Effect of 2000-2050 global change on U.S. ozone air quality
Shiliang Wu
Loretta J. Mickley
Daniel J. Jacob
Eric M. Leibensperger
David Rind (NASA/GISS)
David G. Streets (ANL)
GEOS-Chem users’ meeting, 2007/04
work supported by the EPA-STAR program
GCAP
Background - We are facing rapid global change
IPCC [2007]
2000
2050
2000
2050
IPCC
A1B
scenario
(-40%)
(+90%)
Models and future scenarios
Chemistry, transport, deposition, etc
GHG
Air pollutants & their precursors
Climate Change
GISS GCM III
23 vertical layers extending to 85 km
Horizontal resolution of 4º x 5º
GEOS-Chem
detailed ozone-NOx-VOC-aerosol chemistry
Anthropogenic emissions (IPCC A1B scenario)
Natural emissions
Radiative forcing
| 2000 | 2050 | change |
NOx-lightning, Tg N/yr | 4.9 | 5.8 | +18% |
NOx - soil, Tg N/yr | 6.1 | 6.6 | +8% |
Isoprene, Tg C/yr | 430 | 537 | +25% |
Effects of 2000-2050 global change on tropospheric ozone
(annual zonal mean)
+3%
+17%
+20%
Effects of 2000-2050 global change on U.S. ozone air quality
2000 conditions
2050 climate – 2000
2050 emission – 2000
2050 – 2000
Daily max 8h-avg ozone averaged over JJA (ppb)
Increase of summer max-8h-avg ozone by 1-5 ppb in large areas of U.S. due to 2000-2050 climate change.
Less effects in western U.S. because (1) anthro. emissions there are low (2) increase of ozone from intercontinental transport.
Factors causing worse O3 AQ with the future climate
Mixing depth (2050 / 2000)
Summer surface T. (2050 – 2000)
Convective mass flux (2050-2000)
What’s more: decrease of cyclone frequency
2000 climate 2050 climate
1999-2001
2049-2051
Eric M. Leibensperger, Harvard
Climate change has most effects on pollution events
Cumulative probability (%)
Max. 8-hr-avg ozone
2000s condition
2050s climate
2050s emissions
2050s climate & emis
median
99th percentile
Mitigation of climate penalty by emission reductions in ozone precursors
“climate change penalty” for ozone AQ = Δ[O3] from climate change
Reductions of anthropogenic emissions significantly mitigate the “climate penalty” and can even turn it into a “climate benefit” in southeast and northwest U.S.
(a) 2000 emissions
(b) 2050 emissions
Change of summer average max-8h ozone due to climate change
Conclusions
2000–2050 global change would make fresh air more luxury in the United States.
Effects on annual mean afternoon surface O3