The Health Co-Benefits of Short-lived Climate Forcing Air Pollutants

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The Health Co-Benefits of Short-lived Climate Forcing Air Pollutants Michael Jerrett, PhD Professor, Environmental Health and Geographic Information Sciences School of Public Health UC Berkeley

Good News First: Co-Benefits Lancet Nov. 25, 2009

Shorter-Lived Climate Forcing Air Pollutants Many of the worst-case scenario predictions on greenhouse gas emissions have been surpassed already Difficulty in reducing long-lived carbon dioxide (CO2) has focused attention on short-lived climate forcers Reducing short-lived pollutants can have rapid impact on climate and yield large public health benefits

Global warming in 2005 due to all human emissions since 1750 IPCC, 2007 CO 2 is important for climate, Several of the non-co 2, but so are many other greenhouse gases create pollutants, including the ones a good proportion of both circled that, unlike CO 2, also their climate forcing and have significant health as health damage through well as climate impacts the secondary pollutant, tropospheric Nitrate, sulphate, ozone and organic carbon particles however, have cooling impacts on climate but are still health damaging

What are the Short-Lived Climate Forcers? Some are criteria air pollutants, already under regulatory control Major contributors are ozone (O3) and aerosols (black carbon - BC and sulfate - SO 4 ) Organic carbon also important, but is less studied (always co-emitted with BC complicates control) Climate effects, health effects, spatial distributions and equity issues are different for each pollutant Evidence base still far from complete, but the SLCF are attractive policy intervention targets

Slide Source: Carmichael et al. (2011)

Slide Source: Carmichael et al. (2011)

Approximate Residence Times Ozone usually hours to days (usually <20 days) Aerosols usually less than 10 days and can readily be removed by rain Means climate effects can occur quickly after reductions can buy us time!

Evidence of Long-term Health Effects from the USA American Cancer Society Subjects enrolled in 1982 1.2 million Follow up to 2000 ACS cohort with 352,000 subjects in 66 Metros (93,000 deaths) Central monitor data used per Metro Multilevel Cox model with 44 individual terms (smoking) and 14 ecologic terms (e.g. poverty in zip code area or MSA)

INDIVIDUAL LEVEL COVARIATES: Tobacco smoke variables: 1. Indicator variable for current cigarette smoker, 2. Indicator variable for pipe or cigar smoker, 3. Current smoker s years smoked, 4. Current smoker s years smoked squared, 5. Current smoker s cigarettes per day, 6. Current smoker s cigarettes per day squared, 7. Indicator variable for former cigarette smoker, 8. Former smoker s years smoked, 9. Former smoker s years smoked squared, 10. Former smoker s cigarettes per day, 11. Former smoker s cigarettes per day squared, 12. Indicator variables for starting smoking before or after age eighteen, 13. Number of hours per day exposed to passive cigarette smoke.

Education variables: Indicator variables for high school completed and more than high school completed, versus high school not completed Marital status variables: Indicator variables for single and other versus married BMI: BMI and BMI squared Alcohol consumption: Six variables including indicator variables for beer, liquor, and wine drinkers and nonresponders versus non-drinkers

Occupational exposure: A variable that indicated regular occupational exposure to asbestos, chemicals/acids/solvents, coal or stone dusts, coal tar/pitch/asphalt, diesel engine exhaust, or formaldehyde 9 additional indicator variables that reflected an occupational dirtiness index Diet: Quintile indicator variables for each of two diet indices that accounted for fat consumption an consumption of vegetables, citrus and high-fiber grains were derived based on information given in the enrollment questionnaire.

Long-term Ozone Across the US 1977-2000 1-hour Max

# # # # 30 25 20 N 15 10 5 0 San Francisco Seattle Los Angeles Salt Lake City Phoenix N =151 X 4.0 5.5 7.0 8.5 10.0 11.5 13.0 14.5 16.0 17.5 19.0 20.5 22.0 23.5 25.0 SO 4 [ugm -3 ] Modeled (Kriged) Sulfate (SO 4 ) Surface Billings Denver Oklahoma City Dallas Minneapolis Kansas City Houston Gary Memphis Detroit Nashville New Orleans Steubenville Atlanta Johnstown Tampa 500 0 500 1000 1500 Kilometers 500 0 500 1000 Miles New York Boston Washington Charleston Sulfate Cohort Loc'ns (151) Sulfate ( ) [ ] < 4.00 SO 4.00 4 - ugm 4.99 5.00-5.99 6.00-6.99 7.00-7.99 8.00-8.99 9.00-9.99 10.00-10.99 11.00-11.99 12.00-12.99 13.00-13.99 14.00-14.99 15.00-15.99 16.00-16.99 17.00-17.99 18.00-18.99 19.00-19.99 20.00-20.99 21.00-21.99 22.00-22.99 > 23.00

PM 2.5 Levels (1999-2000) 500 0 500 1000 1500 2000 2500 Kilometers 300 0 300 600 900 1200 1500 Miles ACS Cohort Cities -3 Modelled PM 2.5 Levels [ ug m ] > 19.00 18.51-19.00 18.01-18.50 17.51-18.00 17.01-17.50 16.51-17.00 16.01-16.50 15.51-16.00 15.01-15.50 14.51-15.00 14.01-14.50 13.51-14.00 13.01-13.50 12.51-13.00 12.01-12.50 11.51-12.00 11.01-11.51 10.51-11.00 10.01-10.50 9.51-10.00 9.01-9.50 8.51-9.00 8.01-8.50 7.51-8.00 7.01-7.50 < 7.00

Percent Increase in Excess Risk Due to Air Pollution (Cardiopulmonary Causes of Death) Percent Increase 10 8 6 4 2 0 PM2.5 Ozone Sulphate EC

Percent Increase in Excess Risk Due to Pollution in Multipollutant Models (Cardiopulmonary Causes of Death) Percent Increase 10 8 6 4 2 0-2 Ozone Sulphate EC

Evidence of Heat Interactions with Chronic Exposure

Bottom Line Epidemiological evidence suggests health effects from all the short-lived climate forcers Interpretation of multi-pollutant models complicated by high correlations (r ~ 0.6-0.7 among them) Many other studies implicate ozone and BC as contributors to many chronic diseases

Summary of Findings Climate Toxicology Epidemiology Sulfate Cooling Pure form not toxic Acute and longterm effects Organic Carbon Cooling Many forms toxic to varying degrees Acute and longterm effects Black Carbon Warming Pure form moderately toxic Acute and longterm effects Ozone Warming Pure form very toxic Acute and longterm effects

UN Assessment Published 2011 Major Assessment of All Impacts Indictes Significant Climate, Health, Ecosystem, Food Benefits

Regional Breakdown of Mortality Avoided

Climate Benefits Near Term

What are the Equity Considerations? Different for PM, BC, Sulfate and Ozone Spatial scales vary, source contributions and control strategies differ Populations affected are different regionally and within cities

PM2.5

Wealth and PM2.5 Air Pollution Exposure in Los Angeles ACS Study -- LA in Zip Areas ACS Study -- LA in Zip Areas PM2.5 in ug/m3 19 20 21 22 PM2.5 in ug/m3 18 19 20 21 10000 20000 30000 40000 Median Income in 1979 ACS Study -- LA at individual levels 0.0 0.2 0.4 0.6 0.8 1.0 Proportion of Household with Air conditioner ACS Study -- LA at individual levels PM2.5 in ug/m3 17 18 19 20 21 22 PM2.5 in ug/m3 16 17 18 19 20 21 10000 20000 30000 40000 Median Income in 1979 0.0 0.2 0.4 0.6 0.8 1.0 Proportion of Household with Air conditioner

Diesel PM NATA Ports

Sulfate in PM10

Ozone

Ozone Increases with Higher Temperatures

Equity Considerations Not well understood, but preliminary conclusions: 1. PM2.5 and BC tend to have a negative social gradient (worse for poor groups) 2. Ozone probably has a positive social gradient (worse for richer groups) 3. Sulfate more homogeneous locally, but regionally has a negative gradient

Conclusions SLCF have become major focus in climate change debates BC, sulfate and ozone all have health effects and potential co-benefits Reducing sulfate could accelerate warming, while reducing others will probably slow warming Equity dimension not well understood, but could be very different for BC, sulfate and ozone Controlling SLCFs is essential as a compliment to CO 2 reductions

Acknowledgements John Balmes, Kirk Smith, Seth Shonkoff (UC Berkeley), Andy Haines (London School of Tropical Medicine and Hygiene) California Air Resources Board, Health Effects Institute, National Institute of Environmental Health Science, Wellcome Trust

Heat and Air Pollution: Ozone Higher temperatures, strong sunlight and a stable air mass are ideal for formation of ground level ozone (O 3 ) Difficult to predict, but climate change likely to increase ozone concentrations globally In much of the US, a warming of 4 degrees (F) could increase O 3 concentrations by about 5% (US EPA)

Heat and Air Pollution Heat waves in Europe in summer 2003 provide a case study of heat-related O 3 impacts on public health During the heat waves thousands of excess deaths that occurred above the average recorded for that time of year Epidemiological studies of deaths suggest a substantial portion of the mortality attributable to elevated O 3 and particulate levels that occurred during the heat waves 20-50% of the total excess deaths can be attributed to elevated O 3 and particle levels (Filleul et al.;johnson et al.)

Ozone Concentrations Across the U.S.

Does Acute Ozone Exposure Interact with Heat? The results for confounding and/or effect modification by air pollutants on the temperature-mortality association remain mixed (Basu 2009) With increasing heat and ozone, important to understand interactions

Research Needs Toxicology and chamber studies examining effects of heat and ozone (or photochemical mixtures) to determine biology of dose-response under different heat conditions Need further epidemiological studies to understand ozone-dose response under hotter conditions More generally need better investigation of doseresponse shapes because co-benefits vary widely

Sources of Sulfur and Black Carbon

Research Needs What are the within-city distributions of ozone and black carbon? Are health effects different as scale of analysis focuses on smaller areas? What are the health effects of pollution mixtures associated with these pollutants? What is the global burden of disease from these pollutants?