Global food demand and the sustainable intensification of agriculture David Tilmana,1, Christian Balzerb, Jason Hillc, and Belinda L. Beforta a Department of Ecology, Evolution, and Behavior, University of Minnesota, St. Paul, MN 55108; bDepartment of Ecology, Evolution, and Marine Biology, University of California, Santa Barbara, CA 93106; and cDepartment of Bioproducts and Biosystems Engineering, University of Minnesota, St. Paul, MN 55108 Contributed by David Tilman, October 12, 2011 (sent for review August 24, 2011) Global food demand is increasing rapidly, as are the environmental impacts of agricultural expansion. Here, we project global demand for crop production in 2050 and evaluate the environmental impacts of alternative ways that this demand might be met. We find that per capita demand for crops, when measured as caloric or protein content of all crops combined, has been a similarly increasing function of per capita real income since 1960. This relationship forecasts a 100–110% increase in global crop demand from 2005 to 2050. Quantitative assessments show that the environmental impacts of meeting this demand depend on how global agriculture expands. If current trends of greater agricultural intensification in richer nations and greater land clearing (extensification) in poorer nations were to continue, ∼1 billion ha of land would be cleared globally by 2050, with CO2-C equivalent greenhouse gas emissions reaching ∼3 Gt y−1 and N use ∼250 Mt y−1 by then. In contrast, if 2050 crop demand was met by moderate intensification focused on existing croplands of underyielding nations, adaptation and transfer of high-yielding technologies to these croplands, and global technological improvements, our analyses forecast land clearing of only ∼0.2 billion ha, greenhouse gas emissions of ∼1 Gt y−1, and global N use of ∼225 Mt y−1. Efficient management practices could substantially lower nitrogen use. Attainment of high yields on existing croplands of underyielding nations is of great importance if global crop demand is to be met with minimal environmental impacts. food security | land-use change | biodiversity | climate change | soil fertility G lobal demand for agricultural crops is increasing, and may continue to do so for decades, propelled by a 2.3 billion person increase in global population and greater per capita incomes anticipated through midcentury (1). Both land clearing and more intensive use of existing croplands could contribute to the increased crop production needed to meet such demand, but the environmental impacts and tradeoffs of these alternative paths of agricultural expansion are unclear (1, 2). Agriculture already has major global environmental impacts: land clearing and habitat fragmentation threaten biodiversity (3), about one-quarter of global greenhouse gas (GHG) emissions result from land clearing, crop production, and fertilization (4), and fertilizer can harm marine, freshwater, and terrestrial ecosystems (5). Understanding the future environmental impacts of global crop production and how to achieve greater yields with lower impacts requires quantitative assessments of future crop demand and how different production practices affect yields and environmental variables. Here, we forecast 2050 global crop demand and then quantitatively evaluate the global impacts on land clearing, nitrogen fertilizer use, and GHG release of alternative approaches by which this global crop demand might be achieved. To do these analyses, we compiled annual agricultural and population data for 1961–2007 obtained from the FAOSTAT database (Food and Agriculture Organization of the United Nations; http://faostat.fao.org/) and other sources (SI Materials and Methods) for each of 100 large nations that comprised 91% of the 2006 global population (Table S1). We then calculated net national demand for crop calories and crop protein for each nation for each year 20260–20264 | PNAS | December 13, 2011 | vol. 108 | no. 50 based on national annual yields, production, imports, and exports of 275 major crops (those crops used as human foods or livestock and fish feeds) (Table S2). The resultant per capita demand for calories or protein from all food or feed crops combined (SI Materials and Methods) encompasses annual human crop consumption, crop use for livestock and fish production, and all losses (waste and spoilage during food and crop production, storage, transport, and manufacturing). To determine long-term global trends and better control for economic differences among nations, nations were aggregated into seven economic groups ranging from highest (Group A) to lowest (Group G) national average per capita real (inflation-adjusted) gross domestic product (GDP) (Table S1). Results and Discussion Global Crop Demand. Analyses reveal a simple and temporally consistent global relationship between per capita GDP and per capita demand for crop calories or protein. Across all years, per capita crop use was similarly dependent on per capita GDP both within and among the seven economic groups (Fig. 1). The magnitude of this dependence is surprisingly large. In 2000, for example, per capita use of calories and protein by the richest nations (Group A) were 256% and 430% greater, respectively, than use by the poorest nations (Groups F and G). These large differences in crop demand partially result from greater dietary meat consumption at higher income (6, 7) and the low efficiency with which some types of livestock convert crop calories and protein into edible foods (8). We suggest that the observed relationships between per capita crop use and per capita real GDP (Fig. 1) provide a means of forecasting future crop demand. Specifically, using the fitted curves in Fig. 1, we forecasted per capita crop caloric and protein demand for 2050 for each economic group by its estimated 2050 per capita GDP (Fig. 2 B and C) (Table S3). The GDP estimate (SI Materials and Methods and Fig. S1) assumes that per capita real GDP would grow at ∼2.5% per year globally, with rates for developing nations being greater than developed nations (Fig. 2A). Using United Nations (UN) projections of 2050 population (9) (Fig. S2), we next calculated the total 2050 demand for crop calories or crop protein for each economic group and then summed these values to estimate 2050 global crop demand (SI Materials and Methods). These analyses forecast that global demand for crop calories would increase by 100% ± 11% and global demand for crop protein would increase by 110% ± 7% (mean ± SE) from 2005 to 2050 (Table S3). This projected doubling is lower than the 176% Author contributions: D.T. designed research; D.T., C.B., J.H., and B.L.B. performed research; D.T., C.B., and B.L.B. analyzed data; and D.T., J.H., and B.L.B. wrote the paper. The authors declare no conflict of interest. Freely available online through the PNAS open access option. See Commentary on page 19845. 1 To whom correspondence should be addressed. E-mail: [email protected]. This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10. 1073/pnas.1116437108/-/DCSupplemental. www.pnas.org/cgi/doi/10.1073/pnas.1116437108 1961 7,000 6,000 2003 5,000 4,000 1961 3,000 1961 2,000 Economic group 2003 p < 0.0001 F = 7,860 n = 301 1,000 A B C D E F G 0 0 5,000 10,000 15,000 20,000 25,000 Per Capita GDP (1990$ yr -1) 300 250 35,000 30,000 2005-2050 Growth 101% 2005 Actual 25,000 246% 20,000 338% 15,000 379% 10,000 104% 0% F G 0 A B C 10% 34% 64% D E B 10,000 107% 8,000 6,000 62% 4,000 20% 0% 2,000 0 200 A B 13% 50% C D E F G C 150 p < 0.0001 F = 7,860 n = 301 100 50 0 0 5,000 10,000 15,000 20,000 25,000 Per Capita GDP (1990$ yr -1) Fig. 1. Annual dependence of per capita demand for (A) crop calories and (B) protein on per capita real GDP for each of economic Groups A–G (SI Materials and Methods). Each color of points shows the trajectory for a particular economic group (one point per year for each group). Curves are fitted to the square root of per capita GDP. (caloric) and 238% (protein) increases in global crop use that would occur if per capita demands of all nations in 2050 reached the 2005 levels of Group A nations. Any projection of future global crop production entails many elements of uncertainty and of necessity emphasizes some potentially causative factors over others. Our forecast of a 100– 110% increase in global crop production by 2050 is larger than the 70% increase that has been projected for this same period (10). Although our projection methods and the methods of the earlier study differ in many ways, the different forecasts may occur because of our use of quantitative global trends in per capita crop demand that emphasize income-dependent dietary choices (Fig. 1) vs. their use of expert opinion of national and regional demand trends (10). Quantification of Yield, Input, and Climate Relationships. The environmental impacts of doubling global crop production will depend on how increased production is achieved (11, 12). Production could be increased by agricultural extensification (that is, clearing additional land for crop production) or intensification (that is, achieving higher yields through increased inputs, improved agronomic practices, improved crop varieties, and other innovations). Here, we quantify the global impacts on land clearing, GHG emissions, and nitrogen fertilization of alternative pathways of agricultural development that meet the 2050 global crop production that we forecast. In particular, we evaluate the comTilman et al. 29% 5,000 Per capita protein demand (g day-1) Per capita protein demand (g day -1) B 350 A SEE COMMENTARY 2003 400 350 300 250 200 150 100 50 0 80% 116% 89% 28% 0% A High B C D E Economic Group Per capita GDP F G Low Fig. 2. (A) Per capita GDP, (B) per capita demand for crop calories, and (C) per capita demand for crop protein in 2005 (black) and mean projected 2050 increases (white; percent increases above bars). binations of current or improved agricultural technologies, enhancements to soil fertility, and land clearing that could meet our projected 2050 global caloric demand and what their environmental impacts would be. For brevity, results for protein are not presented here but are similar. Because of data availability, we use past N fertilization rates as quantitative measures of soil fertility enhancement, but we emphasize that soil fertility can also be enhanced by legumes, cover crops, and other means and that yields could increase with less N fertilizer than in the past if N use efficiency increases (1, 2, 13). We used multiple regressions to quantify how nation to nation and year to year differences in caloric yields have been related to N fertilization intensity (N ha−1) and other variables that are thought to impact yields (SI Materials and Methods). We found that caloric yields were simultaneously related to N fertilization intensity, precipitation, potential evapotranspiration, soil pH, elevation, time (year), and economic group (Table S4). A simpler regression that included just N fertilization intensity, precipitation, economic group, and time gave similar results (Table S4). Two otherwise similar regressions used just 2005 data (Table S5). These four regressions show that ∼80% of national-level variation in caloric yields was statistically explained by a few underlying variables. We use these fitted relationships to quantify PNAS | December 13, 2011 | vol. 108 | no. 50 | 20261 SUSTAINABILITY SCIENCE Per capita caloric demand (kcal day -1) 8,000 Per capita GDP (1990$ yr-1) 9,000 Per capita caloric demand (kcal day-1) A scenarios, exploring the potential effects of changes in these variables on caloric yields and the environment. We do so with the caveat that the fitted relationships need not be indicative of causation, while noting that fits are consistent with other analyses of controls of yields (12, 14, 15). After controlling for N fertilization intensity, climate, soil, and elevation in these regressions, we will, for brevity, refer to the residual yield differences ascribed to economic groups as mainly reflecting technological and infrastructure disparities among the economic groups, and we will refer to the residual yield differences that are ascribed to time (year) as mainly reflecting technological improvements from 1965 to 2005. Alternative Pathways of Agricultural Expansion. These regressions can estimate the dependence of global yields on N use (soil fertility enhancement) if future technological advances were to continue along observed temporal trends to 2050 (technology improvement), if underyielding nations were to overcome technological disparities by adapting and then adopting the highyielding technologies of Group A nations (technology transfer), or if both technology improvement and technology transfer were to occur. In particular, we used our regression results to quantify curves defining the dependence of global caloric yields on global N use for four cases that all meet our projected 2050 crop caloric demand forecast (Fig. 3A and SI Materials and Methods). For all cases, we assumed that the currently large disparities among nations in agricultural intensities (measured here as N ha−1) were eliminated by 2050. We call this equalization of N use strategic N utilization, because it provides a larger increase in global crop production per unit of N than would occur from greater N use in nations already applying N at high rates. The current technology curve in Fig. 3 retains each economic group’s N-dependent yield at its 2005 relationship and thus assumes no technological improvements or transfer from 2005 to 2050. This curve provides a potential lower bound for 2050 yields. It is defined by six data points calculated from each of the two regressions that used just 2005 data (Table S5). These two regressions, which differ in the number of variables included, give results so similar to each other as to be almost indistinguishable in Fig. 3 A–C. A potential upper bound is provided by the technology improvement and transfer curve for which complete technology transfer is assumed to allow all nations to achieve (by 2050) the technological improvements and soil- and climate-adjusted yields projected for Group A nations by 2050. The two regressions on which it is based also gave highly similar predictions (Fig. 3 A–C and Table S4). Two intermediate curves, each defined by two regressions, provide benchmarks within the region defined by the upper and lower bounds. The technology improvement curve assumes that yields continue to increase until 2050 along the 1965–2005 time trajectory (Table S4) but that all nations otherwise retain the technology of their economic group. The technology transfer curve has each nation, based on its climate and soils, achieve (in 2050) the climate- and soil-adjusted N-dependent yield of Group A nations in 2005 (Table S5). All four curves in Fig. 3 explore what might occur should lower-yielding nations achieve, by 2050, significant soil fertility enhancements (here quantified by increased N use but potentially achievable by other means). Any point in the shaded region of Fig. 3A represents different combinations of technology improvement and technology transfer that, for the given global N use or its equivalent soil fertility enhancement, would meet global caloric demand in 2050. The increased global yields that could result from various degrees of technology improvement, technology transfer, or N use would meet 2050 crop demand with less cropland clearing (1, 2) (Fig. 3B). For instance, if global N use were held at 200 Mt, achieving the technology transfer and improvement benchmark by 2050 20262 | www.pnas.org/cgi/doi/10.1073/pnas.1116437108 would decrease land clearing by ∼1.2 billion ha compared with current yields (Fig. 3B). Land clearing, soil cultivation, and N fertilizer manufacturing and use all emit GHG. We quantified global emissions from these sources for each curve using Intergovernmental Panel on Climate Change (IPCC) Tier 1 methods (16, 17) (SI Materials and Methods and Tables S6 and S7). Although estimates of N2O emissions that result from N fertilizer are variable (18), such variability is small compared with the other sources of emissions that we quantified. Our analyses found that, when increased global N is focused on croplands of underyielding nations, projected global 2050 net GHG emissions are reduced, as shown by the negative slopes for each of the four curves of Fig. 3C. Reduced GHG emissions occurred because increased N use decreased land clearing. The resultant reduction in GHG emissions from lower land clearing was approximately three times the emissions increase from the N fertilizer. Environmental Impacts of Meeting Increased Crop Demand. These relationships among global N use, yield, land clearing, and GHG emissions allow exploration of the environmental impacts of different pathways of global agricultural development. Four hypothetical pathways that start on the current technology curve at the 2005 global average N use intensity of 94 kg ha−1 (Fig. 3 D–F) illustrate that our forecast of 2050 global crop demand may be met in ways that have markedly different environmental impacts. First, consider a pathway that mimics past trends (black arrows), with poorer, lower-yielding nations increasing crop production mainly through land clearing and richer, higher-yielding nations doing so mainly by yield increases from intensification and yield improvement. The environmental impacts of this past trend trajectory would, as illustrated, increase global land clearing to a total of ∼1 billion ha by 2050, global agricultural GHG emissions to ∼3 Gt y−1 of CO2-carbon equivalents, and global N use to ∼250 Mt y−1. These increases would have major environmental impacts through resultant species extinctions, loss of ecosystem services, elevated atmospheric GHG levels, and water pollution (3–5, 19). Greater global investments in technology improvement and technology adaptation and transfer could markedly reduce these impacts, as illustrated by the other three trajectories, all of which attain the technology improvement and technology adaptation and transfer frontier by 2050. For instance, the N-minimizing trajectory shown (brown arrows) (Fig. 3 D–F) could retain global N use at its current 100 Mt y−1, have land clearing of ∼0.5 billion ha, and have GHG emissions of 1.6 Gt y−1. Alternatively, a current N-intensity trajectory (yellow arrows), with global N intensity staying at 94 kg ha−1 until 2050, would move global values to N use of ∼125 Mt, land clearing of ∼0.4 billion ha, and GHG emissions of ∼1.4 Gt y−1 in 2050. A land sparing trajectory (white arrows) would minimize both land clearing and GHG emissions. It could meet our 2050 projected global crop demand while clearing only ∼0.2 billion ha land globally and producing global GHG emissions of just ∼1 Gt y−1. Global N use would be ∼225 Mt y−1. This analysis suggests that a land sparing trajectory of agricultural development might be the best option for minimizing biodiversity loss and GHG emissions, but it comes with the environmental cost associated with greater global N use. However, a variety of practices can greatly decrease this environmental cost by increasing the efficiency of agricultural nitrogen utilization (1, 11–13, 20, 21). For instance, recent field trials of an integrated soil–crop management system in China achieved a 90% increase in maize yields with no increase in N use (13). Because N inputs in excess of plant uptake increase nitrate loading into surface and ground waters and contribute to marine anoxic zones (20, 22), greater development and adoption of agronomic practices that increase nutrient efficiency (23, 24) could further decrease environmental impacts of increased yields (25–27). Tilman et al. Land cleared for crops (109 ha) nly ro fe ans tr h Tec pr Im 160 ech 140 nt t e r r 120 Cu 1002050 Average 80 N intensity (kg ha-1) 60 250 150 200 Global N use in 2050 (106 tonnes) 80 0.5 Im prove me sfer nt & t 0 100 C 2050 Total annual GHG emissions from land clearing and N fertilizer (109 tonnes CO2e) men tran 2 1 ech t 120 ech 140 rre rove Tec h 100 Cu Imp 1.0 3 2050 Average N intensity (kg ha-1) 60 1.5 4 300 nt t t on 160 ly only 150 200 250 Global N use in 2050 (106 tonnes) SEE COMMENTARY 0.5 Land sparing Current N intensity 100 F 0 300 Past trend 1.0 300 300 Current average N intensity (kg ha-1) 94 N minimizing 0 2050 Average N -1 80 intensity (kg ha ) 100 Cur ren 120 140 Imp t te rove ch 160 men t on ly Tech trans fer on ly Improv ement & tech transfe r Current 94 average N intensity (kg ha-1) 150 200 250 Global N use in 2050 (106 tonnes) 1.5 er 60 100 N minimizing 2.0 ransf 150 200 250 Global N use in 2050 (106 tonnes) Land sparing Past trend 100 E 2.0 5 only ent m ove Current N intensity 150 200 250 Global N use in 2050 (106 tonnes) 300 Current average N intensity 94 (kg ha-1) 5 4 N minimizing 3 Past trend 2 Land sparing 1 Current N intensity 0 100 150 200 250 Global N use in 2050 (106 tonnes) 300 Fig. 3. Projections of 2050 values for (A) global yields, (B) global land clearing, and (C) global agricultural GHG emissions and (D–F) the yields and environmental impacts of four alternative hypothetical trajectories along which agriculture might develop by 2050. Tonnes CO2e in (C) and (F) represents the equivalent tonnes of C that would have been emitted had all GHG emissions in our analyses been in the form of CO2. All abscissas are global annual N use in 2050 calculated as the sum across all economic groups of N use intensity (N ha−1) times total cropland area (ha) needed to meet projected 2050 caloric demand. To derive the curves shown, current N use intensities of lower-yielding nations were strategically increased to equal global mean intensity, which was set at 60, 80, 100, 120, 140, or 160 kg ha−1 to calculate the 12 points shown for each curve (SI Materials and Methods). The four curves shown in each graph (magenta, current technology; blue, improvement only; orange, technology adaptation and transfer only; green, improvement and technology transfer) are regression-based estimates of yields (A and D) and associated land clearing (B and E) needed to meet 2050 global caloric demand and resultant GHG emissions (C and F). Land clearing = (cropland needed to meet 2050 crop demand) − (2005 cropland). Conclusions Trajectories of global agricultural development that are directed to greater achievement of the technology improvement and technology transfer frontier would meet 2050 crop demand with much lower environmental impacts than trajectories that were Tilman et al. continuations of past trends (19). This difference occurs because strategic intensification that elevates yields of existing croplands of underyielding nations can meet the majority of 2050 global crop demand, and in so doing can greatly reduce land clearing and GHG emissions. PNAS | December 13, 2011 | vol. 108 | no. 50 | 20263 SUSTAINABILITY SCIENCE vem ro Imp tec 19 18 17 16 15 14 13 12 11 10 9 8 2050 Global average yield (106 kcal ha-1) & ent 100 B D r sfe an h tr Land cleared for crops (109 ha) 2050 Global average yield (106 kcal ha-1) 19 18 17 16 15 14 13 12 11 10 9 8 2050 Total annual GHG emissions from land clearing and N fertilizer (109 tonnes CO2e) A Current yield differences among nations are large. In 2005, for example, caloric yields for Group A nations were 308% greater than for Groups F and G, 138% greater than for Group E, and 37% greater than for Groups B, C, and D. Our analyses, which incorporate the effects of climate and soils on yields, suggest that agricultural intensification through technology adaptation and transfer and enhancement of soil fertility in poorer nations would greatly reduce these yield gaps (14), provide a more equitable global food supply, and greatly decrease the GHG emissions and species extinctions that otherwise would have resulted from land clearing (4). Our analyses explore the implications of the 100% increase from 2005 to 2050 in global crop production that we forecast. If global crop demand were lower (10), less land clearing and/or N use would be needed, and environmental impacts would be smaller. Our evaluations of the environmental benefits of alternative pathways of global agricultural development are not meant to imply that they might be similarly attainable or feasible. Global yields will likely be impacted by climate change (15). Yield increases in richer nations may be more difficult than in the past if some major crops are approaching yield ceilings (21, 28). Yield increases in poorer nations will require significant investments in innovative adaptation of technologies to new soil types, climates, and pests (29, 30) as well as new infrastructure (2). However, yields have been increased in some nations in which they were long stagnant, such as Malawi and Zimbabwe (31, 32). In Zimbabwe, for instance, field trials on >1,200 farms showed that technology transfer (farmer education) and intensification (N fertilizer use at ∼13% of use by Group A nations) increased maize 1. Godfray HCJ, et al. (2010) Food security: The challenge of feeding 9 billion people. Science 327:812–818. 2. The Government Office for Science (2011) Foresight. The Future of Food and Farming. Final Project Report (The Government Office for Science, London). 3. Dirzo R, Raven PH (2003) Global state of biodiversity and loss. 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(Cambridge University Press, New York). 20264 | www.pnas.org/cgi/doi/10.1073/pnas.1116437108 yields 40%, giving market value returns ∼400% greater than the cost of fertilization (32). Global food demand is growing rapidly, much of the world’s current cropland has yields well below their potential, and the current global trajectory of agricultural expansion has serious longterm implications for the environment. The environmental impacts of escalating crop demand will depend on the trajectory along which global agriculture develops. The preservation of global biodiversity and the minimization of the GHG impacts of agriculture may well hinge on this trajectory. A trajectory that adapts and transfers technologies to underyielding nations, enhances their soil fertility, employs more efficient nutrient use worldwide, and minimizes land clearing provides a promising path to more environmentally sustainable agricultural intensification and more equitable global food supplies. Materials and Methods Detailed descriptions of our data sources and analyses can be found in the SI Materials and Methods. These include data on political, economic, agricultural, and climatic variables; analyzed nations, economic aggregates, and global estimates; crop demand; projections of per capita GDP; yield regressions; four 2050 yield curves and land cleared curves in (Fig. 3); calculation and projections of GHG emissions from land use conversion; and estimation of GHG emissions from N fertilizer manufacture and application. ACKNOWLEDGMENTS. We thank Charles Godfray, Jon Foley, Gretchen Daily, Stephen Polasky, Matt Burgess, and Jonathan Levine for comments. We thank the National Science Foundation for Grant DEB-0620652 and the University of Minnesota Institute on the Environment for support. 18. IPCC (2006) 2006 IPCC Guidelines for National Greenhouse Gas Inventories, eds Eggleston S, et al. (IGES, Hayama, Japan). 19. Tilman D, et al. 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Supporting Information Tilman et al. 10.1073/pnas.1116437108 SI Materials and Methods Data on Political, Economic, Agricultural, and Climatic Variables. We compiled annual national data (Table S1) for 1961–2007 on population from Food and Agriculture Organization’s PopSTAT database (Food and Agriculture Organization of the United Nations, Rome, 2009; http://faostat.fao.org) (Fig. S2) and gross domestic product (GDP; expressed in real 1990 international dollars) from the Total Economy Database (Groningen Growth and Development Centre, New York, 2008; www.conferenceboard.org/data/economydatabase/) on the production, area harvested, imports, exports, and stores of up to 275 nutritious crops (Table S2) and N fertilizer use from the FAOSTAT database (Food and Agriculture Organization of the United Nations, Rome, 2009; http://faostat.fao.org). Annual N fertilizer use intensity was calculated as the annual N use of a nation divided by the total area harvested for all crops. Using commodity- and nation-specific conversion factors from FAOSTAT, we calculated total annual caloric and protein production for each crop, summing across all crops to find national calorie and protein production totals and yields for all nutritious crops combined. We obtained global 5-min latitude/longitude raster data on the within-nation geographic distribution of croplands as well as climate, soil, and elevation variables from the SAGE 1992 Croplands Dataset (Center for Sustainability and the Global Environment, University of Wisconsin–Madison, 1998; www. sage.wisc.edu/mapsdatamodels.html). The national average values of precipitation, elevation, potential evapotranspiration (PET), soil organic carbon, and soil pH weighted across areas cropped in each nation in 1992 were calculated using Esri ArcGIS 9.3. Analyzed Nations, Economic Aggregates, and Global Estimates. We analyzed crop demand (utilization) and yield patterns and trends using data from the 100 more populous nations, representing 91% of total 2006 global population, for which sufficient annual data on nutritious crop production and other variables were available for 1961–2007. Some nations, however, had been formed during this period when a former nation split into two nations. Their data reported after the split had to be combined to make them comparable with the earlier data. This combination reduced the number of distinct entities, which for brevity, we call nations in the text, to 95. A few large nations, including the former USSR and its derivatives, could not be included in our trend analyses because of years of missing data associated with dissolution of state or periods of civil unrest or war. Each nation was assigned to one of seven economic groups ranging from highest (Group A) to lowest (Group G) national average 2000–2007 per capita real (inflation-adjusted) GDP (Table S1). For specific analyses, some otherwise included nations were excluded from regressions. Malaysia (Group B) was excluded from caloric analyses, but not protein analyses, because of poor data on exports and food vs. biodiesel use of palm nut oil, an energy dense commodity. Data from Ireland (Group A), The Netherlands (Group A), and New Zealand (Group B) were excluded when performing regressions against N use, because these nations have applied large proportions of their N fertilizer to pasture rather than nutritious crops, with annual data on amounts so applied being unavailable. The global estimates of the environmental affects of future crop demand that we present in this paper are scaled to encompass the populations of all nations, including the remaining small nations and the few larger nations not included in trend analyses for lack Tilman et al. www.pnas.org/cgi/content/short/1116437108 of data. For all these nations, we obtained populations, GDPs, and cropland areas, assigning each nation the mean per capita crop demands and yields of the economic group to which it belonged (according to its per capita GDP). Crop Demand. We use the term crop demand interchangeably with FAOSTAT’s annual domestic supply, both being defined as annual production + imports − exports + decrease in stocks. Because of low use of crops for biofuels before 2007 (1), we did not exclude such use from demand. For 1961–2003, per capita nutritious crop demand of each economic group was dependent on per capita inflation-adjusted GDP. Two fits were obtained for each of the two nutritional units (tonnes protein and calories), with per capita GDP square root transformed to capture the nonlinear response observed. One was a universal fit, where data from all nations were fit simultaneously to the square root of per capita GDP (Fig. 1 A and B). The other was a specific fit, where data from each economic group were fit separately to the square root of per capita GDP by adding an interaction between economic group and the square root of per capita GDP to the statistical model. Square root was chosen over logarithmic transformation because of its superior fit based on R2 and Akaike Information Criterion (AIC) values. We then used the four resulting fitted formulas to estimate 2050 per capita nutritious crop demand for each of the economic groups based on their predicted 2050 per capita GDP (see below). Group per capita 2050 demand is reported as the average of the two forecasts for each nutritional unit (Table S3). Global crop demand in 2050 was calculated by multiplying each group’s 2050 per capita demand by the total population (included + nonincluded nations) forecasted for 2050 by the United Nations (UN) Population Division’s median variant projection (UN Department of Economic and Social Affairs, New York, 2011; http://esa.un.org/unpd/wpp/unpp/panel_population.htm) (Fig. S2) and then summing demand across all seven economic groups (Table S3). Projections of per Capita GDP. Trajectories of the rate of change of per capita GDP are a Kuznets (2) function of per capita GDP (2–4). This empirical functional relationship is used to forecast per capita GDP (4), especially when information on future values of other terms in the Solow (5) income model are unavailable. To project the per capita GDP that each economic group might achieve by 2050, we statistically fit by least squares the dependence of the observed annual rate of change of per capita GDP for each economic group on its per capita GDP, obtaining the Kuznets (2) curve of Fig. S1. Then, using the method of Seldon and Song (4), we numerically solved the resultant ordinary differential equation to forecast per capita GDP to 2050 for each economic group. We did not make any forecasts for individual nations because these forecasts are not needed for our projections and might be more idiosyncratic than projections for groups of many nations. The model solutions (Fig. S1) gave results similar to other estimates of 2050 per capita GDP (6, 7). Yield Regressions. We used past yield relationships and trends to estimate the yields that might be achievable by 2050. All analyses used 5-y mean data on a nation by nation basis (for example, the mean for 1965 is the average for 1963–1967). In particular, we used four regressions paired in two. One pair, the time series regressions, used nine points in time comprised 1 of 8 of 1965, 1970, 1975, . . . , and 2005 averages and included year as one of its variables (Table S4). The other pair, the 2005 regressions, only used average 2005 (average for 2003–2007) data (Table S5). Within each of these pairs, a four-variable regression determined the dependence of yield on economic group, the 1.333 root of national N use intensity per hectare (that is, N0.75), precipitation, and year (if a time series regression). The other kind of regression, a seven-variable regression, determined the dependence of yield on those variables plus soil pH, elevation, and potential evapotranspiration. Only N0.75 was used in all regressions, because the relationship between yield and N use intensity for the 95 analyzed nations was increasing but nonlinear and N0.75 provided a better fit based on R2 and AIC than N (linear), log[N], N0.5 (square root), or N0.667 (the 1.5 root of N use intensity) for all regressions. For the two time series regressions, each of the variables in both the four-variable regression and the seven-variable regression was significant at P < 0.01, and the overall regressions were significant at P < 0.0001. For the two 2005 regressions, all variables were significant at P < 0.01 in the four-variable regression and remained so in the seven-variable regression, but in the sevenvariable regression, none of the three added variables was significant (P > 0.05 for each). Four 2050 Yield Curves and Land-Cleared Curves in Fig. 3. Each of the two 2005 regression fits provides estimates on which the current technology yield curve in Fig. 3A is based. In particular, each 2005 regression was used to calculate the caloric yield of each nation (adjusted for all other regression variables) for each of six different N use intensities (60, 80, 100, 120, 140, and 160 kg ha−1 N fertilizer). We then calculated the yield for each economic group at each N use intensity by weighting national yields by areas harvested in each nation. Global yields for each N use intensity were similarly calculated as area-weighted means of yields of all seven economic groups; 6 of the 12 2050 global yield points to which the current technology yield curve in Fig. 3A is fit come from one of the 2005 regression variations (one point per N use intensity), and the other 6 come from the other variations. All 12 points are shown in Fig. 3A. The forecasts based on the seven-variable regression and those forecasts based on the four-variable regression are indistinguishable. Although none of the three added variables in the seven-variable regression was significant, those six points predicted by this regression are shown precisely to illustrate how insensitive these forecasts were to inclusion of added soil and climate variables. The 2050 total global N use values associated with these 12 global yields were calculated from 2050 economic group yields and projected 2050 economic group caloric demands as follows (Eq. S1): 2050 Area Harvested ¼ ð2050 Projected DemandÞ=ð2050 YieldÞ [S1] and (Eq. S2) 2050 N Use ¼ ð2050 N Use IntensityÞ × ð2050 Area HarvestedÞ: [S2] Global N use is the sum of the 2050 N use across all seven economic groups. The 2005 regressions were also used to estimate the 2050 yields of the technological transfer curve. The calculations were identical to those calculations just described except that, in using the regressions to project 2050 values, all nations were assigned to be members of economic Group A. The yields so calculated thus represent the yields that could be achieved if each nation by 2050 was able to achieve a yield comparable with the yields of Tilman et al. www.pnas.org/cgi/content/short/1116437108 Group A nations in 2005 but adjusted for its own climate and/or soil and elevation. The two time series regressions were similarly used to obtain the technology improvement curve by using the observed time dependence of yield on year in the multiple regressions to estimate the yields of all nations in 2050 under the assumption that yields would continue to increase along the fitted trend line until 2050. As before, yields of each nation were adjusted for its own climate and/or soil and elevation. Group yields and then global yields were then calculated as above. The technology improvement and transfer curve was also similarly obtained from the two time series regressions under the assumption that all nations would achieve by 2050 the yields that the temporal trends projected for Group A nations in 2050. As before, yields of each nation were adjusted for their own climate and/or soil and elevation. Group yields and then global yields were then calculated as above. The four curves of cropland cleared in Fig. 3B were calculated from the group yields calculated above and the groups’ 2050 projected caloric demands. Each group’s cropland cleared for a given model at a given N use intensity was calculated using the following equation (Eq. S3): 2050 Cropland Required ¼ ð2050 Area HarvestedÞ × ð2005 CroplandÞ=ð2005 Area HarvestedÞ [S3] and (Eq. S4) Cropland Cleared ¼ ð2050 Cropland RequiredÞ − ð2005 Actual CroplandÞ: [S4] Global cropland cleared is the sum of cropland cleared across all seven economic groups. The greenhouse gas (GHG) emission curves in Fig. 3C were calculated, as described below, using forecasts of global cropland cleared and associated global N use values. GHG emissions were calculated as the sum of GHG emissions from land conversions to cropland and from N fertilizer manufacture and application in accordance with Intergovernmental Panel on Climate Change (IPCC) Tier 1 methodology (8). Calculation and Projections of GHG Emissions from Land Use Conversion. IPCC Tier 1 methodology (8) was used to quantify the following three pathways of global GHG emissions after land conversion to cropland. i) Immediate C release from biomass in year of clearing (c1 = 84 tC ha−1) (Table S6). ii) Annual soil C loss (c20 = 1.195 tC ha−1) (Table S7) during the first 20 y after clearing. iii) Annual N2O release from soil N mineralization (n20 = 0.102 tC eq ha−1) associated with the annual soil C loss during the first 20 y after clearing [using a 100-y global warming potential (GWP) of 298 for N2O] (8). Annual land clearing rates were calculated on a group by group basis, assuming a constant clearing rate between 2006 (mean = 2005–2007) and 2050. Total annual GHG release from land conversion to cropland was calculated using the equation (cropland cleared past year) (c1) + (cropland cleared past 20 y) (c20 + n20). For annual soil C loss during the first 20 y after clearing, we made the conservative assumption that all cleared croplands were on mineral as opposed to organic soils. For each of the five biomes, the appropriate average IPCC default organic soil C stocks (IPCC table 2.3) (8) together with the appropriate average IPCC relative stock change factors for cropland use (Table S7) (IPCC table 5.5) (8) were used to calculate annual 2 of 8 soil C loss for 20 y after clearing with the following formula (IPCC equation 2.25) (8) (Eq. S5): annual soil C loss ðsoil org:C stockÞð1 − stock change factor over 20 yÞ : C20 ¼ 20 y [S5] The average value for all biomes was weighted, as c1 above, by the relative proportion of anticipated land use change, yielding the value of c20 = 1.195 tC ha−1. The annual N2O release from soil N mineralization during the first 20 y after clearing (n20 = 0.102 tC ha−1) was calculated from c20 using IPCC equation 11.8 (8), assuming the IPCC default C: N ratio of 15:1 and default N2O emission factor of 0.01 t(N2O-N) t(N)−1 and converting to tC equivalents using a GWP of 298 (IPCC equations 11.1 and 11.8) (8) (Eq. S6): tC 1t N 0:01t N2 O − N 44t N2 O × × × n20 ¼ c20 ha 15t C tN 28t N2 O − N 298t CO2 12t CO2 − C tC × ¼ 0:102 × : t N2 O 44t CO2 ha [S6] sions from N fertilizer manufacture and application were estimated using IPCC Tier 1 methodology (8): i) CO2 emissions from ammonia production (IPCC table 3.1) (8): good practice default value of 3.273 (tCO2) (t NH3)−1 = 1.08 (tC equiv.) (tNH3-N)−1. ii) Direct N2O emissions from N addition to managed soils: default value (IPCC table 11.1) (8) of 0.01 (tN2O-N emission) (tN input)−1 = 1.28 (tC equiv.) (tN input)−1. iii) Indirect N2O emissions from N volatilization (IPCC equation 11.9) (8): 0.001 (tN2O-N emission) (tN input)−1 = 0.13 (tC equiv.) (tN input)−1. The sum of GHG emissions from these three pathways equals 2.49 (tC equiv.) (tN fertilizer)−1. Multiplying this factor by annual global N fertilizer consumption yields annual global GHG emission values from N fertilizer manufacture and application. We acknowledge the uncertainties with ii and iii above (9). In our analyses, increased N use in underyielding nations gives a net GHG benefit compared with the same crop production on newly cleared land, even if N2O emissions were up to about four times the values used by the IPCC. 7. Alexandratos N, et al., eds (2006) World Agriculture: Towards 2030/2050—Interim Report (United Nations Food and Agriculture Organization, Rome). 8. IPCC (2006) IPCC Guidelines for National Greenhouse Gas Inventories, eds Eggleston S et al. (IGES, Hayama, Japan). 9. Crutzen PJ, Mosier AR, Smith KA, Winiwarter W (2007) N2O release from agro-biofuel production negates global warming deduction by replacing fossil fuels. Atmos Chem Phys 7: 11191e111205. 2 y = -0.6284 + 0.1570*ln(x) - 0.0093*ln(x) 0.10 0.05 0.00 Economic group Specific rate of change of per capita GDP (yr -1) 1. Fargione JE, Plevin RJ, Hill JD (2010) The ecological impact of biofuels. Annu Rev Ecol Evol Syst 41:351e377. 2. Kuznets S (1955) Economic growth and income inequality. Am Econ Rev 45:1e28. 3. Baumol WJ (1986) Productivity growth, convergence, and welfare: What the long-run data show. Am Econ Rev 76:1072e1085. 4. Seldon TM, Song D (1994) Environmental quality and development: Is there a Kuznets curve for air pollution? J Environ Econ Manage 27:147e162. 5. Solow RM (1956) A contribution to the theory of economic growth. Q J Econ 70:65e94. 6. Hawksworth J, Cookson G (2006) The World in 2050: How big will the major emerging market economies get and how can the OECD compete? (PriceWaterhouseCoopers, London). Estimation of GHG Emissions from N Fertilizer Manufacture and Application. The following three pathways of global GHG emis- -0.05 -0.10 0 5,000 10,000 15,000 20,000 A B C D E F G 25,000 Per capita GDP (1990$ International) Fig. S1. Fits of the annual specific rates of change of per capita gross domestic product (GDP) against per capita real GDP from 1961 to 2006 for economic Groups A–G give a Kuznets (1) curve. Note the long-term decline in growth rates as economies become wealthier. In the fitted equation shown, y is dG/dt × 1/G, where G is the per capita GDP, and x is per capita GDP or G. The differential equation is dG=dt ¼ Gð− 0:6284 þ 0:157 × ln½G − 0:0093 × ln½G2 Þ. Using the work by Seldon and Song (2), we solved this differential equation to forecast 2050 values of per capita GDP for each economic group based on 2005 initial conditions. Our numerical solutions used the NDSolve[ ] function of Mathematica. 1. Kuznets S (1955) Economic growth and income inequality. Am Econ Rev 45:1e28. 2. Seldon TM, Song D (1994) Environmental quality and development: Is there a Kuznets curve for air pollution? J Environ Econ Manage 27:147e162. Tilman et al. www.pnas.org/cgi/content/short/1116437108 3 of 8 Population (Billions) 2005-2050 Growth 3.5 2005 Actual 3.0 57% 12% 2.5 2.0 1.5 1.0 143% 40% 15% 22% 0.5 177% 0.0 A B C D E F G Fig. S2. Population in 2005 (black bars) and projected increase to 2050 (white bars; percent increase above) for economic Groups A–G (all nations) from the UN Population Divisions 2009 Medium Variant forecasts (UN Department of Economic and Social Affairs, New York, 2011; http://esa.un.org/unpd/wpp/unpp/ panel_population.htm). Table S1. Analyzed nations in the seven economic groups (A–G) Economic group A B C D E F G A–G 100 analyzed nations used as basis for projections Australia, Austria, Canada, Denmark, Finland, France, Germany, Ireland, Japan, The Netherlands, Norway, Sweden, Switzerland, United Kingdom, and United States Argentina, Chile, Greece, Israel, Italy, Malaysia, Mauritius, New Zealand, Portugal, Saudi Arabia, South Korea, Spain, Trinidad and Tobago, Uruguay, and Venezuela Botswana, Brazil, China, Colombia, Costa Rica, Ecuador, Guatemala, Iran, Jordan, Mexico, South Africa, Syria, Thailand, Tunisia, and Turkey Algeria, Bolivia, Cuba, Dominican Republic, Egypt, El Salvador, Indonesia, Jamaica, Lebanon, Morocco, Paraguay, Peru, Philippines, Sri Lanka, and Swaziland Bangladesh and Pakistan, Benin, Cameroon, Cote d’Ivoire, Ghana, Honduras, India, Libya, Mozambique, Myanmar (Burma), Nicaragua, Nigeria, North Korea, Senegal, and Vietnam Burkina Faso, Eritrea and Ethiopia, Gambia, Guinea, Haiti, Kenya, Madagascar, Malawi, Zambia and Zimbabwe, Mali, Nepal, Rwanda and Burundi, Sudan, Tanzania, Togo, and Uganda Central African Republic, Chad, Democratic Republic of the Congo (former Zaire), Niger, and Sierra Leone Total of all Groups A–G Analyzed percent of world population 2006 (2050) 11.4 (9.4) 4.9 (4.3) 30.2 (24.9) 8.3 (8.6) 28.7 (31.8) 5.9 (9.7) 1.4 (2.8) 90.8 (91.5) Nations were assigned to economic Groups A–G based on their ranking by per capita GDP (average for 2000–2007); Group A had the highest and Group G had the lowest per capita GDP. Of the 100 current nations listed, eight nations have had their data reported by the FAO in composite with another of those eight nations in the past, resulting in the 95 distinct nation/composite data units we used in our analyses. The average population of these 95 nation/ composites was 67 million in 2006. The 128 other nations had a much smaller average population of 4.9 million, and data sets that generally had too many missing points to be usable. Tilman et al. www.pnas.org/cgi/content/short/1116437108 4 of 8 Table S2. Crop categories that encompass the 275 nutritious crops included in our analyses and the percent that each crop contributed to total 2005 kcal production within the 100 analyzed nations Crops (in aggregate) Maize (3) Rice from paddies Wheat (3) Soybeans Oil palm fruit Sugar cane Barley Rapeseed Cassava (4) Sorghum (3) Cottonseed Potatoes Groundnuts Sweet potatoes Sugar beet Millet (7) Coconuts Beans (8) Oats Other fresh vegetables (21) Yams Sunflower seed Bananas Grapes Dry peas (2) Chick peas Plantains Apples (2) Tomatoes Onions Sesame seed Triticale Oranges Rye Cow peas (2) Broad beans (3) Linseed Other cereals (4) Lentils (2) Mangoes and guavas (3) Olives % Crops (in aggregate) % Crops (in aggregate) % 23.56 17.20 15.98 7.43 5.09 3.78 3.23 2.23 2.05 1.99 1.60 1.51 1.38 1.23 1.20 1.01 0.68 0.58 0.56 0.55 0.48 0.44 0.41 0.36 0.30 0.29 0.29 0.22 0.21 0.21 0.18 0.18 0.17 0.16 0.15 0.15 0.13 0.13 0.13 0.12 0.12 Watermelons Pigeon peas Other pulses (6) Cabbages (4) Taro Other fresh fruit (15) Other roots/tubers (10) Dates Green chillies and peppers (3) Eggplants Dry chillies/peppers (3) Tangerines (2) Pears Other tropical fruit (15) Peaches and nectarines (3) Carrots and turnips (2) Cashew nuts Pineapples Lupins Other melons Almonds (2) Green maize Karite nuts Cucumbers Squash and gourds (3) Buckwheat Plums and sloes (2) Mixed grain Green peas Cauliflowers and broccoli (2) Lettuce and chicory (4) Persimmons Green beans Melon seed Walnuts Avocados Spinach Lemons and limes (3) Other oilseeds (12) Safflower seed Other sugar crops (3) 0.11 0.11 0.10 0.10 0.09 0.09 0.09 0.08 0.07 0.07 0.07 0.07 0.07 0.06 0.06 0.06 0.06 0.05 0.04 0.04 0.04 0.04 0.04 0.04 0.04 0.03 0.03 0.03 0.03 0.03 0.03 0.03 0.02 0.02 0.02 0.02 0.02 0.02 0.02 0.02 0.02 Pistachios Hazelnuts Papayas Other citrus fruits (4) Okra (2) Vetches Kapok seed Fonio (2) Apricots Canary seed Strawberries Asparagus Cashew apple Green onions (3) Other nuts (6) Grapefruit (3) Cherries (3) Figs Kiwi fruit String beans Mushrooms (3) Yautia Chestnuts Artichokes Bambara beans Hempseed Other legumes Other berries (5) Quinoa Cranberries Poppy seed Sour cherries Carobs Blueberries Quinces Other stone fruit Raspberries Currants (2) Gooseberries Brazil nuts 0.02 0.02 0.02 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.009 0.008 0.008 0.008 0.007 0.007 0.006 0.006 0.005 0.004 0.004 0.004 0.003 0.003 0.003 0.003 0.002 0.002 0.002 0.002 0.002 0.001 0.001 0.001 0.001 0.001 0.001 0.000 0.000 0.000 (Number) of distinct crops included in a category if the number is more than one. Tilman et al. www.pnas.org/cgi/content/short/1116437108 5 of 8 Table S3. Caloric and protein demand for 2005 and projections for 2050 for the group of 100 analyzed nations and extrapolations to all global nations Per capita demand for analyzed nations* Calories Universal fit Specific fit Mean Protein Universal fit Specific fit Mean Total demand for analyzed nations† Total global demand (all nations)† 2005 2050 Change (%) 2005 2050 Change (%) 2005 2050 Change (%) 1.74 1.74 1.74 2.45 2.50 2.48 41 44 42 10,200 10,200 10,200 20,400 20,800 20,600 99 103 101 11,300 11,400 11,300 22,400 22,900 22,700 98 102 100 0.054 0.054 0.054 0.086 0.077 0.082 58 41 50 323 323 323 722 645 683 123 100 112 355 355 355 790 706 748 122 98 110 The universal fit is a regression, using one data point per nation, of demand against the square root of per capita GDP. In contrast, the specific fit also groups nations by economic group and separately determines the dependence of demand on the square root of per capita GDP by adding an interaction term between economic group and the square root of per capita GDP to the statistical model. The mean is the average of the universal and specific fits. The mean total global demands for calories and protein are the estimates of 2050 demand for the 275 nutritious crops that we use in our 2050 projections. *Units of measure are million kilocalories per year for calories and tonnes protein per year for protein. † Units of measure are trillion kilocalories per year for calories and million tonnes protein per year for protein. Table S4. Fit statistics for the two 1965–2005 regressions of yield against N intensity, precipitation, year, and economic group (four-variable analysis) or against these variables plus potential evapotranspiration, elevation, and soil pH (seven-variable analysis) 1965–2005 Four-variable analysis Parameters Overall Intercept N intensity (N0.75) Precipitation Year Economic group Fit F9, 778 = 338 P < 0.0001 R2 = 0.796 F1, 778 = 77.4 P < 0.0001 F1, 778 = 547 P < 0.0001 F1, 778 = 213 P < 0.0001 F1, 778 = 81.7 P < 0.0001 F6, 778 = 39.6 P < 0.0001 PET Elevation Soil pH Tilman et al. www.pnas.org/cgi/content/short/1116437108 6 Estimate (10 kcal/ha) −103.3 25.7 0.68 0.05 Group A: 3.52 Group B: 0.16 Group C: −0.44 Group D: −0.12 Group E: −1.05 Group F: −0.98 1965–2005 Seven-variable analysis Fit F12, 755 = 259 P < 0.0001 R2 = 0.804 F1, 755 = 76.7 P < 0.0001 F1, 755 = 552 P < 0.0001 F1, 755 = 55.4 P < 0.0001 F1, 755 = 84.8 P < 0.0001 F6, 755 = 30.9 P < 0.0001 F1, 755 = 4.99 P = 0.0258 F1, 755 = 7.58 P = 0.0060 F1, 755 = 10.1 P = 0.0015 Estimate (106 kcal/ha) −103.6 26.6 0.49 0.05 Group A: 3.72 Group B: 0.26 Group C: −0.27 Group D: −0.05 Group E: −1.05 Group F: −1.23 0.01 0.001 −0.50 6 of 8 Table S5. Fit statistics for the two 2005 regressions of yield against N intensity, precipitation, year, and economic group (four-variable analysis) or against these variables plus potential evapotranspiration, elevation, and soil pH (seven-variable analysis) 2005 Four-variable analysis Parameters Fit Overall Intercept N intensity (N0.75) Precipitation Economic group 2005 Seven-variable analysis Estimate (106 kcal/ha) F8, 71 = 30.3 P < 0.0001 R2 = 0.773 F1, 71 = 15.0 P < 0.0001 F1, 71 = 48.5 P < 0.0001 F1, 71 = 26.6 P < 0.0001 F6, 71 = 4.14 P = 0.0013 3.06 30.1 1.03 Group A: 4.32 Group B: −0.24 Group C: 0.19 Group D: −0.12 Group E: −1.21 Group F: −1.47 PET Estimate (106 kcal/ha) Fit F11, 66 = 22.2 P < 0.0001 R2 = 0.787 F1, 66 = 1.85 P = 0.1787 F1, 66 = 47.2 P < 0.0001 F1, 66 = 8.70 P = 0.0044 F6, 66 = 2.49 P = 0.0314 F1, 66 = 0.237 P = 0.6283 F1, 66 = 1.11 P = 0.2952 F1, 66 = 0.563 P = 0.4557 Elevation Soil pH 6.76 30.7 0.87 Group A: 4.47 Group B: 0.39 Group C: 0.33 Group D: 0.14 Group E: −1.37 Group F: −1.93 0.01 0.001 −0.73 Table S6. Calculations of carbon emissions per hectare from land cleared for crops in the first year after clearing based on IPCC Tier 1 methods (1) Biome Cropland use increase weight* Grassland 2 Savanna 3 Tropical forests 4 Mediterranean 1 Southern temperate forest 1 Biomass estimation Mean of four temperate categories in IPCC table 6.4; CF = 0.47 (above- + below-ground biomass) Subtropical steppe in IPCC table 4.12 Mean of three tropical forest categories in IPCC table 4.12; CF = 0.5 Mean subtropical dry forest and subtropical steppe in IPCC table 4.12; CF = 0.5 Temperate oceanic forest in IPCC table 4.12, (see also IPCC figure 4.1); CF = 0.5 Ratio of total to Live Above-ground above-ground biomass biomass biomass loss, year 1 (tC ha−1) (IPCC table 4.4) (tC ha−1) 4.66 N/A 4.66 35.00 1.32 46.20 101.67 1.33 135.22 50.00 1.37 68.50 90.00 1.30 117.36 Weighted average Dead organic matter (IPCC table 2.2) N/A Dead organic Live + dead matter loss, biomass year 1 loss, year 1 (tC ha−1) (tC ha−1) 0.00 4.66 Mean of subtropical value Mean tropical value 3.45 49.65 3.65 138.87 Mean subtropical value 3.45 71.95 20.88 138.24 Mean warm temperate (dry and moist) value 84.0 *4, most use; 1, least use. 1. IPCC (2006) IPCC Guidelines for National Greenhouse Gas Inventories, eds Eggleston S et al. (IGES, Hayama, Japan). Tilman et al. www.pnas.org/cgi/content/short/1116437108 7 of 8 Table S7. Carbon emissions per hectare from land cleared for crops for the 2nd to 20th y after clearing based on IPCC Tier 1 methodology and land use changes (1) Biome Cropland use increase weight* Grassland 2 Savanna 3 Tropical forests 4 Mediterranean 1 Southern temperate forests Weighted average 1 Soil climate region (IPCC table 2.3) Mean four temperate categories Mean tropical dry and tropical moist Mean three tropical categories (excluding tropical montane) Mean of warm temperate dry, moist and tropical dry, moist Mean two warm temperate categories Initial soil Stock change factor Soil organic C stock Annual soil C loss from organic C stocks climate region change factor, croplands cropland years 1–20 (tC ha−1) (IPCC table 5.5) (over 20 y) (tC ha−1) 65.09 0.745 0.830 54.70 Mean temperate/ boreal; dry, moist Mean tropical 0.530 1.285 62.20 Mean tropical 0.530 1.462 56.95 Mean tropical, temperate/boral; dry, moist Mean temperate/ boreal; dry, moist 0.638 1.032 0.745 0.755 59.20 1.195 *4, most use; 1, least use. 1. IPCC (2006) IPCC Guidelines for National Greenhouse Gas Inventories, eds Eggleston S, et al. (IGES, Hayama, Japan). Tilman et al. www.pnas.org/cgi/content/short/1116437108 8 of 8
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