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INTERCONTINENTAL INFLUENCES ON OZONE AND AEROSOL AIR QUALITY Daniel J. Jacob Harvard University NO x emissions (2000) with Colette L. Heald, Rokjin Park, Rynda C. Hudman, Solene Turquety and support from NASA, NOAA, EPA, EPRI
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TREND IS TOWARD TIGHTER AIR QUALITY STANDARDS AOT40 ozone growing season standard for Europe: daytime ppb-hours above 40 ppbv over growing season Standards: 10,000 ppbh (forests) 3,000 ppbh (crops) … correspond to mean ozone concentration of 41-45 ppbv EMEP [2005] Current 8-h average ozone standards: 84 pppbv (U.S.), 55 ppbv (EU) AOT40
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REGIONAL HAZE RULE IN THE UNITED STATES: national parks to achieve “natural visibility” by 2064 clean daymoderately polluted day Acadia National Park, Maine visibility (deciviews) Schedule for implementation of Regional Haze Rule [U.S. EPA, 2001] 2004 2018 2064 Anthropogenic emissions (illustrative) YEAR
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U.S. VISIBILITY IMPAIRMENT BY ASIAN DUST STORMS Glen Canyon, Arizona clear dayApril 16, 2001: Asian dust! … anthropogenic pollution is transported together with the dust Colette Heald (Harvard) satellite data Aerosol optical depth (AOD)Carbon monoxide (CO) MODIS satellite datamodel (dust) model (sulfate) MOPITT satellite data
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PATHWAYS FOR INTERCONTINENTAL TRANSPORT Stohl and Eckhard [2004] Transparent arrows: transport in boundary layer below 2 km Colored arrows: transport in free troposphere
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TWO MODES OF INTERCONTINENTAL INFLUENCE AsiaN. America Europe Boundary layer Free troposphere liftingsubsidence boundary layer advection Tropopause HEMISPHERIC POLLUTION BACKGROUND “Direct” intercontinental transport Mixing Direct intercontinental transport: fast (~1 week) transport from source to receptor continent; either by boundary layer advection or by lifting to lower free troposphere followed by subsidence Hemispheric pollution: pollution mixes in free troposphere, affecting free tropospheric background, in turn affecting surface concentrations by subsidence 2 km
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GLOBAL DISTRIBUTION OF TROPOSPERIC OZONE OBSERVED FROM THE GOME SATELLITE INSTRUMENT X. Liu, Harvard SAO/CFA Mean JJA 1997 tropospheric columns (Dobson Units): circumpolar transport around northern midlatitudes pollution belt
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OZONE BACKGROUND AT NORTHERN MID-LATITUDES HAS A LARGE ANTHROPOGENIC COMPONENT Observations at free tropospheric mountain sites in Europe [Marenco et al., 1994] Preindustrial model ranges AOT40 std European 8-h std. stratospheric constribution 0 10 20 30 40 50 60 1870 1890 1910 1930 1950 1970 1990
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GEOS-Chem GLOBAL 3-D MODEL OF ATMOSPHERIC TRANSPORT AND CHEMISTRY driven by GEOS assimilated meteorological observations from NASA Global Modeling and Assimilation Office (GMAO); native resolution 1 o x1 o ( 2 o x2.5 o ), ~50 vertical levels cross-tropopause transport constrained globally from observations (400 Tg O 3 yr -1 ) Coupled tropospheric ozone-aerosol chemistry (~100 interacting species) Ozone precursors: Nitrogen oxides (NO x ): combustion, lightning, soils Methane: wetlands, agriculture, natural gas, coal mining Nonmethane volatile organic compounds (NMVOCs): vegetation, combustion, industry Carbon monoxide (CO): combustion, VOC oxidation Aerosols and precursors: Sulfur gases: combustion, oceans, volcanoes, biomass burning Nitrogen oxides Ammonia: agriculture, soils, biomass burning, oceans Organic carbon (OC): biomass burning, vegetation, industry Black carbon (BC): combustion Soil dust, sea salt
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MEAN SURFACE OZONE ENHANCEMENTS FROM ANTHROPOGENIC NO x AND NMVOC EMISSIONS IN DIFFERENT CONTINENTS GEOS-Chem model, July 1997 North America Europe Asia Li et al. [2002] as determined from sensitivity simulations with these sources shut off
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INTERCONTINENTAL OZONE ENHANCEMENTS ARE LARGER IN FREE TROPOSPHERE THAN AT SURFACE Mean GEOS-Chem ozone enhancements at 45 o N in summer from anthropogenic emissions of NO x and NMVOCs in different continents N America EuropeAsia N. American emissions European emissions Asian emissions Li et al. [2002]
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Fiore et al. [2002] SUMMERTIME VARIABILITY OF OZONE INTERCONTINENTAL POLLUTION ENHANCEMENT IN U.S. tropical air Subsidence of Asian pollution + local production stagnation Effect is maximum for ozone concentrations in mid-range (40-70 ppbv) GEOS-Chem summer statistics of surface afternoon ozone enhancements from Asian and European emissions over ensemble of U.S. surface sites
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EFFECT OF NORTH AMERICAN SOURCES ON EXCEEDANCES OF EUROPEAN AIR QUALITY STANDARD (55 ppbv, 8-h average) GEOS-CHEM model results, summer 1997 Number of exceedance days (out of 92) # of exceedance days that would not have been in absence of N.American emissions Li et al. [2002]
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PROBING TRANSPACIFIC POLLUTION TRANSPORT High-ozone Asian pollution plumes and stratospheric influence observed in lower free troposphere … but not at surface CO O3O3 PAN HNO 3 May 5 plume at 6 km: High CO and PAN, no O 3 enhancement May 17 subsiding plume at 2.5 km: High CO and O 3, PAN NO x HNO 3 Hudman et al. [2004] Observations by D. Parrish, J. Roberts, T. Ryesrson (NOAA/AL) NOAA/ITCT-2K2 aircraft campaign, April-May 2002
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CONCEPTUAL PICTURE OF OZONE PRODUCTION IN TRANSPACIFIC ASIAN POLLUTION PLUMES NO x HNO 3 PAN Asian boundary layer (OPE ~ 5) PAN, weak O 3 Warm conveyor belt; 5-10% export of NO y mainly as PAN strong O 3 Subsidence Over E Pacific OPE 60-80 PAN NO x HNO 3 U.S. boundary layer O 3 = 6 ± 2 ppbv (California) 10x dilution (Asian dust data) E. Asia Pacific United States Hudman et al. [2004] Stratospheric downwelling GEOS-CHEM ozone production efficiency (2-4 km)
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CALIFORNIA MOUNTAIN SITES ARE MOST SENSITIVE TO ASIAN OZONE POLLUTION …because there is less dilution Observed 8-h ozone at Sequoia National Park (1800 m) in May 2002 vs. corresponding simulated (GEOS-CHEM) Asian pollution ozone enhancement Asian enhancements are 6-10 ppbv during exceedances of standard; unlike at surface sites, Asian pollution influence is not minimum under high-ozone conditions! May 17 obs. Asian plume event in red Hudman et al. [2004]
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ICARTT: COORDINATED ATMOSPHERIC CHEMISTRY CAMPAIGN OVER EASTERN NORTH AMERICA AND NORTH ATLANTIC IN SUMMER 2004 International, multi-agency (U.S.) collaboration targeted at U.S. regional air quality, pollution outflow, transatlantic transport, aerosol radiative forcing Terra ERS MISR, MODIS, MOPITT ERS-2 GOME Envisat SCIAMACHY Aqua AIRS, MODIS NASA DC-8 UK BAE-143 DLR Falcon NOAA-P3 DOE G-1 NASA Proteus
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AIRS CO SATELLITE OBSERVATIONS OF INTERCONTINENTAL TRANSPORT DURING ICARTT Asian pollution U.S. pollution Alaskan fires Wallace McMillan (UMBC) Carbon monoxide (CO) columns on July 18
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ASIAN POLLUTION PLUME OVER EASTERN U.S. sampled by NASA aircraft on July 15 Observed O 3 = 20-40 ppbv, CO = 20 ppbv GEOS-Chem O 3 = 5-10 ppbv, CO = 10-20 ppbv High Halon-1211 in plume confirms Asian origin GEOS forecast Asian CO (9 km) Observed O 3 (ppbv) Observed CO (ppbv)
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TRANSPACIFIC TRANSPORT OF AEROSOLS Colette L. Heald, Harvard MODIS satellite observations of aerosol optical depth (AOD) in different seasons, and corresponding GEOS-Chem model simulations DJF MAM JJA SON MODIS AOD GEOS-CHEM AOD: Asian anthrop. Dust
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AIRCRAFT OBSERVATIONS IN ASIAN WARM CONVEYOR BELT (WCB) OUTFLOW ILLUSTRATE SCAVENGING OF AEROSOLS DURING LIFTING TO FREE TROPOSPHERE Longitude Data from E.V. Browell boundary layer outflow WCB outflow Ozone: WCB outflow Aerosols scavenged from WCB outflow TRACE-P campaign out of Hong Kong and Japan, spring 2001
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P3B DATA over NW Pacific (30 – 45 o N, 120 – 140 o E) SCAVENGING OF AEROSOLS INCLUDING BLACK CARBON (BC) APPARENT IN MEAN VERTICAL PROFILES Park et al. [2005] TRACE-P observations over NW Pacific and GEOS-Chem simulations Sulfate is most important exported anthropogenic aerosol in model
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MYSTERY ORGANIC AEROSOL IN HIGH-ALTITUDE ASIAN OUTFLOW ACE-Asia aircraft observations over Japan (spring 2001) Elemental carbon (EC) observed GEOS-Chem Organic carbon (OC) implies large secondary production in free troposphere not included in present models; Dominates aerosol loading in free troposphere; could produce large negative radiative forcing effect (~ 1W m -2 ) Colette Heald (Harvard) (A.D. Clarke)
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INTERCONTINENTAL TRANSPORT OF ASIAN AND NORTH AMERICAN ANTHROPOGENIC SULFATE As determined from GEOS-Chem 2001 sensitivity simulations with these sources shut off Intercontinental enhancements of anthropogenic sulfate over U.S. are of same order as interstate enhancement threshold used for regulation (0.2 g m -3 ) and higher than EPA estimates of natural values (0.1 g m -3 )
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VERTICAL STRUCTURE OF TRANSPACIFIC TRANSPORT GEOS-Chem model results for spring 2001 (15-45 o N) C.L. Heald, Harvard Asian CO Asian sulfate Asia N. America Asia N. America Asian aerosols are transported in lower free troposphere and subside over the NE Pacific; topography in western U.S. promotes contact with surface
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EVIDENCE OF ASIAN SULFATE IN IMPROVE NETWORK OF AEROSOL MEASUREMENTS AT U.S. SITES NW US: 0.72 μgm -3 NW US: 1.04 μgm -3 NW US: 0.60 μgm -3 spring 2001 mean 24-h seasonal max GEOS-Chem Asian influence NW US: 0.18 μgm -3 IMPROVE GEOS-CHEM Asian anthr (GEOS-Chem) March 1 April 1 May 1 June 1 Time series over NW U.S. (spring 01) IMPROVE data: spring 2001 mean days of GEOS-Chem 24-h seasonal max 1.4 g m -3
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Janus mission proposed to NASA: GLOBAL MAPPING OF ATMOSPHERIC COMPOSITION FROM L1 ORBIT Global mapping of tropospheric aerosols, clouds, NO 2, HCHO, SO 2, CO, CO 2 : observe transport on regional to global scales Continuous observation of Earth’s sunlit disk with 5 km nadir horizontal resolution
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