5.1 Introduction
In this chapter emission estimates for radiatively important gases generated
in 40 Special Report on Emission Scenarios (SRES) scenarios are present. These
gases are carbon dioxide (CO2), methane (CH4 ), nitrous oxide (N2O), nitrogen
oxides (NOx), carbon monoxide (CO), non-methane volatile organic compounds
(NMVOCs), sulfur dioxide (SO2 ), chlorofluoro-carbons (CFCs) and hydrochlorofluorocarbons
(HCFCs)1,
hydrofluorocarbons (HFCs), perfluorocarbons (PFCs), and sulfur hexafluoride
(SF6 ) (see Table 5-1). Emission estimates presented here span the interval
from 1990 to 2100 at the global level and at the level of four SRES macro-regions
(OECD90, REF, ASIA, and ALM; see Appendix IV). In
addition, sulfur emission estimates are presented in the regional gridded format
to assist in quantifying the effects at the local level. Links between emissions
and the underlying driving forces presented in Chapter 4
are illustrated also.
Table 5- 1: Overview of greenhouse
gases (GHGs), ozone precursors, and sulfur emissions for the SRES scenario
groups. Numbers are for the four markers and (in brackets) for the range
across all scenarios from the same scenario group (standardized emissions,
see also footnote
2). |
|
|
CO2
(GtC)
|
CH4
(MtCH4 )
|
N2O
( MtN)
|
HFC, PFC, SF6
(MtC equiv.)
|
CO
(Mt CO)
|
NMVOCs
(Mt)
|
NOx
(MtN)
|
SOx
(MtS)
|
|
A1B |
13.5 (13.5- 17.9)
|
289 (289- 640)
|
7.0 (5.8- 17.2)
|
824 combined
|
1663 (1080- 2532)
|
193 (133- 552)
|
40.2 (40.2- 77.0)
|
27.6 (27.6- 71.2)
|
A1C |
(25.9- 36.7)
|
(392- 693)
|
(6.1- 16.2)
|
same as in A1
|
(2298- 3766)
|
(167- 373)
|
(63.3 -151.4)
|
(26.9- 83.3)
|
A1G |
(28.2- 30.8)
|
(289- 735)
|
(5.9- 16.6)
|
same as in A1
|
(3260- 3666)
|
(192- 484)
|
(39.9 -132.7)
|
(27.4- 40.5)
|
A1T |
(4.3- 9.1)
|
(274- 291)
|
(4.8- 5.4)
|
same as in A1
|
(1520- 2077)
|
(114 -128)
|
(28.1- 39.9)
|
(20.2- 27.4)
|
A2 |
29.1 (19.6- 34.5)
|
889 (549- 1069)
|
16.5 (8.1- 19.3)
|
1096 combined
|
2325 (776- 2646)
|
342 (169- 342)
|
109.2 (70.9- 110.0)
|
60.3 (60.3- 92.9)
|
B1 |
4.2 (2.7- 10.4)
|
236 (236- 579)
|
5.7 (5.3- 20.2)
|
386 combined
|
363 (363- 1871)
|
87 (58- 349)
|
18.7 (16.0- 35.0)
|
24.9 (11.4- 24.9)
|
B2 |
13.3 (10.8- 21.8)
|
597 (465- 613)
|
6.9 (6.9- 18.1)
|
839 combined
|
2002 (661- 2002)
|
170 (130- 304)
|
61.2 (34.5- 76.5)
|
ß47.9 (33.3- 47.9)
|
|
As a result of differences in modeling and estimation approaches, base-year
(1990) emission values in SRES scenarios developed using different models show
substantial variation. To facilitate both use of the scenarios and comparisons
across scenarios and families, base-year emissions in all 40 SRES scenarios
were standardized using one common set of values (see Box 5-1). With a few clearly
indicated exceptions, only standardized emission values are discussed in this
chapter. A complete set of standardized emissions, along with other quantitative
scenario information, is provided in Appendix VII.
Box 5-1: Scenario Standardization
One of the primary reasons for developing emissions scenarios is to enable
coordinated studies of climate change, climate impacts, and mitigation
options and strategies. With the multi-model approach used in the SRES
process, 1990 and 2000 emissions do not agree in scenarios developed using
different models. In addition, even with agreed reference values, it is
time consuming and often impractical to fine-tune most integrated assessment
models to reproduce a particular desired result.
Nevertheless, differences in the base year and 2000 emissions may lead
to confusion among the scenario users. Therefore, the 1990 and 2000 emission
estimates were standardized in all the SRES scenarios, with emissions
diverging after the year 2000. The procedure for selecting 1990 and 2000
emission values and the subsequent adjustments to scenario emissions are
described in this box.
The standardized scenarios share the same values for emissions in both
1990 and 2000. Emissions for the year 2000 are, of course, not yet known
and 1990 emissions are also uncertain. The 1990 and 2000 emission estimates
for all gases, except SO2 , were set to be equal to the averages of initial
values in the unadjusted four marker scenarios. This was carried out at
the four-region level, and summed to obtain the standardized global totals.
The resultant estimates are within relevant uncertainty ranges for each
substance, but should not be interpreted as "endorsed" by the Intergovernmental
Panel on Climate Change (IPCC) to represent values for either global or
regional emissions. Rather, they are the standardized base-year estimates
used for the emissions scenarios.
From 2000 to 2100, emissions in all the scenarios (except CO2 emissions
from land-use and SO2 emissions) were adjusted by applying a constant
offset equal to the difference between the standardized 2000 value and
the scenario-specific 2000 value. The purpose was to smooth scenario trajectories
between 2000 and 2010.
This procedure results in small distortions for those emissions that
rise with time, or at least that do not ultimately decrease by a large
amount as compared to the base year. However, for emissions that fall
significantly over time, such as those from deforestation or of SO2 ,
this procedure can cause more significant distortions and can even change
the sign of the emission estimates at later times (i.e., change positive
emission estimates into negative ones and vice versa). To avoid these
distortions, for the aforementioned emissions, the year 2000 offset was
reduced by 10% per decade, cumulatively, to make the offset zero by the
year 2100. This allows preservation of the shape of emission trajectories
and still ensures the 2000 standardization.
The non-standardized scenario values are available from the modeling
teams upon request, although the standardized values should be used for
most purposes.
|
The first section in this chapter presents a "roadmap" that serves as an orientation
to the 40 SRES scenarios. The roadmap gives a simple taxonomy that compares
input parameters, as represented by the four scenario families, and emission
outputs, as represented by the 1990 to 2100 cumulative CO2 emissions. The subsequent
sections discuss in detail emissions of each gas over the next 100 years to
2100.
5.2. Roadmap to the Scenarios
A classification scheme is presented here to assist the reader in understanding
the links between driving forces and scenario outputs. This scheme can also
be used to help select appropriate scenarios for further analysis (see Chapter
6).
The SRES scenarios were developed as quantitative interpretations of the four
alternative storylines that represent possible futures with different combinations
of driving forces. These broad scenario families are broken down further into
seven scenario groups2,
used here to classify the input driving forces (see also Table
4-20 in Chapter 4).
The scenario outputs of most interest are emissions of GHGs, SO2 , and other
radiatively important gases. However, the categorization of scenarios based
on emissions of multiple gases is quite difficult. All gases that contribute
to radiative forcing should be considered, but methods of combining gases such
as the use of global warming potentials (GWP) are appropriate only for near-term
GHG inventories3.
In addition, emission trajectories may display different dynamics, from monotonic
increases to non-linear trajectories in which a subsequent decline from a maximum
occurs. This particularly diminishes the significance of a focus on any given
year, such as 2100. In light of these difficulties, the classification approach
presented here uses cumulative CO2 emissions between 1990 and 2100. CO2 is the
dominant GHG and cumulative CO2 emissions are expected to be roughly proportional
to CO2 radiative forcing over the time scale considered (Houghton et al. 1996).
Total cumulative CO2 emissions from the 40 SRES scenarios fall into the range
from 773 to 2538 gigatonnes of carbon (GtC) with a median of 1509 GtC. To represent
this range, the scenario classification uses four intervals:
-
Figure 5-1: Global cumulative CO2 emissions
in the 40 SRES scenarios, classified into four scenario families (each
denoted by a different color code: A1, red; A2, brown; B1, green; B2,
blue). Marker scenarios are shown with thick lines without ticks, globally
harmonized scenarios with thin lines, and non-harmonized scenarios with
thin, dotted lines. Black lines show percentiles, means, and medians for
the 40 SRES scenarios. For numbers on the two additional illustrative
scenarios A1FI and A1T see Appendix VII.
|
Less than 1100 GtC (low).
- Between 1100 and 1450 GtC (medium-low).
- Between 1450 and 1800 GtC (medium-high).
- Greater than 1800 GtC (high).
Each CO2 interval contains multiple scenarios and scenarios from more than
one family. Each category also includes one of the four marker scenarios. Figure
5-1 shows how cumulative CO2 emissions from the 40 SRES scenarios fit within
the selected emission intervals.
Table 5-2 provides an overview of this scenario classification and links the
scenario outcomes with factors that drive them, organized by family and scenario
group (see also Table 4-20). The rows in Table
5-2 represent the emission categories, while the columns represent the scenario
families. The analysis of Table 5-2 reveals two key results:
- Similar future cumulative CO2 emissions may emerge from different sets of
driving forces;
- Conversely, similar future states of the world with respect to socio-economic
development may yield different outcomes in terms of cumulative CO2 emissions.
Similar cumulative CO2 emissions can be attained in very different social,
economic, and technological circumstances. High emission levels of the A2 marker
scenario (A2-ASF) are also attained in all the A1 family scenarios with high
fossil-fuel use (A1C and A1G groups), for example in A1G-MiniCAM. Medium-high
emissions are attained in most of the A1 group scenarios (including the A1B
marker, A1B-AIM), but also in scenarios from the B2 scenario family with high
fossil-fuel use (e.g., B2-ASF). Medium-low emissions, which are characteristic
of the B2 family, including the B2 marker (B2- MESSAGE), are also attained in
the A2-A1-MiniCAM scenario, which illustrates the transition between the A2
and A1 families. Finally, low emission levels result from almost all the B1
family scenarios (including the B1 marker, B1-IMAGE) as well as from scenarios
that belong to the A1T high-technology scenario group (e.g., A1T-MARIA). In
Table 5-2, italics are used for examples of scenarios
within each emission category that illustrate alternative ways to achieve cumulative
CO2 emissions similar to those of the marker scenarios.
Table 5-2: Scenario classification according to scenario
family and cumulative total carbon dioxide emissions (fossil, industrial,
and net deforestation) from 1990 to 2100. Markers are in bold print, the
two additional illustrative scenarios of the A1 scenario group (see footnote
2 of text) in italics; all harmonized scenarios have shaded background;
and examples of scenarios with similar CO emissions (see text) are underlined. |
Cumulative Carbon Emission 1990-2100
|
|
Family |
A1
|
|
|
A2
|
B1
|
B2
|
|
Scenario Group |
A1C |
A1G |
A1B |
A1T |
A2 |
B1 |
B2 |
|
High
>1800GtC |
A1C- AIM
A1C- MESSAGE
A1C- MiniCAM |
A1G- AIM
A1G- MESSAGE
A1G- MiniCAM |
A1B- ASF
|
|
A2- ASF
A2- AIM |
|
|
|
Medium- High
450- 1800GtC |
|
|
A1B- AIM
A1B- IMAGE
A1B- MESSAGE
A1B- MiniCAM
A1v1- MiniCAM
A1v2- MiniCAM |
|
A2- MESSAGE
A2G- IMAGE
A2- MiniCAM |
|
B2C- MARIA
B2- ASF
B2High- MiniCAM |
|
Medium- Low
1100- 1450 GtC |
|
|
A1B- MARIA
|
A1T- AIM
|
A2- A1- MiniCAM |
B1- ASF
B1High- MiniCAM
|
B2- MESSAGE
B2- AIM
B2- MARIA
B2- IMAGE
B2- MiniCAM |
|
Low
<1100 GtC |
|
|
|
A1T- MESSAGE
A1T -MARIA |
|
B1- IMAGE
B1- AIM
B1- MESSAGE
B1- MiniCAM
B1High- MESSAGE
B1T- MESSAGE
B 1- MARIA |
|
|
Marker scenario |
|
|
1499 |
|
1862 |
983 |
1164 |
Illustr. scenario |
2189 |
|
|
1068 |
|
|
|
Harmonized scenarios |
2127-2538 |
2178-2345 |
1301-2073 |
1068-1114 |
1732 |
773-1390 |
1359-1573 |
Other scenarios |
2148 |
2189 |
1519-1731 |
1049 |
1352-1938 |
947-1201 |
1186-1686 |
|
|