June 2009

Projecting , Projecting Population in IPCC Scenarios

Malea Hoepf Young Kathleen Mogelgaard Karen Hardee

PAI WORKING PAPER WP09-02 Population Action International

uses research and advocacy to improve access to and reproductive

health care across the world so women and families can prosper and live in balance

with the earth. By ensuring couples are able to determine the size of their families,

poverty and the depletion of natural resources are reduced, improving the lives of

millions across the world.

2 Projecting Population, Projecting Climate Change Population in IPCC Scenarios

PAI WORKING PAPER WP09-02

3 INTRODUCTION While population is widely recognized as one of the driving forces behind the growth of emissions, this paper shows that it is not adequately accounted for in the emissions scenarios produced in the Special Report on Emissions Scenarios (SRES) of the Intergovernmental Panel on Climate Change (IPCC). The paper examines the assumptions about fertility, mortality and migration that are built into the low, medium and high variations of the population projections used in scenarios of emissions growth. The SRES shows the implications of changes in population size on emissions, but fails to account for other demographic trends such as , age structure, and household composition. As a result, the SRES likely underestimates demographic impacts on emissions growth. Furthermore, the fertility decline assumptions contained in population projections in the SRES may be over-emphasized given recent declines in political and financial support for policies strongly tied to fertility decline, such as education and equality for women and access to reproductive health and family planning services. The paper concludes that a deeper and more nuanced understanding of the emissions implications of population size, age structure, household size, and urbanization should be incorporated into climate change scenarios that provide the basis for policy decision-making and strategy development for climate change mitigation and adaptation.

4 “By 2100, the world will have changed at which demographic factors underlie the Scientists generally in ways difficult to imagine—as dif- climate science community’s projections of accept that population ficult as it would have been at the end future climate change. size influences global GHG of the 19th century to imagine the The paper describes the devel- changes of the 100 years since.” The emissions, although the role opment of the IPCC’s scenarios, Special Report on Emissions Scenarios of demographics is complex explores the population projec- (Naki´cenovi´c et al. 2000) tions that were used, and explains the and involves significant Climate change is one of the most serious assumptions behind those projections. uncertainty. challenges human society will confront in The paper concludes that the as- the coming decades, and throughout the sumptions made about falling fertility course of the next century. Human produc- and slowed may tion of greenhouse gas emissions (GHGs), be over-emphasized, and that by not largely through the burning of fossil fuels, is taking into account important demo- expected to warm the earth’s surface. This graphic variables beyond population will lead to rising sea levels, changes in pat- size, the scenarios have underestimat- terns of precipitation, heat waves, drought, ed potential demographic impacts on flooding, and increasingly damaging storm greenhouse gas emissions growth. surges. All of these have potentially severe Understanding the strengths and weak- consequences for both humans and ecosys- nesses of the SRES can help shed light on tems. strategies for effectively addressing climate The full range of climate change impacts change, as its scenarios have been used over the course of the next century is dif- for much of the major climate research up ficult to ascertain, both because of uncer- to the present, the results of which have tainty surrounding how the earth’s complex been and will continue to be widely used by physical and environmental systems will policymakers. The IPCC’s next assessment, change, and how much total emissions will due in 2014, will employ a new process of grow. Changes in emissions and subsequent scenario development, and this paper briefly environmental impacts will be affected by fu- describes that process, now in its incipient ture development patterns around the world. stages. Because all population projections The climate science community attempts used in the SRES include in their assump- to understand the range of uncertainty tions large declines in fertility over the next of climate change impacts by developing century, The paper concludes by addressing scenarios–such as those included in the In- the role population policies might play in tergovernmental Panel on Climate Change’s the context of comprehensive solutions to (IPCC) Special Report on Emissions Scenari- climate change. os (SRES)–exploring the range of factors that The IPCC and its influence emissions. These scenarios are assessment reports: then used to drive climate models that show Development and use a range of projected change and impacts. “This report reinforces our under- Scientists generally accept that population standing that the main driving forces size influences global GHG emissions, al- of future greenhouse gas trajectories though the role of demographics is complex will continue to be demographic and involves significant uncertainty. This change, social and economic devel- paper identifies important points opment, and the rate and direction 5 of technological change.” The Spe- tion of the 1992 United Nations Framework cial Report on Emissions Scenarios Convention on Climate Change (UNFCCC), (Naki´cenovi´c et al. 2000) the treaty that provides the current policy framework for addressing climate change. In the late 1980s, the UN’s World Meteoro- The First Assessment Report also identified logical Organization and the United Na- gaps in understanding and future research tions Environmental Program established needs, and it underlined the need for reports the Intergovernmental Panel on Climate geared towards policymakers to bridge the Change (IPCC). It was created to assess and gap between the policy and climate sci- synthesize the state of scientific thinking ence communities. The Second Assessment on human-induced climate change. Ini- Report, published in 1995, provided input tially tasked with gathering climate change for the negotiations of the Kyoto Protocol evidence into its First Assessment Report, in 1997. The Kyoto Protocol is an addition to published in 1990, the IPCC remains the key the UNFCCC treaty, and is a legally bind- organization in coordinating research efforts ing agreement to reduce GHG emissions and compiling results, as well as translating in industrialized countries. The gathered re- evidence for non-scientific communities, search stated that “the balance of evidence particularly policymakers. Today, the IPCC’s suggests a discernible human influence on assessment process involves over 2,500 global climate,” a finding that was further scientists from over 150 countries, with the enforced in the Third Assessment Report majority drawn from the natural sciences. published in 2001 (IPCC 1995, IPCC 2001). The IPCC has three standing working groups that contribute reports to the IPCC’s periodic The Fourth Assessment Report was released assessments: in 2007. In addition to providing stronger scientific evidence that climate change is n Working Group I assesses the physical occurring and that it is caused by human science of climate systems and climate activities, the report also included a section change and produces the report, The entitled “Historical Overview of Climate Physical Basis for Climate Change; Change Science,” which stated that in recent n Working Group II assesses the vulnerability decades research in climate change has of societies and natural systems to climate accelerated dramatically and developed new change impacts and produces the report, methodology and tools such as complex Impacts, Adaptation and Vulnerability modeling. While climate change science n Working Group III assesses options to literature had barely emerged before 1951, it mitigate climate change, and produces the tripled between 1965 and 1997 (Le Treut et report, Mitigation of Climate Change. al. 2007). A special task force of the IPCC works on This proliferation of research has occurred National Greenhouse Gas Inventories (IPCC as models of the earth’s processes have 2004). become increasingly complex, with new The Assessment Reports produced by the factors included. Faster computer speeds IPCC have been extremely important to both allow scientists to increase the number, the research and policymaking communities, complexity, and resolution of the models. providing increasingly detailed information As this information is compiled, the result on all aspects of future climate change. The is a more complete picture of a range of First Assessment Report was published in possible climate futures. Using this range 1990 and formed the basis for the negotia- of possible climate futures, scientists can 6 project impacts of climate change on natural ers. Modelers then delivered their results to and human systems, examine the resilience the impacts assessment and vulnerability of these systems, and develop plans to ad- community, who use this information as the dress both the causes and consequences basis for their research. The next round of of climate change. The basis for all of this scenario development, which will contribute research is the IPCC’s emissions scenarios to the Fifth Assessment Report expected (Le Treut et al. 2007). in 2014, will take advantage of a different approach. Scenario development and climate The IPCC’s Emissions modeling will occur simultaneously and Scenarios use set levels of radiative forcing, resulting “Scenarios are images of the future, from representative concentration pathways or alternative futures. They are neither (RCPs) of GHG emissions. predictions or forecasts. Rather, each The IS92 scenarios formed the basis of the scenario is one alternative image of second assessment report in 1995. How- how the future might unfold… they ever, after that report and a 1994 evaluation, enhance our understanding of how the IPCC announced that because of the systems behave, evolve, and interact… community’s increased understanding of given the uncertainties in both emis- energy supply and non-CO2 GHG emissions, sions models and our understanding and because of a need to explore different of key driving forces, scenarios are an development pathways that show a narrow- appropriate tool for summarizing both ing gap between industrialized and develop- current understanding and current ing countries, it was appropriate to create a uncertainties.” The Special Report on new set of scenarios (Houghton et al. 1994). Emissions Scenarios (Naki´cenovi´c et Begun in 1996 by a group of six modeling al. 2000) teams, the Special Report on Emissions Emissions scenarios project alternative Scenarios (SRES) was published in 2000, paths of greenhouse gas emissions into the and presents projections of future emissions future. Like other aspects of climate science, that could result from different pathways of emissions scenarios have become much demographic, socio-economic and techno- more sophisticated over time, and employ logical development. The authors analyzed increasingly complex patterns of socioeco- existing scenarios in the published literature, nomic, demographic, and technological including their major characteristics, driv- change throughout the world. The IPCC has ing forces, and relationships. The scenarios produced three sets of scenarios: the 1990 represent the range of scenarios in the Scientific Assessment (SA90) with four literature, excluding outlier and “disaster” scenarios, the IPCC Scenarios 1992 (IS92) scenarios. While the scenarios explicitly proj- with six scenarios, and the 2000 SRES with ect a world without climate change mitiga- 40 quantitative scenarios, grouped into four tion policies, authors were asked to identify families, each with a qualitative narrative policies that could affect GHG emissions, storyline describing possible futures and such as efforts to reduce sulfur dioxide in combinations of driving forces (Naki´cenovi´c response to poor air quality and acid rain. et al. 2000). In the past, the IPCC completed Most of the scenarios do anticipate change its scenarios, converted the resulting GHG to cleaner technologies (Naki´cenovi´c et al. emissions to levels of radiative forcing,1 2000). and gave these results to -

7 Each storyline in the SRES The 2000 SRES scenarios cover a relatively or less credible than the other scenarios tells a story of a potential long time period, from 1990 to 2100, in order (Naki´cenovi´c et al. 2000). to express the long-term nature of climate future world. The SRES was explicit about the limitations change, but the authors acknowledged the and appropriate uses of the 40 scenarios, uncertainties involved in projections over stating that they are not policy recommenda- such a lengthy period. The scenarios address tions, none are more or less likely than the uncertainties about the future by locating the others, and none should be construed as scenarios within “storylines,” which make means or medians (the choice of an even certain assumptions about the trajectories number of scenarios was meant to avoid a of three broad categories of human activity, single scenario being construed as a central termed “drivers.” The drivers include popu- or “best guess” projection). The authors lation dynamics (based on three different advised that it was important for those who projections of population growth), economic use the scenarios for modeling or other development, and technological change. Un- purposes to utilize more than one family to like the IS92 scenarios, the SRES scenarios reflect the range of uncertainty surround- showed projections of change in human ing the drivers and emissions outcomes societies, not just changes in the result- (Naki´cenovi´c et al. 2000). ing greenhouse gas emissions (GHG). The authors developed four narrative storylines The SRES scenarios represent an improve- to describe a variety of possible futures, and ment over the IS92 scenarios because of quantified the storylines using integrated as- They connect changes in improved baseline measurements of emis- sessment models. While the scenarios were sions, and more types of GHGs included the number of people in developed under the auspices of the IPCC in the analysis. The SRES also includes the world and the way that (a unique instance in which the IPCC played projections of economic change and devel- a role in conducting rather than synthesizing they live to how much they opment throughout the world, and rates of research), the scenarios and their assump- technological change. The resulting scenarios emit, and subsequently, tions underwent an extensive open review explore a higher bound of emissions than through the work of climate process and several revisions. The resulting the IS92 scenarios, but did not extend the modelers, to how their scenarios created the emissions levels that lower bound. Also in contrast to the IS92 form a basis for models of climate change actions impact global scenarios, the SRES includes some fami- (Naki´cenovi´c et al. 2000). lies in which the gap in per capita income climate change. between more and less developed countries The SRES outlines 40 scenarios of future narrows over time, and overall, assumes a GHG emissions2—both globally and for a more affluent world in the future than exists group of four regions. As noted earlier, there today (Naki´cenovi´c et al. 2000). are four qualitative storylines telling a differ- ent story about the world’s future develop- The SRES was a critical step forward in the ment. Under each storyline, there is a family development of climate models that take of quantitative scenarios showing the GHG into account human population growth and emissions resulting from a combination of activities, and continues to be very important drivers compatible with the storyline. Within in the climate community. Research based the 40 scenarios, the authors chose an illus- on the SRES will be used until the IPCC’s trative marker scenario as most representa- Fifth Assessment Report in 2014 for major tive of each storyline. While these scenarios policy decisions and other research; thus is have received the most scrutiny and are it important to understand the scenarios and the most frequently used, they are no more their assumptions.

8 Table 1: The Four SRES Families of Scenarios CO2 emissions Temp change in marker sce- (degrees Scenario Population Population in Population in Economic growth/technological nario in 2100 Celsius) by Family projection used 2050 (billions) 2100 (billions) change assumptions (GtC/year)3 2090-20994

IIASA 1996 Very rapid economic growth; rapid A1B: + 2.8 A1 – low variant 8.7 7.1 introduction of more efficient 13.83 A1T: + 2.4 (revised) technologies A1FI: + 4.0

Per capita economic growth and IIASA 1996 – A2 11.2 15 technological change slower and 28.19 + 3.4 high variant more fragmented

Rapid change in economic IIASA 1996 structures toward service and B1 – low variant 8.7 7.1 4.04 + 1.8 information economy; clean and (revised) efficient technologies

UN 1998 – long- Intermediate levels of economic B2 range medium 9.3 10.4 development; less rapid and more 13.32 + 2.4 projection diverse technological change

Sources: Naki´cenovi´c et al. 2000; Le Treut et al. 2007.

The SRES storylines it is today: by 2100 world GDP estimates range from 10 to 26 times higher than 1990. Each storyline in the SRES tells a story of Along with greater affluence, many sce- a potential future world. The SRES sce- narios assume greater equality between narios have both qualitative and quantitative today’s developed and developing countries. aspects—a narrative storyline with associ- Forest area continues to decrease in most ated quantitative information. They connect scenarios, but this trend eventually reverses changes in the number of people in the (Naki´cenovi´c et al. 2000; Van Vuuren and world and the way that they live to how O’Neill 2006) much they emit, and subsequently, through the work of climate modelers, to how their Characteristics of the SRES actions impact global climate change. Storylines and Families of Scenarios

There are four storylines and associated The A1 storyline and family of scenarios is families of scenarios: A1, A2, B1, and B2. characterized by a low population trajectory The “A” scenarios place more emphasis on and rapid economic growth. This storyline economic growth, while the “B” scenarios uses the International Institute for Applied place more emphasis on environmental pro- Systems Analysis (IIASA) 1996 low variant tection. The “1” scenarios assume greater projection of ,5 which proj- globalization, while the “2” scenarios show ects a world of 8.7 billion people by 2050, a more regional, less connected world (for which then declines to 7 billion by 2100. a comparison of the major characteristics Alongside assumptions about continued low of the families, see Table 1). Several trends fertility in parts of the world such as Eu- span multiple storylines. All scenarios show rope, this projection also assumes dramatic a world that becomes more affluent than declines in fertility in areas where fertility is

9 currently high. For example, in sub-Saharan the importance of technological change in Africa, fertility would fall from 5.9 in 2000 pathways of future emissions. Controlling to 1.8 in 2050 (Lutz 1996). Additionally, the for demographic and socioeconomic fac- A1 storyline projects the development and tors, different patterns of technology and adoption of new, more efficient technolo- resource use can result in very different gies. It also describes a world with greater levels of emissions. The fossil-intensive cultural and social interaction, and a reduc- A1F1 scenario leads to some of the highest tion in the gap between incomes in devel- CO2 emissions of all the scenarios, while oped and developing countries. the alternative-energy emphasis of the A1T results in some of the lowest. The A1 storyline is unique in that it was chosen to examine different future paths of In contrast, storyline A2 assumes a more energy use. Within the A1 family of sce- heterogeneous world, with regional differ- narios, there are three groups of scenarios— ences in development, slower and more A1FI, A1T, and A1B– with similar develop- fragmented economic growth, and slower ment pathways, but very different projected technological change. This storyline also energy use. The A1FI scenarios are fossil assumes higher population growth (IIASA’s fuel intensive, the A1T scenarios are non- high variant), with global population reaching fossil fuel intensive, while the A1B group 15 billion by 2100—over twice the projection is balanced across sources. The emissions of the A1 storyline. Under this scenario, total projection results from these groups show fertility rates—the number of children the

Figure 1: Population changes and carbon emissions under different IPCC SRES Scenarios 16 30

POPULATION

14 HISTORICAL 25 A2 12 B2 CARBON EMISSION (GtC/YEAR) 20 10 A1 / B1

8 15 CARBON EMISSIONS 6 POPULATION (BILLIONS) POPULATION HISTORICAL 10 A2 4 A1 5 2 B2

B1 0 0 2010 2100 1950 1960 1970 1980 1990 2020 2030 2040 2050 2060 2070 2080 2090 2000 Source: Jiang and Hardee 2009. 10 average woman has in her lifetime­—decline this storyline spans the lowest end of the in various regions, but global fertility remains range of SRES scenarios. above replacement level6 by the end of the Finally, storyline B2 illustrates a world that century, following the IIASA high variant develops localized solutions to sustainability, projection. Furthermore, the A2 storyline has while experiencing a continuously growing largely negative environmental implications. population (although at a slower rate than This is the only scenario in which forest A2) and intermediate development and cover continues to decline through 2100, technological change. Its results are based and the associated CO2 emissions from on the 1998 long-range UN medium fertility this change continue to grow. Further, the variant population projection, which results high population growth is paired with slower in 10.4 billion people by 2100. This storyline increases in agricultural productivity than in describes a more equitable world with more other scenarios, leading to higher nitrous environmental protection, but with solutions oxide and methane emissions from land generated at the regional and local levels. use, as opposed to the A1 and B1 storylines, Under this scenario, about half of the world’s which see limited amounts of these emis- energy comes from non-fossil fuels, with sions. The shift in energy under A2 is marked the remaining half split between coal, oil by transition away from oil and gas, and back and gas. The corresponding emissions levels to coal as an energy source, with a moder- under this scenario span an intermediate ate increase in non-fossil energy sources. range by 2100. The resulting emissions under this storyline span from medium to high, although not Emissions from the SRES Scenario as high as the A1F1, fossil fuel-intensive Families scenario, mainly because there is much slower economic growth in the A2 storyline As noted throughout, the scenarios cover a (Naki´cenovi´c et al. 2000). wide and overlapping range of emissions, widening over time with increased uncertain- Storyline B1 describes a world in which in- ty in the long term. The range of total GHG come gaps between rich and poor countries emissions in the SRES reflects the range in are reduced, with rapid economic change the published literature (excluding outlying and shifts to an information and service “disaster” scenarios). By 2100, estimates economy. This storyline uses the same popu- of total cumulative CO2 emissions range lation projection as A1 (IIASA’s low variant), from 700 to 2540 gigatons. The scenarios projecting 8.7 billion people by 2050 and a also show that different development paths decline to 7 billion by 2100.In this storyline, can result in similar GHG emission levels, there is extensive use of clean and resource- and different driving forces (demographic, efficient technology, with widespread development, and technological change) exchange of technology across regions, and can result in very different emissions levels. an improvement in economic equity around Thus, the range of emissions levels overlap the world. Under this scenario, CO2 emis- significantly between families and, impor- sions from loss of forest cover decrease at tantly, no single driver is a determining factor the fastest rate among the four families of of emissions, as they all have very different scenarios, as population declines and agricul- outcomes in different combinations of other tural productivity increases. A large share of drivers. For example, regional per capita energy comes from renewable and nuclear income convergence (e.g., more equitable sources. The range of carbon emissions from economic development) can lead to high or

11 low emissions. Also, in the A1 storyline, eco- of low, central, and high estimates of these nomic and demographic changes were held three factors, resulting in 27 projections constant, but different shifts in technology for 13 world regions. Emphasis is given to resulted in very different emissions out- those combinations that are most intuitive, comes among the scenarios in this family. i.e., high mortality and high fertility, and low Thus, all driving forces should be considered mortality and low fertility, in the two IIASA when developing mitigation strategies. projections used in the SRES. These are also referred to as slow and rapid demographic Population Projections transition variants. Just as in the UN medium and the SRES projection used in the B2 storyline, both of “Population projections are argu- these projections show a world population ably the backbone of GHG emissions that will grow substantially, will age substan- scenarios.” The Special Report on tially, and will be increasingly concentrated in Emissions Scenarios (Naki´cenovi´c et today’s developing countries (Lutz 1996). al. 2000) In IIASA’s low variant projections, global aver- As noted in Table 1, and illustrated in Figure age fertility rates fall from 2.81 in 1995-2000 1, the SRES scenarios utilize three popula- to 1.39 in 2100. This drop is most dramatic tion projections: the 1998 UN long-range in sub-Saharan Africa, where fertility rates projection, and IIASA low fertility and low fall from 5.87 to 1.44 over this period (Lutz mortality variant, and the IIASA high fertility, 1996). For use in the SRES storylines A1 and high mortality variant. Their assumptions are B1, IIASA modified their projection in this important to understand, and are detailed category slightly. Rather than the population below. estimates of 8.5 billion in 2050 and 6.5 billion in 2100, the projections are slightly higher at IIASA Projections: Storylines A1, A2, 8.7 in 2050 and 7.1 in 2100. This adjustment and B1 was made to project more rapidly decreas- ing mortality rates in developing regions that The IIASA variants were chosen as the high better correspond with the narrative story- and low population projections for the SRES line describing more rapid economic growth in part because they are probabilistic, in that in industrialized and developing countries they assign a probability distribution to cover alike (IIASA 2007). However, in the original the range of current knowledge of uncertain- population projection (before it was altered ty around future world population growth. for use in the SRES), increases in life expec- The intervals of the full population projection tancy under this scenario were still dramatic, are between 6.7 and 15.6 billion by 2100, increasing from 65.4 years in 2000 to 84.3 representing 90 percent of the range of years in 2100. uncertainty in the literature (between the 5th and 95th percentile).7 This range was The A2 storyline, marked by slower and developed by inviting experts on the factors more fragmented economic growth and contributing to population growth (fertility, technological change, has the highest mortality, and migration) to provide high and population projection. This upper bound was low estimates for each of these factors for created by IIASA’s high fertility, high mortality 2030-2035. The factors were then extended scenario. Under this scenario, fertility rates to 2080-2085 and held constant until the remain above replacement, at 2.86 in 2050, end of the century. The IIASA projections and 2.40 in 2100. The result is a world of are composed of all possible combinations 15 billion people by the end of the century. 12 Life expectancy remains low, at 64.0 years, lation size is projected to grow worldwide increasing less than a year over the course even though the projection shows that all of the 21st century. The gap in life expec- regions converge to just above replacement tancy between industrialized and developing level fertility by 2050, and fall to replacement regions under this scenario is more than 14 of 2.1 births per woman shortly thereafter. years larger in this than in the low fertility, This assumes both a dramatic drop in fertility low mortality scenario described above (a in the less developed regions– particularly gap of 14.6 years vs. 11.2 years). Africa– and increases in fertility rates in North America, Europe, and China that have UN Medium Projection—Storyline not yet been observed (fertility rates are B2 currently 4.7 for Africa, and 2, 1.5, and 1.7 for Storyline B2 (marked by localized solutions North America, Europe, and China, respec- to sustainability) utilizes the 1998 long-range tively) (UN Population Division 2007). Slight UN medium fertility variant projection. Under adjustments are made in replacement level this projection, fertility stabilizes at replace- fertility to match the projected increases in ment level (2.1) and global population grows life expectancy over the long term, so that from 5.7 billion in 1995 to 9.4 billion in 2050 replacement level fertility comes closer to and 10.4 billion in 2100. Population continues 2.0 than 2.1 (UN Population Division 1998). to grow before stabilizing at fewer than 11 Aside from fertility, the other factors con- billion people by 2200. The SRES authors tributing to population growth and change chose this projection because of its wide- are mortality and migration patterns. In the spread use and its assumption of replace- population projection used for B2, mortality ment level fertility. It is also remarkably close is projected to decline in all regions, with life to the IIASA central fertility and mortality expectancy projected to accelerate faster scenario of 10.35 billion people in 2100, in the areas currently experiencing higher despite using significantly different method- mortality. Thus the gap in life expectancy ologies (UN Population Division 1998; Lutz between more and less developed countries 1996). narrows from 13 years in 1995 to less than The 1998 UN long-range population projec- four years by 2150, and global life expec- tions were based on the UN’s 1996 near- tancy increases worldwide by 21 years, term population projections, which extended from 62.2 years and 66.5 years for men and to 2050, and follow the same assumptions. women, respectively, in 1995, to 83.4 years The 1996 projections were developed with for men and 88.2 years for women in 2150. improved information on fertility patterns While migration plays a role in population (particularly in sub-Saharan Africa), and also size and structure at the regional level, none extend the upper bounds of life expectancy of the 1998 projections assume net migra- to 82.5 years for men and 87.5 years for tion for the regions after 2025, because, as women. The end result is a lower total popu- the UN report states, “international migra- lation figure than that used in the IS92 sce- tion patterns are highly unpredictable in the narios that preceded the SRES (Naki´cenovi´c long run” (UN Population Division 1998, 10). 1997; UN Population Division 1998).8 This The dramatic changes in fertility observed population projection assumes an increase in the medium variant of the UN population in population size in all areas of the world projection lead to dramatic population aging except Europe, which would decline in size worldwide by 2150, with the median age of by 18 percent over the next 155 years. Popu- the world’s population rising from 25.4 in 13 Since the publication of 1995 to 36.5 in 2100. In turn, the share of fertility at a rate of 1.85 children per woman the SRES in 2000, the UN global population under age 15 will decline for a period of around 100 years, before ris- from 31.3 percent of the world’s population ing again to replacement levels (UN Popula- has updated and refined in 1995 to 20.5 percent in 2100. The propor- tion Division 2004). their long-range population tion of the population over 65 and over 80 In terms of the other factors in population projections, with significant will also increase. While this significant shift growth, the UN’s 2004 long-range population in population composition is likely to have implications for projected projection revision extends projections of mi- implications for energy use, these implica- gration out to 2050, rather than to 2025, but population outcomes. tions were not considered in the develop- migration falls to zero after that point. During ment of the SRES. the period when it is incorporated into the Updates to the UN and IIASA projections, migration prevents a more rapid Projections decline in population growth rates in devel- oped countries because they are projected Since the publication of the SRES in 2000, to continue to receive immigrants from other the UN has updated and refined their countries. Life expectancy does not have an long-range population projections, with upper bound in the new projections, with significant implications for projected popula- a range between 87 and 106 years in 2300 tion outcomes. The most recent version of (because mortality rates have already de- the UN’s long-range population projections clined significantly in all regions, increases in was published in 2004, and includes some life expectancy contribute far less to popula- notable changes in methodology and results. tion growth than fertility rates) (UN Popula- World population under the medium projec- tion Division 2004). tion reaches 8.9 billion in 2050, peaks at 9.2 billion in 2075, and falls to 9.1 in 2100. This Like the UN, IIASA has since updated their is significantly lower than the 1998 projec- population projections, and has shown lower tion included in the B2 storyline, in which population growth under all scenarios in global population reaches 9.3 billion in 2050 the medium and long term. The confidence and 10.4 in 2100. The changes resulted from interval for population in 2100 in the new improved baseline information from more population projection spans 6.2 to 11.1 bil- and better national census data than were lion, significantly lower than the projections previously available. The projections also used in the SRES, suggesting that the 15 changed assumptions about fertility, assum- billion estimates used in the A2 scenario, ing that fertility will fall below replacement representing more than a doubling of today’s levels, and then increase again to stabilize population, has a less than 2% likelihood at replacement. Although the updated 2004 of occurring (Van Vuuren and O’Neill 2006). projection does not project all countries While all of these trends have potential to reach or go below replacement levels implications for GHG emissions trends, by 2050, it does assume that once fertility these refined population projections are not rates reach four to five births per woman in currently reflected in the SRES. current high fertility countries, the decline in fertility accelerates. As a group, less devel- oped countries are projected to undergo the most dramatic demographic changes, with fertility falling from 3.1 currently to 2.04 (below replacement) by 2050. Each country is expected to converge below replacement 14 Demography and the SRES ic production), the amount of energy used The trend in changing Scenarios per unit of economic production (energy household size is closely intensity), and the amount of CO2 emit- tied to population aging. As “Broadly speaking, demographic ted per unit of energy produced (carbon change, changes in economic output, intensity). Many other factors influence age, the number and changes in the GHG intensity of these determinants, such as the stage of of people per household the global economy are the forces that industrialization (service-oriented economies tends to fall, which results drive GHG emissions. Each of these tend to have lower energy intensity). Their is, in turn, influenced by a number of multiplicative relationship means that chang- in a loss in economies of important indirect variables.” Popula- es in one variable are amplified or mitigated scale in energy use. tion, Greenhouse Gas Emissions, and by the others (e.g., population increase in a Climate Change (O’Neill et al. 2004) country of high per capita GDP would have a greater impact than that in a country with In its discussion of the main driving forces low GDP) (O’Neill et al. 2004). of climate change, the SRES explains the scenarios’ conceptions of population, but While the Kaya Identity underpins the treat- the authors are careful to avoid suggesting ment of population in the process of sce- a linear relationship between population nario development in the SRES, the authors and emissions, emphasizing that relation- of the SRES acknowledge that total popula- ships among drivers of GHG emissions are tion size has less direct relation to emis- very complex. The report states that the sions than other demographic units, such relationships can be expressed as the I=PAT as households. However, the authors of the Identity, in which: SRES faced the limitation that nearly all the integrated assessment models in the litera- ture used to develop the scenarios are based Impact = Population × Affluence on population size at the regional level, thus × Technology precluding scenarios based on factors.

This implies that the level of emissions re- The trend in changing household size is sults from the size of population, multiplied closely tied to population aging. As popu- by affluence and the level of technology lations age, the number of people per (Naki´cenovi´c et al. 2000). This conceptualiza- household tends to fall, which results in a tion has been used to describe the impact of loss in economies of scale in energy use. human activities on a range of environmental Household size shrinks as older people tend issues (O’Neill et al. 2004). to live alone, or as couples live in house- holds longer without children. Due to aging, When examining climate change, a variation under both the medium and low population on the I=PAT Identity, known as the Kaya projections used in the SRES, the number Identity, is often used. The Kaya Identity is of households will grow faster than popula- expressed as: tion in developing and developed counties alike, although this may unfold differently CO2 emissions = Population × (GDP/Popula- in developing countries where multigenera- tion) × (Energy/GDP) × (CO2/Energy) tional households are still common. Because of this, the SRES authors note that the rapid In the Kaya Identify equation, annual CO2 aging expected in the next century could emissions are the product of population, significantly increase CO2 emissions more per capita income (or per capita econom- than currently accounted for in the SRES, 15 but say that at the time of the report’s pub- size on emissions scenarios. Assuming that lication, uncertainties surrounded this effect household emissions grow at the same rate (Naki´cenovi´c et al. 2000). as per capita emissions, under a scenario of central population growth and emissions, The SRES also discussed the potential emissions are 25 percent higher in 2100 in a effect of urbanization on emissions. The model using households as its demographic report stated that urbanization is likely to unit than those using population size alone. increase emissions, mainly through a func- The 25 percent difference between the two tion of increased income, as the promise of makes it important for modelers to include higher income drives rural-urban migration, households in their analyses (O’Neill et al. higher incomes result in more fossil fuel 2004). use in households, and transportation use increases. However, neither the effect of Population in Post- urbanization nor population aging is explicitly SRES Scenarios and addressed in the SRES scenarios. the Representative Concentration Pathways O’Neill and colleagues addressed some of Process these issues subsequent to the publication of the SRES, noting that the SRES analysis The SRES scenarios were published in 2000 could have explored population and emis- and were based on data from the mid-1990s. sions relationships by holding other drivers Because these scenarios were used for the constant and examining the outcomes, as IPCC Fourth Assessment Report, published was done for energy under the A1 scenario. in 2007, it is important to assess their perfor- In 2004, O’Neill, MacKellar and Lutz conduct- mance against updated historical data and ed a simple sensitivity analysis, using the against emissions scenarios published since 1996 IIASA projections and IS92 scenarios, 2000. The IPCC’s Working Group on Mitiga- examining the model’s sensitivity to changes tion–Working Group III–conducted such a in population. In their analysis, the authors review in its Working Group Report for the found that total emissions in the medium Fourth Assessment Report. This review term (to 2050) are much more sensitive documents the scenarios published in the to changes in per capita emissions than literature since the publication of the SRES to differences in population size (using the and compares the new scenarios with those central vs. the low population projections). used in the SRES. The report found that the The results found a significantly larger differ- emissions ranges identified in the post-SRES ence between a scenario of central and low scenarios did not vary significantly from per capita emissions than between central the SRES ranges. While the Working Group and low population projections. However, in Report notes that population projections 2100, the opposite occurs; the difference is have been lowered since the publication of much more pronounced in scenarios with the SRES, they conclude that many of the different populations. When a central per new scenarios still use more dated popula- capita emissions scenario was assumed, a tion projections. Review of the literature low population projection led to 37 percent also found that while lower population levels less total emissions than the central popula- are generally associated with lower emis- tion scenario. sions, scenarios that do incorporate the new population figures had largely unchanged O’Neill, MacKellar and Lutz also conducted emissions results, because changes in other sensitivity analyses for aging and household contributors to emissions, such as economic 16 growth and energy use patterns, offset the develop their scenarios of atmosphere, cli- effects of lower population figures (Fisher mate, and related changes, such as sea level et al. 2007). The report drew heavily on a rise and ocean acidification. This is an impor- review by Van Vuuren and O’Neill, who found tant change from the sequential procession that most of the SRES data ranges remain from scenario development to climate mod- credible, and thus a large-scale update of eling and then to adaptation and impacts the scenarios was not necessary in the near assessment used in previous assessment term. They emphasized, however, that new reports. This extra time also allows climate scenarios should consider lower population modelers to make projections out to both growth— using smaller population size at the near (2035) and long terms (2300). At the the low end of the range of estimates, as same time, integrated assessment modelers well as a smaller population size under the will develop RCPs into a suite of scenarios high population projection. Particularly at that include a range of technological and the highest ends, the authors conclude that policy options. The scenario development the high population estimate included in the and impact assessment, adaptation and SRES “strains credibility,” falling as it does vulnerability communities can work together outside the 90 percent confidence interval to develop narrative storylines, before all of future population (Van Vuuren and O’Neill, the various pieces are ultimately integrated 2006). and aligned for the publication of the IPCC’s Fifth Assessment Report in 2014 (Moss et al. While the SRES scenarios have been found 2008). This new phase of development is an to be relatively robust, as mentioned earlier important opportunity to include improved they are being replaced by new scenarios consideration of demographic and popula- that are currently under development. The tion variables discussed in the SRES and new scenarios have important differences, subsequent research, including household both in their structure and development level analysis, and consideration of aging and process. Requests from policymakers have urbanization on regional and global emis- led to the inclusion of scenarios that assume sions pathways. climate mitigation efforts, including one that reflects very stringent emissions reduc- Population Policy and tions. Also, the IPCC will be less involved Climate Change in scenario development, acting instead as While the IPCC includes population in its a catalyst for their creation. The new round scenario development, and thus in its projec- will be centered on four Representative tions of climate change, population is not Concentration Pathways (RCPs) drawn from fully integrated into several key areas of the published literature. The name is meant IPCC work. to emphasize that it is not only the point of stabilization of GHG concentration that mat- While the SRES assumes a future without ters, but also the path a country or the world policies intended to mitigate climate change, takes to get to a stabilization point (O’Neill, such as emissions reductions under the Jiang and Pitcher, 2008). Kyoto Protocol, it does include a review of “non-climate” policies that impact emis- Beginning with a given starting point- of sions, such as those influencing economic radiative forcing, the RCPs will also allow development, technological innovation, integrated assessment modelers to develop energy, agriculture, transportation, and infra- scenarios of future emissions at the same structure. This review includes a brief discus- time climate modelers will use the RCPs to 17 The linkages between sion of population policies. The SRES notes must be addressed. They also argued that population and emissions that studies support the notion that reduced slowed population growth can have a benefi- population growth significantly abates GHG cial impact on emissions in the long run, and are complex but real. emissions, and that therefore, policies influ- make emissions targets easier to reach. They encing fertility, mortality and migration rates counter the coercion argument with the fact could have a significant impact on future that there is existing high unmet need for emissions. At the same time, SRES authors family planning and high rates of unintended note, policies relating to health, education, pregnancy in developed and developing and gender equality can also influence eco- countries alike (Bongaarts et al. 1997). nomic growth, consumption, and per capita Despite these arguments, the 2007 Fourth emissions, with the overall effects likely to Assessment Report also does not include vary from country to country. At the end of population policies in its recommendations this brief section of the report, SRES authors for mitigation (Fisher et al. 2007), just as assert that while policies that reduce fertil- the Kyoto Protocol, adopted in 1997, did not ity may have significant effects on climate include consideration of population issues. change, implementation of such policies was The absence of population in critical climate unrelated to concerns about climate change change dialogues is possibly influenced by at that time (Naki´cenovi´c et al. 2000). continuing controversy over family planning In a 1997 commentary, Bongaarts, O’Neill and reproductive health issues, as the con- and Gaffin note that the Second Assessment servative political environment—particularly Report, published in 1995, did not mention in the U.S.– conflates family planning poli- population in its mitigation strategies, and cies with abortion (de Sherbinin et al. 2007). devoted little attention to the role of demo- Further, population related policies have graphic and population growth on emissions. not been examined as an adaptation strat- The commentary discusses three common egy despite the contribution these policies misconceptions that fuel this resistance to can make to reducing many environmental considering population as a part of climate stresses, such as those on water, land, and change mitigation. The first was the belief forests, in addition to improving health and that “the real problem is consumption, not reducing poverty. population,” emphasizing that the main Assumptions in Population cause of climate change was high levels Projections: Are They of historic emissions from the developed Realistic? countries, and not the result of population growth or over-consumption in the develop- There are many policies that influence GHG ing world. The second was the belief that emissions more directly than those sur- “not much can be done about population,” rounding population. However, given that ignoring the effect of population policies on they are still acknowledged as important, fertility reduction over the past decades. and are cost-effective and beneficial in their The third was that “strengthening popula- own right, it is important to consider popula- tion polices is likely to lead to coercion.” The tion in combination with other GHG mitiga- authors presented a rebuttal, stating that tion interventions. The linkages between emissions from developing countries will population and emissions are complex but surpass those of developed countries in the real. The vast gap in consumption, energy medium term, such that rapid population use, and per capita emissions between the growth as well as over-consumption issues more and less developed countries man-

18 Figure 2: Fertility Rates in Africa: 2004 UN Long-range Projections

8

7

6

5

4 AFRICA

SOUTHERN AFRICA 3 EASTERN AFRICA

MIDDLE AFRICA 2 WESTERN AFRICA

1 NORTHERN AFRICA 1950 2000 2050 2100

Source: United Nations Department of Economic and Social Affairs Population Division. 2007. World Population Prospects: the 2006 Revision. dates commitments on the part of indus- In Uganda, where 41 percent of married It is also useful to revisit trialized nations to reduce their emissions women have an unmet need for family some of the assumptions in order to mitigate global warming, which planning, in which they wish to space or made in population will have a disproportionate impact on the limit their childbearing, but are not using world’s poorest countries, and on disad- contraception (Uganda Bureau of Statistics projections like those vantaged groups within those countries. and Macro International Inc. 2007), the UN used in the SRES. In their However, it is also useful to revisit some of projects a fall in fertility from 6.95 in 2000 to projections of a world with the assumptions made in population projec- 2.78 in 2050—a nearly 60 percent drop–– af- tions like those used in the SRES. In their ter falling only four percent since 1960 (UN falling fertility and slowed projections of a world with falling fertility Population Division 2007). A recent study population growth, the and slowed population growth, the projec- has shown that “in sub-Saharan African projections forecast some tions forecast some dramatic changes that countries, the average pace of decline in dramatic changes that might not be realistic. To focus on the most fertility was lower around 2000 than in the recent UN long-range population projec- mid-1990s and that more than half the coun- might not be realistic. tion, fertility in Africa is projected to fall tries in transition in this region have stalled” 50 percent from 2000 levels by 2050, after (Bongaarts 2008). This is not to say that the falling only 26 percent since 1950 (see dramatic fertility declines assumed in popula- Figure 1) (UN Population Division 2004) tion projections are impossible, but they are

19 Given the GHG emissions unlikely to occur in the absence of sound slower population growth will generally implications of population policies supporting education and equal- lead to lower emissions and allow devel- ity for women, and, importantly, political oping countries to better adapt to climate policies, they warrant and economic support for the reproductive change (O’Neill et al. 2004). Slower popula- further consideration as the health services—including family planning tion growth, they note, will make the other international community supplies and services—necessary for fami- policies less burdensome to implement and lies to have the number of healthy children make emissions reductions easier to attain. strives to develop of a that they desire. Further, policies that influence fertility, such comprehensive set of as women’s education and access to repro- O’Neill, MacKellar, and Lutz’s conclusions re- effective solutions to ductive health and family planning services, garding the benefits of including population- have their own inherent benefits, making climate change challenges. related policies in both mitigating emissions them no-regrets strategies. However, such and facilitating adaptation to likely climate policies are currently underfunded world- change impacts note that there are other wide (O’Neill et al. 2004). more direct measures to address climate change mitigation through reduction in GHG emissions and land use change. However,

Conclusion

Like many factors contributing to climate change, population is one part of a great, complex climate system. This paper has demonstrated that the influences of demographic factors on emissions are significant, and not adequately accounted for in the IPCC’s emissions sce- narios. A deeper and more nuanced understanding of the emissions implications of population size, age structure, household size, and urbanization should be better incorporated into cli- mate change scenarios that provide the basis for policy decision-making and strategy develop- ment for climate change mitigation and adaptation.

Furthermore, the fertility decline assumptions contained in long-range population projections that are incorporated into climate change scenarios may be overly optimistic given recent declines in political and financial support for policies strongly tied to fertility decline, such as education and equality for women and access to reproductive health and family planning services. Given the GHG emissions implications of population policies, they warrant further consideration as the international community strives to develop of a comprehensive set of effective solutions to climate change challenges.

20 endnotes References

1 Radiative forcing is a measure of the influ- Bongaarts, J, B O’Neill and S Gaffin. 1997. ence that a climatic factor has in altering the “Global Warming Policy: Population Left Out in balance of incoming and outgoing energy the Cold.” Environment 39(9):40-41. in the Earth-atmosphere system. The term de Sherbinin, A, DCarr, S Cassels and L Jiang. radiative forcing is also used as an index of 2007. “Population and Environment.” Annual the influence a factor has as a potential cli- Review of Environmental Resources 32:345- mate change mechanism (Nodvin and Vranes 373. 2007). Fisher, B S, N Naki´cenovi´c, K Alfsen, J Corfee 2 GHG and sulfur emissions accounted for in Morlot, F de la Chesnaye, J-Ch Hourcade, K the SRES include CO2, CH4, N2O, HFCs, Jiang, M Kainuma, E La Rovere, A Matysek, A PFCs, SF6, HCFCs, CFCs, and SO2, CO, Rana, K Riahi, R Richels, S Rose, D van Vuuren, NOx and non-methane volatile organic com- R Warren. 2007. “Issues related to mitigation in pounds the long term context.” In B Metz, O R David- 3 GtC stands for gigatons of carbon son, P R Bosch, R Dave and L A Meyer (Eds.). Climate Change 2007: Mitigation. Contribution 4 The numbers in this column represent multi- of Working Group III to the Fourth Assessment model mean SAT warming. Please see Le Report of the Inter-governmental Panel on Treut et al. 2007 for complete temperature Climate Change. Cambridge, UK: Cambridge range information. University Press. 5 The assumptions of this and other population Houghton, J T, L G Meira Fliho, J Bruce, H projections are discussed in detail in the next Lee, B A Callander, E Haites, N Harris, and K section. Maskell. 1994. Climate Change 1994: Radiative 6 The fertility rate at which population growth Forcing of Climate Change and an Evaluation stabilizes is approximately 2.1 children per of the IPCC IS92 Scenarios. Cambridge, UK: woman. Cambridge University Press. 7 It is important to note that the confidence International Institute for Applied Systems Anal- interval is not an assignment of likelihood ysis (IIASA) World Population Program. 2007. for a given population, but rather an expres- “Population Projections for the IPCC Special sion of the range of uncertainty surrounding Report on Emission Scenarios (1996).” http:// future growth. www.iiasa.ac.at/Research/POP/IPCC/index. 8 The IS92 scenarios used the World Bank’s html. Accessed 10 November 2008. 1991 projection (the World Bank had ceased Intergovernmental Panel on Climate Change publication of its population projections by (IPCC). 2004. “Sixteen Years of Scientific As- 1994, the time the SRES scenarios were sessment in Support of the Climate Conven- developed), and the UN 1992 medium high tion.” Geneva: IPCC. and medium low projections. Thus, the range Intergovernmental Panel on Climate Change in the IS92 had both higher estimates at the (IPCC). 2001. Climate Change 2001: Synthesis high and medium end, as well as slightly Report. A Contribution of Working Groups I, II, lower population estimates in the low projec- and III to the Third Assessment Report of the tion. Intergovernmental Panel on Climate Change. Cambridge, UK: Cambridge University Press. Intergovernmental Panel on Climate Change (IPCC). 1995. IPCC Second Assessment: Cli- mate Change 1995. Geneva: IPCC. Jiang, L and K Hardee. 2009. How Do Recent Population Trends Matter to Climate Change? Washington DC: Population Action Interna- tional. Le Treut, H, R Somerville, U Cubasch, Y Ding, C Mauritzen, A Mokssit, T Peterson and M Prather. 2007. “Historical Overview of Climate Change.” In Solomon, S, D Qin, M Manning, Z Chen, M Marquis, K B Averyt, M Tignor and 21 H L Miller (Eds.). Climate Change 2007: The Uganda Bureau of Statistics (UBOS) and Macro Physical Science Basis. Contribution of Work- International Inc. 2007. Uganda Demographic ing Group I to the Fourth Assessment Report and Health Survey 2006. Calverton, Maryland, of the Intergovernmental Panel on Climate USA: UBOS and Macro International Inc. Change. Cambridge, UK: Cambridge University United Nations Population Division. 2007. World Press. Population Prospects: the 2006 Revision. New Lutz, W (Ed.). 1996. The Future Population of York: United Nations. the World: What Can We Assume Today? Lon- Van Vuuren, D and B O’Neill. 2006. “The Con- don: Earthscan Publications Ltd. sistency of IPCC’s SRES Scenarios to Recent Moss, R, M Babiker, S Brinkman, E Calvo, T Literature and Recent Projections.” Climatic Carter, J Edmonds, I Elgizouli, S Emori, L Erda, Change 75:9-46. K Hibbard, R Jones, M Kainuma, J Kelleher, J F Lamarque, M Manning, B Matthews, J Meehl, L Meyer, J Mitchell, N Naki´cenovi´c, B O’Neill, R Pichs, K Riahi, S Rose, P Runci, R Stouffer, D van Vuuren, J Weyant, T Wilbanks, J P van Ypersele and M Zurek. 2008. Towards New Scenarios for Analysis of Emissions, Climate Change, Impacts, and Response Strategies. Geneva: Intergovernmental Panel on Climate Change. Naki´cenovi´c, N, J Alcamo, G Davis, B de Vries, J Fenhann, S Gaffin, K Gregory, A Grubler, T Y Jung, T Kram, E L La Rovere, L Michaelis, S Mori, T Morita, W Pepper, H Pitcher, L Price, K Riahi, A Roehrl, H-H Rogner, A Sankovski, M Schlesinger, P Shukla, S Smith, R Swart, S van Rooijen, N Victor and Z Dadi. 2000. Special Re- port on Emissions Scenarios. A Special Report of Working Group III of the Intergovernmental Panel on Climate Change. Cambridge, UK: Cambridge University Press. Nodvin, S C and K Vranes. 2007. “Radiative forcing.” In C J Cleveland (Ed.). Encyclopedia of Earth. Washington, D.C.: Environmental Infor- mation Coalition, National Council for Science and the Environment. http://www.eoearth.org/ article/Radiative_forcing. Accessed February 3, 2009. O’Neill, B, L Jiang and H Pitcher. Personal com- munication. 28 August 2008. O’Neill, B, F L MacKellar, and W Lutz. 2004. “Population, Greenhouse Gas Emissions, and Climate Change.” In Lutz, W, W C Sanderson and S Scherbov (Eds.). The End of Population Growth in the 21st Century: New Challenges for Human Capital Formation and . London: IIASA and Earthscan, Pp. 283-314.

22 ACKNOWLEDGMENTS This paper greatly benefited from reviews from Dr. John Bongaarts, Population Council, Dr. Geoffrey Dabelko, Woodrow Wilson International Center for Scholars, and Dr. Peter Frumhoff, Union of Concerned Scientists. At PAI, the authors appreciate review from Amy Coen, Leiwen Jiang, Kimberly Rovin, and Elizabeth Leahy Madsen and editorial assistance from Kristine Berzins.

AUTHORS Malea Hoepf Young was a Research Associate at Population Action International through December 2008. Kathleen Mogelgaard is Senior Program Manager of Population and Climate Change at Population Action International. Karen Hardee is Vice President of Research at Population Action International.

© 2009 Population Action International

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