Substantial effects of land cover uncertainty on carbon and climate projections Difference in forest area between Max and Min Forest cases (1985-2004 avg) Alan V. Di Vittorio With special thanks to the iESM team Lawrence Berkeley National Laboratory Jiafu Mao and Xiaoying Shi Oak Ridge National Laboratory LMWG/BGCWG/SDWG Meeting 1 March 2017 Earth Systems and Society Program 2 ~15 ppmv CO2 bias in 2004 iESM v1 (CESM 1.1.2,CAM5,CLM4) Obs: NASA GISS ~392 CO2 concentration (ppmv) ~377 Year 3 ~15 ppmv CO2 bias in 2004 iESM v1 (CESM 1.1.2,CAM5,CLM4) Obs: NASA GISS ~392 CO2 concentration (ppmv) ~377 ~7M km2 more forest increases veg C gain by ~54 Pg and decreases CO2 gain by ~15 ppmv over 90 years Year 4 Different CMIP5 LULC/C can obscure LULC/C change effects on regional climate Model (1870) Model (1992 - 1870) North America 1974-2004 minus 1862-1891 (Lejeune et al., 2017) Model 5 • What is the contribution of land cover uncertainty to simulated carbon cycle uncertainty? • How does the land cover-driven carbon uncertainty compare to the effects of CO2 concentration, nitrogen deposition, and climate? • What are the effects of land cover uncertainty on local/regional climate? 6 iESM-CLM simulations: 1850 - 2004 • Identical CMIP5 land use inputs (* indicates fully coupled sim) Case LULCC Reference LULCC assumptions No LULCC Constant 1850 No conversion Default* Year 2000 Proportional to PFTs Max forest* Previous year ∆ Pasture/crop maximizes forest area Pasture rule* Previous year + Pasture replaces grass/shrub PFTs first Proportional* Previous year Proportional to PFTs; accounts for pasture Crop rule Previous year + Crop replaces tree PFTs first Min Forest* Previous year ∆ Pasture/crop minimizes forest area Prop constant CO2 Previous year Proportional to PFTs (max/min forest also) Prop const CO2/clim Previous year Proportional to PFTs (max/min forest also) Prop const N dep Previous year Proportional to PFTs (max/min forest also) • Atmosphere: CRU-NCEP, transient CO2, N deposition, and aerosols 7 5.1 Million km2 range in forest area by 2005 2.1 M km2 5.1 M km2 4.9 M km2 3.9 M km2 -200 0 LC uncertainty substantially affects total ecosystem carbon (Pg C) 43 Pg C *(37 Pg C, +10 ppmv) 28 Pg C *(22 Pg C, +6 ppmv) 33 Pg C *(23 Pg C, ~5 ppmv) Year 0 24 Pg C 41 Pg C -200 8 11 Pg C Year 9 Regional dependence of climate impacts Max forest minus Min forest (1985-2004 avg) 60 + - 30 + 0 -30 60 30 0 -30 ~ + ~ + + ~ + ~ 0.8 0 (°C) -0.8 7 % of grid cell 0 -7 10 Temperature diff (C) 2.0 Raw Data What drives temperature sign? 8 66 Difference of Albedo (%) 4 Albedo diff (%) Difference of Atmospheric Air Temperature (oC) 1.5 1 1.0 84.50 0.5 67.00 49.50 0 32.00 0.0 14.50 -3.000 -20.50 -0.5 -38.00 -55.50 -1.0 2 -60 -40 -60 00 -2 84.50 0 20 0 Latitude Latitude 40 60 60 80 67.00 -4 49.50 32.00 -6 14.50 -8 -10 -12 -20 R = -0.39, Sig. Raw Data Linear Fit 95% Confidence Band 95% Prediction Band -3.000 -20.50 -38.00 -55.50 5 10 15 20 25 30 35 00 30 Tree Percentage (%) DifferenceDifference in Treeof Cover (% of grid cell) Max Forest minus Min Forest (1985-2004 avg) (tree diff > 0) 11 Sensible heat may dominate latent heat Max Forest minus Min Forest (1985-2004 avg) (tree diff > 0) 10 10 Sensible Heat diff (W/m2) Latent Heat diff (W/m2) 88 6 4 2 00 Raw Data Linear Fit 95% Confidence Band 95% Prediction Band -8 R = 0.26, Sig. 0 0 5 10 15 20 25 Difference of Tree Percentage (%) 30 30 2 49.50 -2 14.50 -6 4 00 32.00 -4 6 67.00 84.50 -2 -10 Difference of Latern Heat Flux (W/m-2) 8 -3.000 -4 -6 -20.50 -38.00 -55.50 35 -8 Raw Data Linear Fit 95% Confidence Band 95% Prediction Band -10 -12 R = 0.007, Sig. 0 5 10 15 20 25 30 0 Difference of Tree Percentage (%) 30 Difference in Tree cover (% of grid cell) 12 Albedo vs Evaporative Fraction Max Forest minus Min Forest (1985-2004 avg, tree diff > 0) -0.10 12 -0.05 0.00 0.05 0.10 12 Difference of Albedo (%) 10 10 Temperature Difference 8 0.3 6 0 -0.3 8 6 4 4 2 2 0 0 -2 -2 -4 -4 -6 -6 -8 -10 -8 Tree Difference 5 10 15 20 -12 -0.10 25 -10 30 -0.05 0.00 0.05 Difference of Evaporative Fraction -12 0.10 13 Latent heat and temperature Max Forest minus Min Forest (1985-2004 avg, tree diff > 0) -6 -4 -2 0 Tree Difference Tree Difference 6 4 6 8 Temperature Difference < 0 0.500 30 30% -10 10 Temperature Differencre 10 10% 20 20% 8 2 0.00 10 10 8 8 6 4 4 2 2 0 0 -2 -2 -4 -4 -6 -6 -8 -8 -10 -10 -10 -8 -6 -4 -2 0 2 4 6 8 Difference of Latent Heat Flux (W/m -2) 2 Difference in Latent Heat (W/m ) 10 Difference of Albedo 10 -8 Difference in Albedo (%) -10 -8 -6 -4 -2 0 Tree Difference Tree Difference 4 6 8 10 Temperature Difference > 0 Temperature Differencre 10 10% 20 20% 0.500 30 30% 6 2 0.00 10 8 6 4 4 2 2 0 0 -2 -2 -4 -4 -6 -6 -8 -8 -10 -10 -10 -8 -6 -4 -2 0 2 4 6 8 Difference of Latent Heat Flux (W/m -2) 2 Difference in Latent Heat (W/m ) 10 14 Summary • Land cover uncertainty contributes ~5 ppmv uncertainty to CO2 concentration • This is about 1/3 of original bias • • • • • • • Land cover uncertainty can contribute on the order of 1 degree to temperature uncertainty This is on the order of LULCC-attributed effects Regional dependence Sensible heat vs albedo vs latent heat? Local vs distributed LULCC-driven uncertainty is reducible LULCC is an integrated process 14 Summary • Land cover uncertainty contributes ~5 ppmv uncertainty to CO2 concentration • This is about 1/3 of original bias • • • • • • • Land cover uncertainty can contribute on the order of 1 degree to temperature uncertainty This is on the order of LULCC-attributed effects Regional dependence Sensible heat vs albedo vs latent heat? Local vs distributed LULCC-driven uncertainty is reducible LULCC is an integrated process 14 Summary • Land cover uncertainty contributes ~5 ppmv uncertainty to CO2 concentration • This is about 1/3 of original bias • • • • • • • Land cover uncertainty can contribute on the order of 1 degree to temperature uncertainty This is on the order of LULCC-attributed effects Regional dependence Sensible heat vs albedo vs latent heat? Local vs distributed LULCC-driven uncertainty is reducible LULCC is an integrated process Questions? Difference in 2004 forest area between the Max forest case and the Proportional case This work is supported by the Director, Office of Science, Office of Biological and Environmental Research of the U.S. Department of Energy under Contract No. DEAC02-05CH11231 as part of the Integrated Assessment Research and Earth System Modeling Programs. E1 Different LUCID LULC/C can obscure LULC/C change effects on regional climate Model (1870) Model (1992-1870) North America 1974-2004 minus 1862-1891 (Lejeune et al., 2017) MM M Model
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