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Current Status of Canada’s Black Carbon Inventory

Current Status of Canada’s Black Carbon Inventory. Rock Radovan, P.Eng. Sr. Program Engineer Greenhouse Gas Division Environment Canada. Canada’s BC Inventory. Prepared in 2010 assuming a 2006 base year Developed by staff in Greenhouse Gas Division with support from other groups within EC

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Current Status of Canada’s Black Carbon Inventory

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  1. Current Status of Canada’s Black Carbon Inventory Rock Radovan, P.Eng. Sr. Program Engineer Greenhouse Gas Division Environment Canada

  2. Canada’s BC Inventory • Prepared in 2010 assuming a 2006 base year • Developed by staff in Greenhouse Gas Division with support from other groups within EC • Presented as a preliminary estimate • Prepared to support multilateral discussions on Short Lived Climate Forcers (SLCFs) which included Black Carbon • No common or accepted methodology currently in place • Few comparable national inventories • Not prepared as a standalone document as is the case with the National GHG Inventory Report

  3. Canada’s 2006 Black CarbonEmissions - 55.1 kt Emissions from natural sources (e.g. wildfires) are not included in the total. BC emissions from wildfires were estimated to be 20.0 kt for 2006 however this value has a high uncertainty associated with it.

  4. Canada’s BC Inventory Methodology • Builds on existing Criteria Air Contaminant (CAC) and National Pollutant Release Inventory (NPRI) inventories • EC’s atmospheric modelling experts use data from the CAC and NPRI inventories in their research • Allows for consistency across groups, particularly in air quality modelling research • Method similar to approach adopted by US EPA • PM2.5 emissions from inventories are divided into particle components based on source-specific characterization profiles • Use ‘SPECIATE’ database (developed by US) as well as Canadian specific information when available • Generic emission factors also used, mainly for open burning

  5. International Perspective • Government of Canada participating in several multilateral initiatives on SLCFs: • The Arctic Council’s Tromso Declaration (April 2009) established a Task Force on Short-Lived Climate Forcers with a mandate to: • Produce a Technical Report and Summary for Policy Makers on SLCFs, including recommendations for further national and international mitigation actions. (Jan/Feb 2011) • Ad Hoc Expert Group on Black Carbon under the UN Economic Commission for Europe Convention (UNECE) on Long-range Transboundary Air Pollution (LRTAP) • Will provide a report identifying options for potential revisions to the Gothenburg Protocol to mitigate black carbon (due Dec. 2010)

  6. Global & National BC Inventories • Several global emission inventories exist in addition to a number of national level data sets • e.g. the International Institute for Applied Systems Analysis (IIASA)provided a GAINS model of BC/OC emissions for each country party to the UNECE Convention on LRTAP (July 2010) • Disparity between existing inventories, in part due to: • Significant uncertainties in the magnitude of emissions, lack of information on physical distribution of sources, and gaps in knowledge on emissions from specific source categories • Information also lacking for several potentially important sectors such as flaring, shipping, agriculture and forest burning

  7. Geographic distribution ofblack carbon emissions • About 8,000 kt of black carbon emitted globally each year (2004) • Major source contributions for black carbon include approx.: • 40% from coal and oil burned in industrial and mobile sources, • 18% percent from residential biofuels for heating and cooking (wood, agricultural and animal waste), • 42% from open biomass burning - agriculture and forestry and wildfires • Developing countries emit approx. 80% of total BC emissions, while Europe and N. America a combined 13% • Africa emits about 25% of global BC, but nearly all from open burning • China, India and rest of Asia account for est. 39% of global emissions • Europe and North America BC emissions come primarily from fossil fuel combustion and largely above 40°N, therefore contribute disproportionately to warming • BC emissions north of 40°N are most likely to be transported to Arctic regions • Emissions from fossil fuel combustion contribute more to warming due to higher BC to OC ratio.

  8. Geographic distribution of black carbon emissions Adapted from Bond et. al 2004

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