Abstract
ensemble simulations with the A.M. Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences (IAP RAS) climate model (CM) for the 21st century are analyzed taking into account anthropogenic forcings in accordance with the Special Report on Emission Scenarios (SRES) A2, A1B, and B1, whereas agricultural land areas were assumed to change in accordance with the Land Use Harmonization project scenarios. Different realizations within these ensemble experiments were constructed by varying two governing parameters of the terrestrial carbon cycle. The ensemble simulations were analyzed with the use of Bayesian statistics, which makes it possible to suppress the influence of unrealistic members of these experiments on their results. It is established that, for global values of the main characteristics of the terrestrial carbon cycle, the SRES scenarios used do not differ statistically from each other, so within the framework of the model, the primary productivity of terrestrial vegetation will increase in the 21st century from 74 ± 1 to 102 ± 13 PgC yr−1 and the carbon storage in terrestrial vegetation will increase from 511 ± 8 to 611 ± 8 PgC (here and below, we indicate the mean ± standard deviations). The mutual compensation of changes in the soil carbon stock in different regions will make global changes in the soil carbon storage in the 21st century statistically insignificant. The global CO2 uptake by terrestrial ecosystems will increase in the first half of the 21st century, whereupon it will decrease. The uncertainty interval of this variable in the middle (end) of the 21st century will be from 1.3 to 3.4 PgC yr−1 (from 0.3 to 3.1 PgC yr−1). In most regions, an increase in the net productivity of terrestrial vegetation (especially outside the tropics), the accumulation of carbon in this vegetation, and changes in the amount of soil carbon stock (with the total carbon accumulation in soils of the tropics and subtropics and the regions of both accumulation and loss of soil carbon at higher latitudes) will be robust within the ensemble in the 21st century, as will the CO2 uptake from the atmosphere only by terrestrial ecosystems located at extratropical latitudes of Eurasia, first and foremost by the Siberian taiga. However, substantial differences in anthropogenic emissions between the SRES scenarios in the 21st century lead to statistically significant differences between these scenarios in the carbon dioxide uptake by the ocean, the carbon dioxide content in the atmosphere, and changes in the surface air temperature. In particular, according to the SRES A2 (A1B, B1) scenario, in 2071–2100 the carbon flux from the atmosphere to the ocean will be 10.6 ± 0.6 PgC yr−1 (8.3 ± 0.5, 5.6 ± 0.3 PgC yr−1), and the carbon dioxide concentration in the atmosphere will reach 773 ± 28 ppmv (662 ± 24, 534 ± 16 ppmv) by 2100. The annual mean warming in 2071–2100 relatively to 1961–1990 will be 3.19 ± 0.09 K (2.52 ± 0.08, 1.84 ± 0.06 K).
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References
J. Räisänen and T. N. Palmer, “A Probability and Decision-Model Analysis of a Multimodel Ensemble of Climate Change Simulations,” J. Clim. 14(15), 3212–3226 (2001).
J. M. Murphy, D. M. H. Sexton, D. N. Barnett, et al., “Quantifying Uncertainties in Climate Change from a Large Ensemble of General Circulation Model Predictions,” Nature 430(7001), 768–772 (2004).
G. C. Hegerl, T. R. Karl, M. Allen, et al., “Climate Change Detection and Distribution: Beyond Mean Temperature Signals,” J. Clim. 19(20), 5058–5077 (2006).
J. M. Murphy, B. B. B. Booth, M. Collins, et al., “A Methodology for Probabilistic Predictions of Regional Climate Change from Perturbed Physics Ensembles,” Philos. Trans. R. Soc. Ser. A 364(1857), 1993–2028 (2007).
P. A. Stott and C. E. Forest, “Ensemble Climate Predictions Using Climate Models and Observational Constraints,” Philos. Trans. R. Soc. Ser. A 364(1857), 2029–2052 (2007).
D. Ackerley, E. J. Highwood, and D. J. Frame, “Quantifying the Effects of Perturbing the Physics of an Interactive Sulfur Scheme Using an Ensemble of Gems on the climateprediction.net Platform,” J. Geophys. Res. 114(D1), D01203 (2009).
T. J. Osborn, S. C. B. Raper, and K. R. Briffa, “Simulated Climate Change during the Last 1000 years: Comparing the ECHO-G General Circulation Model with the MAGICC Simple Climate Model,” Clim. Dyn. 27(2–3), 185–197 (2006).
P. F. Demchenko, A. V. Eliseev, M. M. Arzhanov, et al., “Impact of Global Warming Rate on Permafrost Degradation,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 42(1), 35–43 (2006) [Izv., Atmos. Ocean. Phys. 42, 32–39 (2006)].
A. V. Eliseev, “Estimation of Uncertainty of Future Changes in the Concentration of Carbon Dioxide in the Atmosphere and Radiative Forcing of CO2,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 44(3), 301–310 (2008) [Izv., Atmos. Ocean. Phys. 44, 279–287 (2008)].
O. Yokohata, M. J. Webb, M. Collins, et al., “Structural Similarities and Differences in Climate Responses to CO2 Increase between Two Perturbed Physics Ensembles,” J. Clim. 23(6), 1392–1410 (2010).
P. A. Stott and J. A. Kettleborough, “Origins and Estimates of Uncertainty in Predictions of Twenty-First Century Temperature Rise,” Nature 416(6882), 723–726 (2002).
A. S. Monin, Introduction to the Climate Theory (Gidrometeoizdat, Leningrad, 1982) [in Russian].
V. P. Meleshko, G. S. Golitsyn, V. A. Govorkova, et al., “Possible Anthropogenic Climate Changes in Russia in the 21st Century: Estimations from an Ensemble of Climate Models,” Meteorol. Gidrol., No. 4, 38–49 (2004).
Climate Change 2007: The Physical Science Basis, Ed. by S. Solomon, D. Qin, M. Manning, et al. (Cambridge Univ. Press, Cambridge, 2007).
A. M. Greene, L. Goddard, and U. Lall, “Probabilistic Multimodel Regional Temperature Change Projections,” J. Clim. 19(17), 4326–4343 (2006).
V. Ch. Khon and I. I. Mokhov, “Climatic Changes in the Arctic and Possible Conditions of the Arctic Marine Navigation in the XXI Century,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 46(1), 19–25 (2010) [Izv., Atmos. Ocean. Phys. 46, 14–20 (2010)].
D. A. Stone, M. R. Allen, F. Selten, et al., “The Detection and Attribution of Climate Change Using an Ensemble of Opportunity,” J. Clim. 20(3), 504–516 (2007).
P. Friedlingstein, P. Cox, R. Betts, et al., “Climate-Carbon Cycle Feedback Analysis: Results from the C4MIP Model Intercomparison,” J. Clim. 19(22), 3337–3353 (2006).
C. E. Forest, P. H. Stone, and A. P. Sokolov, “Estimated PDFs of Climate System Properties Including Natural and Anthropogenic Forcings,” Geophys. Rev. Lett. 33(1), L01705 (2006).
O. Schneider von Deimling, H. Held, A. Ganopolski, et al., “Climate Sensitivity Estimated from Ensemble Simulations of Glacial Climate,” Clim. Dyn. 27(2–3), 149–163 (2006).
A. V. Eliseev and I. I. Mokhov, “The Sensitivity of the Feedback between Climate and Carbon Cycle to the Choice of the Defining Parameters of Terrestrial Carbon Cycle in a Climate Model of Intermediate Complexity,” in Selected Papers of the International Conference on Measurement, Modeling, and Information Systems for Environmental Studies: ENVIROMIS-2006, Russia, Tomsk, 2006. Vychislit. Tekhnol. 11 (2006).
A. V. Eliseev and I. I. Mokhov, “Carbon Cycle-Climate Feedback Sensitivity to Parameter Changes of a Zero-Dimensional Terrestrial Carbon Cycle Scheme in a Climate Model of Intermediate Complexity,” Theor. Appl. Climatol. 89(1–2), 9–24 (2007).
S. Sitch, V. Brovkin, W. von Bloh, et al., “Impacts of Future Land Cover Changes on Atmospheric CO2 and Climate,” Glob. Biogeochem. Cycles 19(2), GB2013 (2005).
E. M. Volodin, “General Circulation Model of the Atmosphere and Ocean with the Carbon Cycle,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 43(3), 298–313 (2007) [Izv., Atmos. Ocean. Phys. 43, 266–280 (2007)].
V. K. Petoukhov, I. I. Mokhov, A. V. Eliseev, et al., The IAP RAS Global Climate Model (Dialogue-MSU, Moscow, 1998).
D. Handorf, V. K. Petoukhov, K. Dethloff, et al., “Decadal Climate Variability in a Coupled Atmosphere-Ocean Climate Model of Moderate Complexity,” J. Geophys. Res. 104(D22), 27253–27275 (1999).
I. I. Mokhov, A. V. Eliseev, P. F. Demchenko, et al., “Climate Changes and Their Assessment with the IAP RAS Global Model,” Dokl. Akad. Nauk 402, 243–247 (2005) [Doklady Earth Sci., 402, 591–595 (2005)].
I. I. Mokhov, V. A. Bezverkhnii, A. V. Eliseev, et al., “Model Estimates of Global Climatic Changes in the 21st Century with Account for Different Variation Scenarios of Solar Activity,” Dokl. Akad. Nauk 411(2), 250–253 (2006) [Doklady Earth Sci., 411, 1327–1330 (2006)].
I. I. Mokhov, V. A. Bezverkhnii, A. V. Eliseev, et al., “Model Estimations of Possible Climatic Changes in 21st Century at Different Scenarios of Solar and Volcanic Activities and anthropogenic forcings,” Kosm. Issl. 46(4), 363–367 (2008) [Cosmic. Res., 46, 354–357 (2006)].
A. V. Eliseev and I. I. Mokhov, “Uncertainty of Climate Response to Natural and Anthropogenic Forcings due to Different Land Use Scenarios,” Adv. Atmos. Sci. 28(5) (2011).
Climate Change 2001: The Scientific Basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change, Ed. by J. T. Houghton, Y. Ding, D. J. Griggs, et al. (Cambridge Univ. Press, Cambridge, 2001).
I. I. Mokhov, A. V. Eliseev, and A. A. Karpenko, “Sensitivity of the IAP RAS Global Climate Model with an Interactive Carbon Cycle to Anthropogenic Forcings,” Dokl. Akad. Nauk 407, 400–404 (2006) [Doklady Earth Sci., 407, 424–428 (2006)].
A. V. Eliseev, I. I. Mokhov, and A. A. Karpenko, “Climate and Carbon Cycle Variations in the 20th and the 21st Centuries in a Model of Intermediate Complexity,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 43(1), 3–17 (2007) [Izv., Atmos. Ocean. Phys. 43, 1–14 (2007)].
I. I. Mokhov and A. V. Eliseev, “Explaining the Eventual Transient Saturation of Climate-Carbon Cycle Feedback,” Carbon Balance Management 3(4) (2008).
I. I. Mokhov, A. V. Eliseev, and A. A. Karpenko, Climate Change Research Trends, Ed. by L. N. Peretz (Nova Sci. Publ., Hauppauge, New York, 2008), pp. 217–241.
A. V. Eliseev, I. I. Mokhov, and A. A. Karpenko, “Influence of Direct Sulfate-Aerosol Radiative Forcing on the Results of Numerical Experiments with a Climate Model of Intermediate Complexity,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 43(5), 591–601 (2007) [Izv., Atmos. Ocean. Phys. 43, 544–554 (2007)].
M. M. Arzhanov, A. V. Eliseev, P. F. Demchenko, et al., “Modeling of Changes in Temperature and Hydrological Regimes of Subsurface Permafrost, using the Climate Data (Reanalysis),” Kriosfera Zemli 11(4), 65–69 (2007).
M. M. Arzhanov, A. V. Eliseev, P. F. Demchenko, et al., “Simulation of Thermal and Hydrologic Regimes of Siberian River Watersheds under Permafrost Conditions from Reanalysis Data,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 44, 86–93 (2008) [Izv., Atmos. Ocean. Phys. 44, 83–89 (2008)].
M. M. Arzhanov, P. F. Demchenko, A. V. Eliseev, et al., “Simulation of Characteristics of Thermal and Hydrological Soil Regimes in Equilibrium Numerical Experiments with a Climate Model of Intermediate Complexity,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 44, 591–610 (2008) [Izv., Atmos. Ocean. Phys. 44, 548–566 (2008)].
A. V. Eliseev, M. M. Arzhanov, P. F. Demchenko, et al., “Changes in Climatic Characteristics of Northern Hemisphere Extratropical Land in the 21st Century: Assessments with the IAP RAS Climate Model,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 45(3), 291–304 (2009) [Izv., Atmos. Ocean. Phys. 45 (3), 271–283 (2009)].
G. Marland, T. A. Boden, and R. J. Andres, “Global, Regional, and National CO2 Emissions,” Trends: A Compendium of Data on Global Change (Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, U.S. Department of Energy, Oak Ridge, Tennessee, 2005).
G. C. Hurtt, L. R. Chini, S. Frolking, et al., “Harmonization of Global Land-Use Scenarios for the Period 1500–2100 for IPCC-AR5,” Integr. Land Ecosyst.-Atm. Proc. Study (iLEAPS) Newslett., No. 7, 6–8 (2009).
C. MacFarling Meure, D. Etheridge, C. Trudinger, et al., “Dome CO2, CH4, and N2O Ice Core Records Extended to 2000 Years BP,” Geophys. Res. Lett. 33(14), L14810 (2006).
S. J. Walker, R. F. Weiss, and P. K. Salameh, “Reconstructed Histories of the Annual Mean Atmospheric Mole Fractions for the Halocarbons CFC-11, CFC-12, CFC-113, and Carbon Tetrachloride,” J. Geophys. Res. 105(C6), 14285–14296 (2000).
L. W. Horowitz, “Past, Present, and Future Concentrations of Tropospheric Ozone and Aerosols: Methodology, Ozone Evaluation, and Sensitivity to Aerosol Wet Deposition,” J. Geophys. Res. 111(D22), D22211 (2006).
Y.-M. Wang, J. Lean, and N. R. Sheeley, “Modeling the Sun’s Magnetic Field and Irradiance Since 1713,” Astrophys. J. 625(1), 522–538 (2005).
A. Robertson, J. Overpeck, D. Rind, et al., “Hypothesized Climate Forcing Time Series for the Last 500 years,” J. Geophys. Res. 106(D14), 14783–14804 (2001).
S. M. Ammann, G. A. Meehl, W. M. Washington, et al., “A Monthly and Latitudinally Varying Volcanic Forcing Dataset in Simulations of 20th Century Climate,” Geophys. Res. Lett. 30(12), 1657 (2003).
S. O. Los, G. J. Collatz, P. J. Sellers, et al., “A Global 9-year Biophysical Land-Surface Data Set from NOAA AVHRR Data,” J. Hydrometeorol. 1(2), 183–199 (2000).
A. V. Eliseev and I. I. Mokhov, et al., “Effect of Changes in Land Surface Albedo During Land Use on the Climate in XVI-XXI Century: Assessment using the Climate Model of IAP RAS,” in Problems of Ecological Monitoring and Ecosystem Modeling, Ed. by Yu. A. Izrael, S. M. Semenov, and V. A. Abakumov (Inst. Global. Klimata Ekol. Rosgidrometa i RAN, Moscow, 2010), vol. XXIII [in Russian].
A. V. Eliseev and I. I. Mokhov, “Effect of Registration of the Radiation Effect of a Change in Land Surface Albedo for Land Use on Reproducing the Climate of XVI-XXI Centuries,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 47(1), 18–34 (2011) [Izv., Atmos. Ocean. Phys. 47, 15–30 (2011)].
A. V. Eliseev, “Comparison of the Efficiency of Changes in Land Surface Albedo for Land Use,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 47(3) (2011) [Izv., Atmos. Ocean. Phys. 47 (2011) (in press)].
A. P. Sokolov, D. W. Kicklighter, J. M. Melillo, et al., “Consequences of Considering Carbon-Nitrogen Interactions on the Feedbacks Between Climate and the Terrestrial Carbon Cycle,” J. Clim. 21(15), 3776–3796 (2008).
S. Piao, P. Ciais, P. Friedlingstein, et al., “Spatiotemporal Patterns of Terrestrial Carbon Cycle during the 20th Century,” Glob. Biogeochem. Cycles 23(4), GB4026 (2009).
J. M. Gregory, C. D. Jones, P. Cadule, et al., “Quantifying Carbon Cycle Feedbacks,” J. Clim. 22(19), 5232–5250 (2009).
R. E. Kass and A. E. Raftery, “Bayes Factors,” J. Amer. Stat. Assoc. 90(430), 773–795 (1995).
J. A. Hoeting, D. Madigan, A. E. Raftery, et al., “Bayesian Model Averaging: A Tutorial,” Stat. Sci 14(4), 382–401 (1999).
S. S. Leroy, “Detecting Climate Signals: Some Bayesian Aspects,” J. Clim. 11(4), 640–651 (1998).
C. Tebaldi, L. O. Mearns, D. Nychka, et al., “Regional Probabilities of Precipitation Change: A Bayesian Analysis of Multimodel Simulations,” Geophys. Rev. Lett. 31(24), L24213 (2004).
C. Tebaldi, R. W. Smith, D. Nychka, et al., “Quantifying Uncertainty in Projections of Regional Climate Change: A Bayesian Approach to the Analysis of Multi-Model Ensembles,” J. Clim. 18(10), 1524–1540 (2005).
D. J. Frame, B. B. B. Booth, J. A. Kettleborough, et al., “Constraining Climate Forecasts: The Role of Prior Assumptions,” Geophys. Rev. Lett. 32(9), L09702 (2005).
A. Lopez, C. Tebaldi, M. New, et al., “Two Approaches to Quantifying Uncertainty in Global Temperature Changes,” J. Clim. 19(19), 4785–4796 (2006).
C. D. Keeling, J. F. S. Chine, and T. P. Whorf, “Increased Activity of Northern Vegetation Inferred from Atmospheric CO2 Measurements,” Nature 382, 146–149 (1996).
N. Zeng, H. Qian, C. Roedenbeck, et al., “Impact of 1998–2002 Midlatitude Drought and Warming on Terrestrial Ecosystem and the Global Carbon Cycle,” Geophys. Rev. Lett. 32(22) (2005).
P. Cadule, P. Friedlingstein, L. Bopp, et al., “Benchmarking Coupled Climate-Carbon Models Against Long-Term Atmospheric CO2 Measurements,” Glob. Biogeochem. Cycles 24(2), GB2016 (2010).
Anthropogenic Climate Changes, Ed. by M. I. Budyko and Yu. A. Izrael’ (Gidrometeoizdat, Leningrad, 1987) [in Russian].
A. M. Tarko, Anthropogenic Changes in Global Biosphere Processes (Fizmatlit, Moscow, 2005) [in Russian].
O. I. Lenton, “Land and Ocean Carbon Cycle Feedback Effects on Global Warming in a Simple Earth System Model,” Tellus 52B(5), 1159–1188 (2000).
P. E. Thornton, J.-F. Lamarque, N. A. Rosenbloom, et al., “Influence of Carbon-Nitrogen Cycle Coupling on Land Model Response to CO2 Fertilization and Climate Variability,” Glob. Biogeochem. Cycles 21(4), GB4018 (2007).
A. Jain, X. Yang, H. Kheshgi, et al., “Nitrogen Attenuation of Terrestrial Carbon Cycle Response to Global Environmental Factors,” Glob. Biogeochem. Cycles 23(4), GB4028 (2009).
S. Gerber, L. O. Hedin, M. Oppenheimer, et al., “Nitrogen Cycling and Feedbacks in a Global Dynamic Land Model,” Glob. Biogeochem. Cycles 24(1), GB1001 (2010).
V. K. Arora, G. J. Boer, J. R. Christian, et al., “The Effect of Terrestrial Photosynthesis Down Regulation on the Twentieth-Century Carbon Budget Simulated with the CCCma Earth System Model,” J. Clim. 22(22), 6066–6088 (2009).
S. Zaehle, A. D. Friend, P. Friedlingstein, et al., “Carbon and Nitrogen Cycle Dynamics in the O-CN Land Surface Model: 2. Role of the Nitrogen Cycle in the Historical Terrestrial Carbon Balance,” Glob. Biogeochem. Cycles 24(1), GB1006 (2010).
Yu. A. Izrael’, S. M. Semenov, I. M. Kunina, et al., “Modifikatsiya pryamogo effekta dioksila ugleroda na vysshie rasteniya vsledstvie vozdeistviya troposfernogo ozona,” Dokl. Akad. Nauk 338(5), 711–713 (1994).
S. M. Semenov, I. M. Kunina, and B. A. Kukhta, “Comparison of Anthropogenic Changes in Surface Concentrations O3, SO2, and CO2 in Europe on the Basis of Environmental Criteria,” Dokl. Akad. Nauk 361(2), 275–279 (1998).
J. C. I. Kuylenstierna, H. Rodhe, S. Cinderby, et al., “Acidification in Developing Countries: Ecosystem Sensitivity and the Critical Load Approach on a Global Scale,” Ambio 30(1), 20–28 (2001).
S. Sitch, P. M. Cox, W. J. Collins, et al., “Indirect Radiative Forcing of Climate Change through Ozone Effects on the Land-Carbon Sink,” Nature 448(7155), 791–794 (2007).
V. K. Arora and H. D. Matthews, “Characterizing Uncertainty in Modeling Primary Terrestrial Ecosystem Processes,” Glob. Biogeochem. Cycles 23(2), GB2016 (2009).
S. Manabe, M. J. Spelman, and R. J. Stouffer, “Transient Responses of a Coupled Ocean-Atmosphere Model to Gradual Changes of Atmospheric CO2,” J. Clim. 5(2), 105–126 (1992).
I. I. Mokhov and A. V. Eliseev, “Tropospheric and Stratospheric Temperature Annual Cycle: Tendencies of Change,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 33, 452–463 (1997) [Izv., Atmos. Ocean. Phys. 33, 415–426 (1997)].
P. D. Jones, M. New, D. E. Parker, et al., “Surface Air Temperature and Its Changes over the Past 150 years,” Rev. Geophys. 37(2), 173–199 (1999).
J. Hansen, R. Ruedy, J. Glascoe, et al., “GISS Analysis of Surface Temperature Change,” J. Geophys. Res. 104(D24), 30997–31022 (1999).
S. M. Semenov and E. S. Gel’ver, “Changes in the Annual Cycle of Daily Average Air Temperature in Russia in the XX Century,” Dokl. Akad. Nauk 386(3), 389–394 (2002).
J. Räisänen, “CO2-Induced Climate Change in CMIP2 Experiments: Quantification of Agreement and Role of Internal Variability,” J. Clim. 14(9), 2088–2104 (2001).
C. J. Wallace and T. J. Osborn, “Recent and Future Modulation of the Annual Cycle,” Clim. Res. 22(1), 1–11 (2002).
A. V. Eliseev and I. I. Mokhov, “Amplitude-Phase Characteristics of the Annual Cycle of Surface Air Temperature in the Northern Hemisphere,” Adv. Atmos. Sci. 20(1), 1–16 (2003).
A. V. Eliseev, I. I. Mokhov, and M. S. Guseva, “Sensitivity of Amplitude-Phase Characteristics of the Surface Air Temperature Annual Cycle to Variations in Annual Mean Temperature,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 42, 326–340 (2006) [Izv., Atmos. Ocean. Phys. 42, 300–312 (2006)].
I. I. Mokhov and A. V. Eliseev, Encyclopedia of Ecology, Ed. by S. E. Jorgensen and B. Fath (Elsevier, Amsterdam, 2008), pp. 598–602.
R. A. Monserud and R. Leemans, “Comparing Global Vegetation Maps with the Kappa Statistic,” Ecol. Mod. 62(4), 275–293 (1992).
N. E. Rodin and N. I. Bazilevich, Dynamics of Organic Matter and Biological Cycle of Ash Elements and Nitrogen in the Major Vegetation Types of the World (Nauka, Moscow, 1965) [in Russian].
A. A. Titlyanova, Biological Carbon Cycle in Herbaceous Biogeocenoses (Nauka, Novosibirsk, 1977) [in Russian].
K. I. Kobak, Biotic Components of the Carbon Cycle (Gidrometeoizdat, Leningrad, 1988) [in Russian].
N. I. Bazilevich and A. A. Titlyanova, Biotic Turnover on the Five Continents: Nitrogen and Ash Elements in Natural Terrestrial Ecosystems (Izd. SO RAN, Novosibirsk, 2008) [in Russian].
P. M. Cox, Description of the TRIFFID Dynamic Global Vegetation Model, Hadley Centre Technical Note 24 (Hadley Centre, Met. Office, Bracknell, 2000).
Yu. M. Svirezhev and W. von Bloh, “Climate, Vegetation, and Global Carbon Cycle: The Simplest Zero-Dimensional Model,” Ecol. Mod. 101, 79–95 (1997).
A. Adams, A. White, and T. M. Lenton, “An Analysis of Some Diverse Approaches to Modelling Terrestrial Net Primary Productivity,” Ecol. Mod. 177, 353–391 (2004).
M. S. Williamson, T. M. Lenton, J. G. Shepherd, et al., “An Efficient Numerical Terrestrial Scheme (ENTS) for Earth System Modelling,” Ecol. Mod. 198, 362–374 (2006).
K. Thonicke, S. Venevsky, S. Sitch, et al., “The Role of Fire Disturbance for Global Vegetation Dynamics: Coupling Fire Into a Dynamic Global Vegetation Model,” Glob. Ecol. Biogeogr. 10(6), 661–677 (2001).
V. Brovkin, S. Sitch, W. von Bloh, et al., “Role of Land Cover Changes for Atmospheric CO2 Increase and Climate Change during the Last 150 years,” Glob. Change Biol. 10, 1253–1266 (2004).
R. A. Houghton, J. E. Hobbie, J. M. Melillo, et al., “Changes in the Carbon Content of Terrestrial Biota and Soils between 1860 and 1980: A Net Release of CO2 to the Atmosphere,” Ecol. Monographs 53(3), 235–262 (1983).
P. Brohan, J. J. Kennedy, I. Harris, et al., “Uncertainty Estimates in Regional and Global Observed Temperature Changes: A New Data Set from 1850,” J. Geophys. Res. 111(D12), D12106 (2006).
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Original Russian Text © A.V. Eliseev, 2011, published in Izvestiya AN. Fizika Atmosfery i Okeana, 2011, Vol. 47, No. 2, pp. 147–170.
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Eliseev, A.V. Estimation of changes in characteristics of the climate and carbon cycle in the 21st century accounting for the uncertainty of terrestrial biota parameter values. Izv. Atmos. Ocean. Phys. 47, 131–153 (2011). https://doi.org/10.1134/S0001433811020046
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DOI: https://doi.org/10.1134/S0001433811020046