Climate Change 2001:
Working Group II: Impacts, Adaptation and Vulnerability
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3.8. Scenarios of the 21st Century

This section summarizes recent developments that are likely to affect the construction of scenarios over the coming few years. One of these developments is construction of the new SRES emission scenarios. Some features of these scenarios and their implications for atmospheric composition, global climate, and sea level are described below. In addition, a brief review of possible regional climate changes during the 21st century is presented, followed by discussions of stabilization scenarios and changes in climate variability and extreme events—key issues in constructing scenarios for policy-relevant impact and adaptation assessments.

3.8.1. SRES Storylines and Emissions Scenarios

Development of the SRES scenarios (Nakicenovic et al., 2000) is outlined in Section The 40 scenarios, 35 of which are fully quantified, are based on four different narrative storylines and associated scenario families. Each storyline describes a different world evolving through the 21st century, and each may lead to quite different GHG emissions trajectories. Four of the scenarios are designated as "markers," each characterizing one of four "scenario families"; two additional scenarios illustrate alternative energy developments in one of the families. The storylines and scenario families are as follows:

Measures of global population, economic development (expressed in annual GDP), and equity (per capita income ratio) for 2050 and 2100 that are implied under the SRES scenarios are shown in Table 3-9, alongside the IS92a scenario and estimates for the present day. Attempts are underway to "downscale" aspects of these global scenarios for use in regional impact assessment (e.g., Lorenzoni et al., 2000).

Table 3-10: Examples of impacts resulting from projected changes in extreme climate events.
Projected Changes during the
21 st Century in Extreme Climate
Phenomena and their Likelihooda
Representative Examples of Projected Impactsb
(all high confidence of occurrence in some areasc)
Simple Extremes  
Higher maximum temperatures; more hot
days and heat wavesd over nearly all land
areas (Very Likelya)
  • Increased incidence of death and serious illness in older age groups and urban poor
  • Increased heat stress in livestock and wildlife
  • Shift in tourist destinations
  • Increased risk of damage to a number of crops
  • Increased electric cooling demand and reduced energy supply reliability
Higher (increasing) minimum temperatures;
fewer cold days, frost days, and cold
wavesdover nearly all land areas
(Very Likelya)
  • Decreased cold-related human morbidity and mortality
  • Decreased risk of damage to a number of crops, and increased risk to others
  • Extended range and activity of some pest and disease vectors
  • Reduced heating energy demand
More intense precipitation events
(Very Likelya over many areas)
  • Increased flood, landslide, avalanche, and mudslide damage
  • Increased soil erosion
  • Increased flood runoff could increase recharge of some floodplain aquifers
  • Increased pressure on government and private flood insurance systems and
    disaster relief
Complex Extremes  
Increased summer drying over most
mid-latitude continental interiors and
associated risk of drought (Likelya)
  • Decreased crop yields
  • Increased damage to building foundations caused by ground shrinkage
  • Decreased water resource quantity and quality
  • Increased risk of forest fire
Increase in tropical cyclone peak wind
intensities, mean and peak precipitation
intensities (Likelya over some areas)e
  • Increased risks to human life, risk of infectious disease epidemics, and many
    other risks
  • Increased coastal erosion and damage to coastal buildings and infrastructure
  • Increased damage to coastal ecosystems such as coral reefs and mangroves
Intensified droughts and floods associated
with El Niño events in many different
regions (Likelya)
(see also under droughts and intense
precipitation events)
  • Decreased agricultural and rangeland productivity in drought- and flood-prone
  • Decreased hydro-power potential in drought-prone regions
Increased Asian summer monsoon
precipitation variability (Likelya)
  • Increase in flood and drought magnitude and damages in temperate and
    tropical Asia
Increased intensity of mid-latitude storms
(little agreement between current models)d
  • Increased risks to human life and health
  • Increased property and infrastructure losses
  • Increased damage to coastal ecosystems
a Likelihood refers to judgmental estimates of confidence used by TAR WGI: very likely (90-99% chance); likely (66-90% chance). Unless otherwise stated, information on climate phenomena is taken from the Summary for Policymakers, TAR WGI.
b These impacts can be lessened by appropriate response measures.
c Based on information from chapters in this report; high confidence refers to probabilities between 67 and 95% as described in Footnote 6 of TAR WGII, Summary for Policymakers.
d Information from TAR WGI, Technical Summary, Section F.5.
e Changes in regional distribution of tropical cyclones are possible but have not been established.

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