Emissions of Regional and Global Air Pollutants David Streets Argonne National Laboratory, U.S.A. EPA Workshop on Climate Change and Air Quality Research.

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Presentation transcript:

Emissions of Regional and Global Air Pollutants David Streets Argonne National Laboratory, U.S.A. EPA Workshop on Climate Change and Air Quality Research Triangle Park December 3-5, 2001

Sources of airborne pollution in developing countries are many: home cooking, power generation, industry, traffic, and biomass burning

Important species in the Asian atmosphere and their origin l Particles like BC and OC (residential fuel combustion, diesel vehicles) l SO 2 and sulfate aerosol (coal combustion) l CO 2, CH 4, and other greenhouse gases (fossil fuels, agriculture) l NO x, nitrate aerosol, and other nitrogen compounds (vehicles) l Non-methane volatile organic compounds (NMVOC) (all kinds) l Ozone (formed from NO x and NMVOC) l Ammonia (agriculture mainly) l Trace elements such as Hg (fossil-fuel combustion) l Mineral dust (wind-blown from arid and semi-arid regions) Small particles like BC, OC, and SO 4 are implicated in regional- and continental-scale problems and global warming. Tropospheric ozone is also now recognized as an important greenhouse gas.

Methodology for Asian Emission Estimates Energy Use RAINS-Asia Model Emission Controls Activity data Other human activities Biomass burning Natural emissions Biogenic, Volcanic... Emission factors, Regulations Anthropogenic emissions “Total” emissions

Coordinated emission profiles for Asia for the year 2000 are being constructed for TRACE-P and ACE-Asia

The distribution of emissions among source types varies considerably

Coal-burning cook stoves in Xian, China Inefficient combustion in Asia produces large quantities of CO, CH 4, NMHC, and BC

New investigations have forced a re-assessment of BC emission factors (Streets et al., Atmos. Environ., 35, 4281, 2001)

Black carbon emissions in China are distributed in a broad SW to NE swath across the rural heartland TRACE-P gridded emissions at 5 mins x 5 mins resolution

INDOEX measurements show unusually high BC concentrations off the Indian continent (Dickerson et al., 2001) High BC may be due to biomass burning, vehicle fuel adulteration, small coal combustors or…?

There has been a remarkable change in air pollution emissions in China since 1996, due to: l The economic downturn in in East and Southeast Asia l Reform of industry and power, leading to a reduction in coal use l Structural shift away from heavy industry towards high-tech industries and services l Improvements in energy efficiency and fuel quality l Closing of many small, inefficient, high-sulfur coal mines, reducing the over-supply of coal l Slowdown in electricity demand, due to higher electricity prices l Opening up of electricity and coal markets l Residential fuel switching from coal to electricity and gas in (large) cities l Technological progress in the energy-intensive sectors (Source: Sinton and Fridley, Energy Policy, 28, 671, 2000)

Future SO 2 emissions in Asia are likely to be much lower than the latest IPCC forecasts

Long-term emission changes in Asia are reflected in sulfate aerosol measurements at Midway Island (Prospero et al., 2001)

Annual trends in CO 2 and CH 4 emissions in China ( Streets et al., Science, November 30, 2001)

Indexed trends in greenhouse-gas emissions in China The net effect of these emission changes on global mean temperatures is an INCREASE, due to the dominant effect of the sulfate aerosol

NMVOC emission profiles are very different around the world

NMVOC emissions in China come from varied sources and are growing fast (Klimont et al., Atmos. Environ., 2001)

NMVOC Emissions are Speciated into 19 Reactivity Classes

Ammonia emissions are high in Asia (due to animals and fertilizer use) and important for the formation of (NH 4 ) 2 SO 4 TRACE-P gridded NH 3 emissions

Biomass burning can have a large influence on hemispheric air quality; this figure shows the Siberian forest fires of 1998

TOMS AI data show progression of Siberian smoke plume across East Asia and the Pacific Ocean

AVHRR fire count image for 3/28/2001 showed no burning over SE Asia and China, due to clouds ….

…. however, TOMS AI data for the same day show heavy aerosol over southern China ….

…. so we can use the TOMS AI data to “fill in” missing AVHRR data (cautiously!)

On April 16, 1998, a huge dust cloud formed over China and was pushed eastward by a frontal system (NASA SeaWiFS) ….

…. nine days later, some of the dust reached the California coastline (on April 25, 1998)

TRACE-P (Transport and Chemical Evolution over the Pacific) ACE-Asia (Asian Pacific Regional Aerosol Characterization Experiment) Experimental measurements Theoretical modeling

On 3/10/2001, the TRACE-P DC-8 traversed plumes of man- made pollution from China (red) and biomass burning from Southeast Asia (orange)

Elevated biomass- burning plume from Southeast Asia Low-level pollution from mainland China Chemical forecasting was able to successfully predict pollution features during TRACE-P (BC)

Research Needs for Regional and Global Emissions l more source testing in developing countries to produce reliable emission factors l the development of emitter inventories (e.g., vehicles) and surveys to gauge the representativeness of emission factors l greater consistency of estimates of primary particulate emissions, particularly BC and OC, by size and chemical composition l special investigations of emissions/modeling/observation inconsistencies (e.g., Asian CO and BC) l improve the use of satellite data to develop fine temporal and spatial resolution of biomass burning l “narrow the gaps” by studying unconventional sources: coal-mine fires, field combustion, waste burning…… Experimental programs like TRACE-P and ACE-Asia promise new insights into pollutant release, transformation, and transport