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Emissions Scenarios - IPCC

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Emission Scénarios 241<br />

5.1 Introduction<br />

In this chapter emission estimates for radiatively important<br />

gases generated in 40 Special Report on Emission <strong>Scenarios</strong><br />

(SRES) scenarios are present. These gases are carbon dioxide<br />

(COj), methane (CH^), nitrous oxide (N2O), nitrogen oxides<br />

(NOj,), carbon monoxide (CO), non-methane volatile organic<br />

compounds (NMVOCs), sulfur dioxide (SO,), chlorofluorocarbons<br />

(CFCs) and hydrochlorofluorocarbons (HCFCs),^<br />

hydrofluorocarbons (HFCs), perfluorocarbons (PFCs), and<br />

sulfur hexafluoride (SFg) (see Table 5-1). Emission estimates<br />

presented here span the interval from 1990 to 2100 at the<br />

global level and at the level of four SRES macro-regions<br />

(OECD90, REF, ASIA, and ALM; see Appendix IV). In<br />

addition, sulfur emission estimates are presented in the<br />

regional gridded format to assist in quantifying the effects at<br />

the local level. Links between emissions and the underlying<br />

driving forces presented in Chapter 4 are illustrated also.<br />

As a result of differences in modeling and estimation<br />

approaches, base-year (1990) emission values in SRES<br />

scenarios developed using different models show substantial<br />

variation. To facilitate both use of the scenarios and<br />

comparisons across scenarios and families, base-year<br />

emissions in all 40 SRES scenarios were standardized using<br />

one common set of values (see Box 5-1). With a few clearly<br />

indicated exceptions, only standardized emission values are<br />

discussed in this chapter. A complete set of standardized<br />

emissions, along with other quantitative scenario information,<br />

is provided in Appendix VII.<br />

The first section in this chapter presents a "roadmap" that<br />

serves as an orientation to the 40 SRES scenarios. The<br />

roadmap gives a simple taxonomy that compares input<br />

parameters, as represented by the four scenario families, and<br />

emission outputs, as represented by the 1990 to 2100<br />

cumulative CO^ emissions. The subsequent sections discuss in<br />

detail emissions of each gas over the next 100 years to 2100.<br />

5.2. Roadmap to the <strong>Scenarios</strong><br />

A classification scheme is presented here to assist the reader in<br />

understanding the links between driving forces and scenario<br />

outputs. This scheme can also be used to help select<br />

appropriate scenarios for further analysis (see Chapter 6).<br />

The SRES scenarios were developed as quantitative<br />

interpretations of the four alternative storylines that represent<br />

possible futures with different combinations of driving forces.<br />

These broad scenario families are broken down further into<br />

seven scenario groups,- used here to classify the input driving<br />

forces (see also Table 4-20 in Chapter 4).<br />

' Emission trajectories of these ozone-depleting substances (ODSs)<br />

are not developed by the SRES team, but adopted from WMO/UNEP<br />

(1998).<br />

The scenario outputs of most interest are emissions of GHGs,<br />

SOj, and other radiatively important gases. However, the<br />

categorization of scenarios based on emissions of multiple<br />

gases is quite difficult. All gases that contribute to radiative<br />

forcing should be considered, but methods of combining gases<br />

such as the use of global warming potentials (GWP) are<br />

appropriate only for near-term GHG inventories.-' In addition,<br />

emission trajectories may display different dynamics, from<br />

monotonie increases to non-Unear trajectories in which a<br />

subsequent decline from a maximum occurs. This particularly<br />

diminishes the significance of a focus on any given year, such<br />

as 2100. In light of these difficulties, the classification<br />

approach presented here uses cumulative COj emissions<br />

between 1990 and 2100. COj is the dominant GHG and<br />

cumulative CO2 emissions are expected to be roughly<br />

proportional to CO2 radiative forcing over the time scale<br />

considered (Houghton et al. 1996).<br />

Total cumulative COj emissions from the 40 SRES scenarios<br />

fall into the range from 773 to 2538 gigatonnes of carbon (GtC)<br />

with a median of 1509 GtC. To represent this range, the<br />

scenario classification uses four intervals:<br />

• Less than 1100 GtC (low).<br />

• Between 1100 and 1450 GtC (medium-low).<br />

• Between 1450 and 1800 GtC (medium-high).<br />

• Greater than 1800 GtC (high).<br />

Each CO2 interval contains multiple scenarios and scenarios<br />

from more than one family. Each category also includes one of<br />

the four marker scenarios. Figure 5-1 shows how cumulative<br />

CO2 emissions from the 40 SRES scenarios fit within the<br />

selected emission intervals.<br />

Table 5-2 provides an overview of this scenario classification<br />

and links the scenario outcomes with factors that drive them,<br />

organized by family and scenario group (see also Table 4-20).<br />

The rows in Table 5-2 represent the emission categories, while<br />

the columns represent the scenario families. The analysis of<br />

Table 5-2 reveals two key resuhs:<br />

^ During the approval process of the Summary for Policymakers at the<br />

5th Session of Working Group III (WGIII) of the <strong>IPCC</strong> from 8 to 11<br />

March 2000 in Katmandu, Nepal, h was decided to combine the AlC<br />

and AIG groups into one "fossil intensive" group AlFI in contrast to<br />

the non-fossil group AIT, and to select two illustrative scenarios from<br />

these two Al groups to facilitate use by modelers and policy makers.<br />

This leads to six scenario gi-oups that constitute the four scenario<br />

families, three of which are in the Al family. All scenarios are equally<br />

sound.<br />

In particular, the <strong>IPCC</strong> Working Group 1 (WGI) Second Assessment<br />

Report (SAR) GWPs are calculated for constant concentrations. In<br />

long-tei-m scenarios, concentrations may change significantly, as do<br />

GWP values. It is unclear how to apply GWPs to long-tetm scenarios<br />

in a meaningful manner. In addition, the GWP approach is not<br />

applicable to gases such as SO^ and ozone precursors.

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