Intercontinental Transport of Ozone Pollution in the Context of Global Change Shiliang Wu and Aditya Kumar Michigan Technological University International Conference on Ozone and Plants & HTAP meeting Beijing, China May 19, 2014 Global change and tropospheric ozone ∆ (strat. ozone recovery) ( ∆ (land use/land cover) ( STE ∆ (climate) ( O3 ∆ (anthro. emissions) ( Ozone precursors: Deposition Nitrogen oxides (NOx ≡ NO + NO2) Carbon monoxide (CO) Volatile organic compounds (VOCs) [WMO, 2006] Decreasing U.S. emissions in the past decade http://www.epa.gov/ttnchie1/trends/ Ozone measurement at Pico for 2001-2011 75 Ozone mixing ratio (ppbv) 65 55 45 35 25 15 6/23/2000 11/5/2001 3/20/2003 8/1/2004 12/14/2005 4/28/2007 Date 9/9/2008 1/22/2010 6/6/2011 10/18/2012 Statistical analysis of the Pico data Ct = daily average concentrations of CO or O3 at Pico t = days since the reference time (e.g., Jan 1, 2001) a0, a1, a2, a3 = Regression coefficients et = Residual from the regression model Null Hypothesis: No significant trends exist at Pico for CO & O3 (i.e. a1=0) Statistical analysis of the Pico data 75 2001-2011 trend analysis of ozone measured at Pico (North Atlantic) Ozone concentration (ppbv) 65 55 45 35 25 15 6/23/2000 3/20/2003 12/14/2005 Date 9/9/2008 6/6/2011 [Kumar et al., 2013] a1: - 0.21 ppb/yr P-value: 0.0001 Ozone trends at other remote sites (2001-2012) [based on data from the World Data Center for Greenhouse Gases] [Very preliminary analysis!] Ozone trend at South Pole (Antarctica) for the past decades Period Trend (ppbv/year) P-value Significance R2 1975-2000 - 0.117 < 0.0001 Significant 0.62 2001-2012 + 0.086 < 0.0001 Significant 0.68 1975-2000 2001-2012 Changes in surface ozone (annual mean) due to 2000-2050 changes in anthropogenic emissions and climate [Wu et al., 2008] Climate-driven changes in vegetation for 2000-2050 Tropical broadleaf evergreen Tropical broadleaf raingreen Temp. broadleaf evergreen Temp. broadleaf summergreen Boreal needleleaf evergeern +17% Boreal summergreen Temp. needleleaf evergreen C3 perennial grass -9% C4 perennial grass Changes in JJA O3 due to land use/land cover change 2000 2100 – 2050 2050 – 2000 2100 – 2000 [Wu et al., 2012] Changes in intercontinental transport of ozone from Asia due to strat. ozone recovery (JJA) Control sensitivity – control Sensitivity (w/ strat. O3 recovery) Sensitivity / control [Zhang et al., 2014] Ozone trend at South Pole (Antarctica) for the past decades Period Trend (ppbv/year) P-value Significance R2 1975-2000 - 0.117 < 0.0001 Significant 0.62 2001-2012 + 0.086 < 0.0001 Significant 0.68 1975-2000 2001-2012 Inter-comparison to various factors in affecting the future evolution of surface ozone (ppb; JJA) Effects from ∆(anthro. emissions) [Wu et al. 2008] Effects from ∆(land use/land cover) [Wu et al. 2012] Effects from ∆(climate) [Wu et al. 2008] Effects from ∆(strat. O3 column) Acknowledgement Huanxin Zhang, Richard Honrath, and Mark Weise @ Michigan Tech; Loretta Mickley and Daniel Jacob @ Harvard University; Jed Kaplan @ University of Lausanne; Funding support from U.S. EPA (grant 83518901) and NSF (grant 1313755).
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