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onshore percentages to the projected emissions scenarios shows BLM's potential decision scope of <br /> approximately 3.32 percent to 7.15 percent of the carbon budget.As a nation,the total projected demand <br /> for all fossil fuels (Federal, non-Federal, domestic and imported) relative to the future year projections <br /> would result in the consumption of between 16.7 percent to 35.9 percent of the carbon budget. Federal <br /> scope emissions would account for approximately 20 percent of the national scope budget consumption <br /> for either projection scenario. <br /> The Proposed Action is expected to extend the life of the mine for 22 years with a total of 17 million tons <br /> of coal being mined (19 years @ 800,000 tons and 3 years @ 600,000 tons). Direct, indirect, and <br /> downstream coal combustion emissions were calculated over the life of the mine (22 years). Based on <br /> estimated mining rates, EPA FLIGHT data from 2017 for the Tijeras and Pueblo cement facilities and <br /> current estimated downstream combustion, approximately 450.6 million tons of COze could be emitted <br /> over the life of the project.This value represents approximately 0.09 percent of the mean face value (500 <br /> GtCO2) of the carbon budget. <br /> Projected Climate Impacts <br /> The following information on predicted climate change has been summarized from the Intergovernmental <br /> Panel on Climate Change (IPCC). <br /> The future climate equilibrium is dependent upon warming caused by past anthropogenic emissions, <br /> future anthropogenic emissions, and natural variability. Global mean surface temperature change for the <br /> period 2016-2035 relative to 1986-2005 is similar for the four RCPs and will likely be in the range 0.3°C <br /> to 0.7°C (medium confidence). The projection assumes no major volcanic eruptions, changes in natural <br /> emissions sources (e.g., CH4 and N2O), or unexpected changes in total solar irradiance. By 2050, the <br /> magnitude of the projected climate change is significantly affected by the overall emissions path the world <br /> is tracking along. <br /> The projected increase of global mean surface temperature by the end of the 21st century (2081-2100) <br /> relative to 1986-2005 is likely to be 0.3°C to 1.7°C under RCP2.6, 1.VC to 2.6°C under RCP4.5, 1.4°C to <br /> 3.1°C under RCP6.0 and 2.6°C to 4.8°C under RCP8.5. It is virtually certain that there will be more frequent <br /> hot and fewer cold temperature extremes over most land areas on daily and seasonal timescales,as global <br /> mean surface temperature increases. It is also very likely that heat waves will occur with a higher <br /> frequency and longer duration. Occasional cold winter extremes will continue to occur, due to the <br /> inherent variability within the climate system. Changes in precipitation patterns will not be uniform, but <br /> in general arid regions are expected to become dryer while wetter areas can expect more frequent <br /> exceptional precipitation events. Oceans will continue to warm, with the greatest impacts occurring at <br /> the surface of tropical and northern hemisphere subtropical regions. Models also predict ocean <br /> acidification will increase for all RCP scenarios, where surface pH can be expected to decrease by 0.06 to <br /> 0.07 (15 to 17 percent)for RCP2.6 and 0.14 to 0.15 (38 to 41 percent)for RCP4.5.Year-round reductions <br /> in Arctic sea ice are projected for all RCP scenarios and it is virtually certain that near-surface (upper 3.5 <br /> m) permafrost extent at high northern latitudes will be reduced (37 percent - RCP2.6 to 81 percent - <br /> RCP8.5)as global mean surface temperature increases. Global mean sea level rise will very likely continue <br /> at a faster rate than observed from 1971 to 2010. For the period 2081-2100 relative to 1986-2005, the <br /> Dunn Ranch Area LBA and Mining Plan Modification 46 <br /> Technical Resources Report <br />