Global atmospheric changes and future impacts on regional air quality

Slides:



Advertisements
Similar presentations
Air Pollution and Climate
Advertisements

The other Harvard 3-D model: CACTUS Chemistry, Aerosols, Climate: Tropospheric Unified Simulation Objective: to improve understanding of the interaction.
QUESTIONS 1.Is hexane more or less reactive with OH than propane? 2.Is pentene or isoprene more reactive with OH?
Climate change, fires, and carbon aerosol over N. America with preliminary detour to discuss GCAP model development (GCAP= Global change and air pollution)
Chemistry-climate interactions: a new direction for GEOS-CHEM GEOS-CHEM research to date GCAP project Current project: drive GEOS-CHEM into.
SETTING THE STAGE FOR: BIOSPHERE, CHEMISTRY, CLIMATE INTERACTIONS.
GEOS-CHEM GLOBAL 3-D MODEL OF TROPOSPHERIC CHEMISTRY Assimilated NASA/DAO meteorological observations for o x1 o to 4 o x5 o horizontal resolution,
ATMOSPHERIC CHEMISTRY: FROM AIR POLLUTION TO GLOBAL CHANGE AND BACK Daniel J. Jacob.
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
Atmospheric chemistry Day 5 Ozone and air quality Air quality and climate change.
FROM AIR POLLUTION TO GLOBAL CHANGE AND BACK: Towards an integrated international policy for air pollution and climate change Daniel J. Jacob Harvard University.
Joshua Fu, Yun-Fat Lam* and Yang Gao University of Tennessee Daniel Jacob, Loretta Mickley and Shiliang Wu Harvard University Oct 20, 2009 The effects.
Application of a unified aerosol-chemistry-climate GCM to understand the effects of changing climate and global anthropogenic emissions on U.S. air quality.
INTERACTIONS OF AIR POLLUTION AND CLIMATE CHANGE Daniel J. Jacob How do air pollutants contribute to climate change? How will climate change affect air.
Report available from Workshop held in Washington, DC, April 27-29, 2005 Daniel J. Jacob (chair),
TROPOSPHERIC CHEMISTRY: FROM AIR POLLUTION TO GLOBAL CHANGE AND BACK Daniel J. Jacob.
E.A. Mathez, 2009, Climate Change: The Science of Global Warming and Our Energy Future, Columbia University Press. Source: Solomon et al., 2007 Chapter.
QUESTIONS 1.Is hexane more or less reactive with OH than propane? 2.Is pentene or isoprene more reactive with OH? 3.Using the EKMA diagram (the ozone isopleth.
INTERCONTINENTAL TRANSPORT OF OZONE AND ITS SEASONAL VARIATIONS IN EUROPE Dick Derwent rdscientific 2 nd ICAP Workshop Chapel Hill, North Carolina October.
OVERVIEW OF ATMOSPHERIC PROCESSES: Daniel J. Jacob Ozone and particulate matter (PM) with a global change perspective.
Loretta J. Mickley, Harvard University Shiliang Wu, Eric Liebensperger, Moeko Yoshitomi, Dominick Spracklen, Brendan Field Daniel Jacob, David Rind, Cynthia.
REGIONAL/GLOBAL INTERACTIONS IN ATMOSPHERIC CHEMISTRY Greenhouse gases Halocarbons Ozone Aerosols Acids Nutrients Toxics SOURCE CONTINENT REGIONAL ISSUES:
Climatic implications of changes in O 3 Loretta J. Mickley, Daniel J. Jacob Harvard University David Rind Goddard Institute for Space Studies How well.
The Pollution-Climate Connection How climate change could affect pollution episodes in the United States: a model study Loretta J. Mickley, Harvard University.
CHARGE QUESTIONS: ENDPOINTS  anthropogenic emissions   air pollution   climate OK, but can we be more specific?  Intercontinental transport of.
GCAP (Global Climate and Air Pollution): One of six projects funded by EPA-STAR to study effect of climate change on air quality. Collaborators: Harvard.
The Double Dividend of Methane Control Arlene M. Fiore IIASA, Laxenburg, Austria January 28, 2003 ANIMALS 90 LANDFILLS 50 GAS 60 COAL 40 RICE 85 TERMITES.
ORIGIN OF BACKGROUND OZONE IN SURFACE AIR OVER THE UNITED STATES: CONTRIBUTION TO POLLUTION EPISODES Daniel J. Jacob and Arlene M. Fiore Atmospheric Chemistry.
FIVE CHALLENGES IN ATMOSPHERIC COMPOSITION RESEARCH 1.Exploit satellite and other “top-down” atmospheric composition data to quantify emissions and export.
Background ozone in surface air over the United States Arlene M. Fiore Daniel J. Jacob US EPA Workshop on Developing Criteria for the Chemistry and Physics.
Why care about methane Daniel J. Jacob. Global present-day budget of atmospheric methane Wetlands: 160 Fires: 20 Livestock: 110 Rice: 40 Oil/Gas: 70 Coal:
Ozone Budget From: Jacob. Ozone in the Atmosphere Lifetime: –~1 month –Highly variable – dependent on season, latitude, altitude, etc. Background concentrations:
TROPOSPHERIC OZONE AS A CLIMATE GAS AND AIR POLLUTANT: THE CASE FOR CONTROLLING METHANE Daniel J. Jacob with Loretta J. Mickley, Arlene M. Fiore, Yaping.
Chemistry-climate interactions in CCSM
AIR QUALITY & AIR POLLUTION
Atmospheric Processes and Composition:
Frank Dentener, PhD Terry Keating, PhD EC JRC U.S. EPA
Linking regional air pollution with global chemistry and climate:
Daniel J. Jacob Harvard University
Mingwei Li Department of Earth, Atmospheric and Planetary Sciences
Impact of Solar and Sulfate Geoengineering on Surface Ozone
The Climate Change – Urban Pollution Relationship
Distribution and Trends: Impacts on Climate and Ozone Air Quality
Ozone Trends along U.S. West Coast
Global Change and Air Pollution
INTERCONTINENTAL TRANSPORT EXPERIMENT – NORTH AMERICA (INTEX-NA)
INTERCONTINENTAL TRANSPORT OF TROPOSPHERIC OZONE AND PRECURSORS AT NORTHERN MIDLATITUDES: IMPLICATIONS FOR SURFACE AIR QUALITY AND GLOBAL CHANGE Daniel.
TROPOSPHERIC OZONE AND OXIDANT CHEMISTRY
Randall Martin Aaron Van Donkelaar Daniel Jacob Dorian Abbot
Chemistry, Aerosols, and Climate: Tropospheric Unified Simulation (CACTUS) Objective: to improve understanding of interactions between atmospheric chemistry,
The Double Dividend of Methane Control
Daniel J. Jacob Harvard University
FOUR MAJOR RESEARCH CHALLENGES FOR THE SECOND DECADE OF THE USGCRP
AIR QUALITY & AIR POLLUTION
Shiliang Wu1 Loretta J. Mickley1, Daniel J
Intercontinental Transport, Hemispheric Pollution,
Linking Ozone Pollution and Climate Change:
OZONE PRODUCTION IN TROPOSPHERE
SCALE ISSUES IN MODELING INTERCONTINENTAL TRANSPORT
AIR POLLUTION AND GLOBAL CHANGE: TOWARDS AN INTEGRATED POLICY
The Human Influence on Climate: How much is known, What’s in store for us? Loretta Mickley Harvard University CO2 concentrations, Mauna Loa.
Questions for consideration
SATELLITE OBSERVATIONS OF OZONE PRECURSORS FROM GOME
The Climate Change – Urban Pollution Relationship
Effects of global change on U.S. ozone air quality
Geophysical Fluid Dynamics Laboratory Review
Geophysical Fluid Dynamics Laboratory Review
Benchmarking of chemical mechanisms
Fine particulate matter and ozone pollution in China: recent trends, future controls, and impact of climate change Daniel J. Jacob A typical day in Beijing.
Climatic implications of changes in O3
Presentation transcript:

Global atmospheric changes and future impacts on regional air quality Will O3 produced elsewhere in the world affect local air quality? How will a changing climate affect surface O3 concentrations? Loretta J. Mickley Harvard University

Number of people living in US counties violating National Air Quality standards, 1999 Focus of talk

Good O3 vs Bad O3 NOx = nitrogen oxide radicals VOC = volatile organic carbon

How has tropospheric O3 increased in last 100 years? Ozone measured on various mountaintops in Europe, 1870 to 1990

What could increase regional O3 in 21st century? Increase of local emissions of O3 precursors (NOx, VOCs) Transport of O3 or O3 precursors produced elsewhere Can use model with observed winds to calculate current influence Climate change effects on O3 loss and production rates Need to use model that generates its own climate (GCM)

How does intercontinental transport of O3 enhance local O3 surface concentrations today? North America Europe Asia GEOS-CHEM model, July 1997, Li et al 2002

How does N. American O3 affect O3 violations in Europe? Number of exceedance days for European standards (55 ppb, 8 hour average) Number of exceedance days due to North American sources GEOS-CHEM model, summer, Li et al 2002

Does Asian O3 enhance US surface O3 in summer? Subsidence of Asian pollution + production aloft Maximum Asian enhancements (up to 14 ppb) occur at intermediate ozone levels (50-70 ppb) Tropical air Stagnation Major concern if O3 standard decreases or Asian O3 increases Fiore et al. 2002

How important is methane to O3 and climate? Methane = overlooked precursor of ozone, has long lifetime (8-10 years) Cutting methane by 50% would: decrease incidence of ozone > 80 ppb in surface air by more than 50% decrease radiative forcing by both ozone and methane Trends in methane

How might climate change affect O3 loss and production? O2 + hn Stratospheric ozone ? Complex non-linear chemistry ? hn hn, H2O Nitrogen oxides (NOx) CO, Hydrocarbons ? Ozone (O3) Hydroxyl (OH) O3 source with high NOx O3 sink with low NOx Fires Biosphere Human activity physics chemistry biology Ocean

How might changing climate affect surface O3? Temperature changes ? (not the whole story!) Changes in circulation frequency of stagnation? stratospheric influx of ozone? transport from other continents? Lightning frequency? Water vapor concentrations? Emissions of VOCs from trees, grasses? Sum of climate changes more ozone? less ozone?

Chemistry, Aerosols, and Climate: Tropospheric Unified Simulation (CACTUS) Objective: to improve understanding of interactions between atmospheric chemistry, aerosols, and climate

Approach: coupled chemistry-aerosol-climate General Circulation Model (GCM) CACTUS model Atmospheric chemistry emissions land use greenhouse gas GISS GCM Aerosol microphysics D climate chemistry

CACTUS model study of preindustrial O3 Monthly mean observations at two sites in Europe Two model attempts, with differing natural emissions, but same climate as present-day Mickley et al. 2000

How will atmospheric motions change in 2xCO2 climate? Use SF6 to show how atmospheric motions change with warmer climate Stronger convective transport Weaker interhemispheric exchange Rind et al., 2001

How can we calculate change in O3 due to climate? 2000-2100: change well-mixed greenhouse gases year-by-year, calculate D climate 2. 2000,2025,2050,etc: change emissions of O3 precursors, use current climate, calculate D ozone 2000,2025,2050,etc: recalculate D ozone using climate from step 1. Diagnose D in ozone due to climate change. (Step 3- Step2)

Final thoughts Transport could have a big effect in future if Asian emissions increase. We need to learn how climate change may affect local ozone levels Ozone in July 2100, worst case scenario