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LCFS Indirect Land Use Change Expert Workgroup Carbon Emission Factors Subworkgroup Presentation to California Air Resources Board Sacramento, CA August.

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Presentation on theme: "LCFS Indirect Land Use Change Expert Workgroup Carbon Emission Factors Subworkgroup Presentation to California Air Resources Board Sacramento, CA August."— Presentation transcript:

1 LCFS Indirect Land Use Change Expert Workgroup Carbon Emission Factors Subworkgroup Presentation to California Air Resources Board Sacramento, CA August 17, 2010 8/17/20101CARB ILUC EWG Emission Factors

2 Membership Sonia Yeh (University of California, Davis) – Co-chair Richard Nelson (Kansas State University) – Co-chair Uwe Fritsche (Oeko-Institut, Germany) Holly Gibbs (Stanford University) Keith Kline (ORNL) Steffen Mueller (University of Illinois at Chicago) Don O’Connor (representing CDFA, S&T Consulting) Michael O’Hare (University of California, Berkeley) ARB staff representative: Kevin Cleary Special thanks to: – Sahoko Yui, graduate student, UC Davis – Susan Tarka Sanchez, Lifecycle Associates – Richard Plevin, UC Berkeley 2 LCFS Indirect Land Use Change Expert Workgroup July Update

3 Outline Biomass C – Review – Pay attention to the issue of scale: Develop spatially explicit C stocks by AEZ Soil C – Changes in Soil C Stock – depth, percent loss, management Loss rates on conversion, including the specific time profile, including non-CO2 emissions Emission factors for other indirect effects: livestock emissions, rice cultivation, and crop switching Uncertainty Analysis The list only includes what the subgroup is able to examine to date, and does not imply the exclusion of other important emission factors yet to be examined 8/17/20103CARB ILUC EWG Emission Factors

4 4 Land conversion emissions Above-ground biomass ✦ Is land cover accurately categorized? ✦ Is converted region same as average? ✦ What is the time profile of emissions? Below-ground biomass ✦ Estimated using roots:shoots ratio ✦ How much is affected by conversion? Soil carbon ✦ Varies spatially and with LU history ✦ How much is affected by conversion? ✦ What is time profile of emissions? Foregone sequestration ✦ What would have been stored? ✦ Over what time period?

5 Generic Approach Total Carbon stock change is the area times the change in carbon stock density. Area is a GTAP output. GTAP provides the change in forest area and pasture (livestock) area for each AEZ in each of the regions as shown in the next couple of slides.

6 Forestry Changes

7 Livestock Changes

8 GTAP AEZ

9 Ideally carbon stock changes can be determined for each AEZ rather than using a country average as has been the practice to date. This depends on having good carbon stock data at the AEZ level.

10 IPCC Tier 1 -- Default Values Gibbs et al. (2007) ERL, Ruesch and Gibbs (2008) Rough approximations that are immediately available 8/17/201010CARB ILUC EWG Emission Factors

11 Forest Carbon “Tier 1.75” Extrapolate up using range of satellite data Saachi et al (2007) 8/17/201011CARB ILUC EWG Emission Factors

12 Data Sources for Forest Carbon Stock Estimates in Winrock Analysis 8/17/2010CARB ILUC EWG Emission Factors12 Ruesch and Gibbs (2008)

13 Range in C Stock Biome Estimates 8/17/2010CARB ILUC EWG Emission Factors13

14 8/17/2010CARB ILUC EWG Emission Factors14

15 Biomass C Stock Evaluate the spatially-explicit Winrock database as a basis for estimating biomass C stock by AEZ – Holly Gibbs can provide data and assistance in the implementation Supplement with databases to improve the accuracy of certain regions/eco-system types, or to include the consideration of certain factors (e.g. forest degradation) Estimate the ranges of uncertainties (confidence interval) associated with these biomass C stock values according to the origins of the data or other methods (e.g default uncertainty values presented in the IPCC Guidelines) 8/17/201015CARB ILUC EWG Emission Factors

16 Soil C Stock Winrock analysis – World Harmonized Soil Database (2009) has a resolution of 1 km – Evaluate 30 cm depth (Winrock/IPCC) vs. 100 cm depth used on WHRC Peatlands treated differently – Evaluate 20-50% soil C loss (Winrock) vs. 25% soil C loss (WHRC) for forest to cropland conversion – Evaluate management factors For example: Full till practice and medium cultivation assumed for all croplands in Winrock – Coefficient of variation is 0.45 8/17/201016CARB ILUC EWG Emission Factors

17 Comparison of Soil C Loss in CARB/WHRC vs. Winrock Analysis (not weighted by land type converted) 8/17/2010CARB ILUC EWG Emission Factors17

18 IPCC Activity Data Stock Change Factors (20 yrs) (LULUCF) 8/17/2010CARB ILUC EWG Emission Factors18 Factor value typeLevel Temperature regime Moisture regime IPCC defaults Est. Error Description Land use (FLU) Long term cultivated Temperate/ Boreal Dry0.89% Represents area continuously managed for >20 yrs, to predominately annual crops. Input and tillage factors are also applied to est. C stock changes. LU factor est. relative to use of full tillage and nominal ('medium') carbon input levels. Moist0.6912% Tropical Dry0.5861% Moist/Wet 0.4846% Tropical montanen/a0.6450% Land use (FLU) Paddy Rice All Dry and Moist/Wet 1.150% Long term (>20 year) annual cropping of wetlands. Can include double- cropping with non-flooded crops. Tillage and input factors not used for paddy rice. Land use (FLU) Perennial/ Tree All Dry and Moist/Wet 150% Long term perennial tree crops such as fruit and nut trees, coffee and cacao.

19 Peatlands Emissions Winrock – Represented in Indonesia and Malaysia, and cover 2-44% and 2- 22% in some of the corresponding administrative regions. – Emission factors = 20 t C/ha/yr assuming 80 cm drainage depth – Constant emissions for 80 yrs (cumulative emissions = 1600 t C/ha) Globally peatlands are net C sinks and net methane sources. – Winrock’s analysis concludes CH 4 emissions from undisturbed tropical peatlands are small compared with C emissions after disturbance. Our analysis of boreal peatlands shows the same results. However, local conditions vary. 8/17/201019CARB ILUC EWG Emission Factors

20 Peatlands Emissions – Fossil Fuel LU Peatlands emissions from oil and oil sands extraction in Alberta available from Yeh et al. (ES&T, submitted) – ~22% of current oil sands surface leases is covered by peatland 8/17/2010CARB ILUC EWG Emission Factors20 Soil carbon (in t C/ha) of peatland of continental western Canada (Alberta, Saskatchewan, and Manitoba). Extracted from Yeh et al. based on Tables 1 and 3 of Vitt et al. (2000) Source: Yeh, Sonia, Jordaan, Sarah, Brandt, Adam, Turetsky, Merritt, Spatari, Sabrina and Keith, David. Land Use Greenhouse Gas Emissions from Conventional and Unconventional Oil Production. ES&T, submitted.

21 Loss Rates on Conversion Changes in BM C stock – Fire emissions (in the disturbed case and in the reference case) – Harvested wood products – Forest categories (disturbed vs undisturbed, by maturity status, by degradation status) – Drought? – Management practices? Foregone Sequestration Livestock emission factors Other non Kyoto climate forcing-emissions N2O emissions 8/17/201021CARB ILUC EWG Emission Factors

22 Harvested Wood Products Disposition of C in harvested wood products: products-in-use, landfill, emitted with energy capture, emitted without energy capture. IPCC guidelines recommend default reporting of the removals from forest system as instantaneous emission to the atmosphere for UNFCCC reporting purposes Other guidelines dealing with C sequestration of harvested wood products : IPCC, California Climate Action Registry (CCAR), DOE 1605 Forestry Emission Guidelines, Chicago Climate Exchange, etc. – Consider the storage factor and the fate of the C in the products – Example (Next slide) Need to know the (dynamic) market share of these products in order to allocate emissions to various pools 8/17/201022CARB ILUC EWG Emission Factors

23 Examples of C sequestration in forest products 8/17/2010CARB ILUC EWG Emission Factors23 Source: Intergovernmental Panel on Climate Change (IPCC): 2003a, Estimation, reporting and accounting of harvested wood products – technical paper. UNFCCC paper FCCC/TP/2003/7,, UNFCCC Secretariat, Bonn, Germany October 27, 2003. http://unfccc.int/resource/docs/tp/tp0307.pdf. February 3, 2005. Source: DOE. Technical Guidelines for Voluntary Reporting of Greenhouse Gas Program. Appendix D. Summary of Data and Methods Contributing to Calculation of the Disposition of Carbon in Harvested Wood Products

24 Harvested Wood Products (HWP) in the US USDA’s Resource Planning Act RPA tables Used in LU spreadsheet appended to GREET 1.8d for US region HWP = Fraction of softwood/hardwood removal from harvested sites * Fraction of sawlogs/pulpwood production from softwood/hardwood * Disposition patterns for different time horizons

25 Emission Factors for other Indirect Effects Increased demand leads to higher prices that lead to increased production and lower consumption. Two areas where there may be significant GHG impacts of reduced consumption are: – Livestock emissions – Rice production emissions 8/17/201025CARB ILUC EWG Emission Factors

26 Livestock Emissions Ag emissions account for ~32% of total anthropogenic emissions. Two major categories of livestock emissions – Enteric fermentation (~34% of total ag emissions) – Manure (~8% of total ag emissions) and indirect emissions from manure management highly variable and substantial 8/17/201026CARB ILUC EWG Emission Factors

27 Livestock Emissions Results from RFS2 g CO 2 eq/MJ Corn Ethanol-0.27 Soybean Biodiesel-8.07 Sugar Cane Ethanol-0.12 8/17/201027CARB ILUC EWG Emission Factors

28 Livestock Emissions Approach – Take the change in livestock population from GTAP. – Multiply by the livestock emissions per region. – Inventories are available for UNFCCC Annex 1 countries. – EPA has published estimates of emissions for 92 countries plus 8 regions. 8/17/201028CARB ILUC EWG Emission Factors

29 Rice Emissions Rice emissions account for 11% of ag emissions. RFS2 Results g CO 2 eq/MJ Corn Ethanol1.78 Soybean Biodiesel-5.45 Sugar Cane Ethanol0.46 8/17/201029CARB ILUC EWG Emission Factors

30 Rice Emissions Same basic approach – Take the change in rice production from GTAP – Multiply by the rice emissions per GTAP region – UNFCCC and EPA inventories. 8/17/201030CARB ILUC EWG Emission Factors

31 Crop Switching GHG emissions per acre are significantly different between crops, rotation and management practices. 8/17/201031CARB ILUC EWG Emission Factors

32 8/17/201032CARB ILUC EWG Emission Factors GHG emission intensities per unit area and per unit of dry matter (DM) for the 21 most important field crops in Canada during 2006

33 Land Use After Conversion For example: Factors by by Ogle et al. Assess land use and management impacts on soil organic carbon storage for US agricultural lands – Factors represent the change in SOC storage for the top 30cm of the soil profile after 20 years following the management change. Used in LU spreadsheet appended to GREET 1.8d

34 Crop Switching Total GHG emissions from ag land therefore depend on the crop mix and field management practices. Some of the crop shifting is driven by the availability of co-products. In the direct GHG analysis, we already attempted to put a GHG values on those co-products, so there is some overlaps between the GHG change from crop shifting and the GHG benefits from the direct analysis of co-products. 8/17/201034CARB ILUC EWG Emission Factors

35 Summary of Emission Factors of Other Indirect Effects There are other indirect impacts beyond changes in carbon stocks (biomass + Soil C). The changes can be positive or negative. For some pathways the other emissions are significant (~25% of ILUC for soybean biodiesel). 8/17/201035CARB ILUC EWG Emission Factors

36 36 Climate-active emissions Direct LLGHGs – CO 2, CH 4, N 2 O, halocarbons (SF 6, CFCs, etc.) Indirect GHGs – affect the fate of direct GHGs – CO, NO X, NMVOC Aerosols: short-lived, vary regionally – organic carbon, SO 2 (cooling) – black carbon (mainly warming)

37 37 Black Carbon (soot) Formed by incomplete combustion Absorbs heat and reduces albedo (reflectance) Short atmospheric lifetime (days or weeks) 2nd largest contributor to GW after CO 2 Despite many uncertainties, it’s useful to include BC in uncertainty analysis

38 38 Emission factor for savanna fires Emission g/kg DM a GWP 100 g CO 2 e/kg EF contrib. CO 2 16401 b 164070% CO653 c 1958% CH 4 2.425 b 603% NMHC3.18 c 251% NO X 3.1-1 c -30% N2ON2O0.15298 b 452% BC0.8680 d 54423% OC3.2-50 e -160-7% Total EF2345100% a Delmas et al. 1995; b IPCC AR4; c Brakkee et al 2008; d Bond and Sun 2005; e Sanhueza 2009

39 39 Savanna burning emission factor

40 Treatment of Uncertainties Include confidence intervals in all estimates – Monte Carlo simulation can better represent the skewness of the overall distribution Use parametric analysis to estimate emission of specific time profile to examine emissions over time Include specific emission factors such as forest degradation factor, N 2 O emissions, N application rates, treatment of forest wood products, livestock emissions, inclusion/exclusion of non-CO 2 GHG emissions (with uncertainty range) in the sensitivity analysis Use global SA to estimate uncertainty importance to identify which parameters drive overall variance. 8/17/201040CARB ILUC EWG Emission Factors

41 Next Step Examine the following issues and identify recommendations for: – Changes in BM C stock Fire emissions Forest categories (disturbed vs undisturbed, maturity, degradation, drought) – Soil C emissions – Dynamic modeling of LU emission changes (stock + flow) vs. categorical modeling (percent changes in stock) 8/17/201041CARB ILUC EWG Emission Factors


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