on Hemispheric Transport of Air Pollution Source-Receptor global chemical transport model (CTM) simulations, assessing uncertainty (mean ± 1 standard deviation) across multiple CTMs. We evaluate steady state Oâ responses, including long-term feedbacks via CHâ. With a radiative transfer model that includes greenhouse gases and the aerosol direct effect, we find that regional NOx reductions produce global, annually averaged positive net RFs (0.2 ± 0.6 to 1.7 ± 2 mWmâ»Â²/Tg N yrâ»1), with some variation among models. Negative net RFs result from reductions in global CHâ (â162.6 ± 2 mWmâ»Â² for a change from 1760 to 1408 ppbv CHâ) and regional NMVOC (â0.4 ± 0.2 to â0.7 ± 0.2 mWmâ»Â²/Tg C yrâ»1) and CO emissions (â0.13 ± 0.02 to â0.15 ± 0.02 mWmâ»2/Tg CO yrâ»1). Including the effect of Oâ on COâ uptake by vegetation likely makes these net RFs more negative by â1.9 to â5.2 mWmâ»Â²/Tg N yrâ»1, â0.2 to â0.7 mWmâ»Â²/Tg C yrâ»1, and â0.02 to â0.05 mWmâ»Â²/Tg CO yrâ»1. Net RF impacts reflect the distribution of concentration changes, where RF is affected locally by changes in SOâ²â», regionally to hemispherically by Oâ, and globally by CHâ. Global annual average SOâ²⻠responses to oxidant changes range from 0.4 ± 2.6 to â1.9 ± 1.3 Gg for NOx reductions, 0.1 ± 1.2 to â0.9 ± 0.8 Gg for NMVOC reductions, and â0.09 ± 0.5 to â0.9 ± 0.8 Gg for CO reductions, suggesting additional research is needed. The 100-year global warming potentials (GWPâââ) are calculated for the global CHâ reduction (20.9 ± 3.7 without stratospheric Oâ or water vapor, 24.2 ± 4.2 including those components), and for the regional NOx, NMVOC, and CO reductions (â18.7 ± 25.9 to â1.9 ± 8.7 for NOx, 4.8 ± 1.7 to 8.3 ± 1.9 for NMVOC, and 1.5 ± 0.4 to 1.7 ± 0.5 for CO). Variation in GWPâââ for NOx, NMVOC, and CO suggests that regionally specific GWPs may be necessary and could support the inclusion of Oâ precursors in future policies that address air quality and climate change simultaneously. Both global net RF and GWPâââ are more sensitive to NOx and NMVOC reductions from South Asia than the other three regions.
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https://n2t.org/ark:/85065/d78w3dz7
eng
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publication
2016-01-01T00:00:00Z
publication
2012-04-13T00:00:00Z
Copyright 2012 American Geophysical Union.
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