Table 4
Population at Risk in 2085 for Coastal Flooding
Population at Risk in the
Additional Population at
Total Population
Absence of Climate Change
Risk Because of Climate Change
at Risk
Units
Millions
Percentage of
Millions
Percentage of
Millions
Percentage of
Global Population
Global Population
Global Population
Baseline 1990
10
0.2
10
0.2
A1FI 2085
1 to 3
0
10 to 42
0.1 to 0.5
11 to 45
0.1 to 0.6
A2 2085
30 to 74
0.2 to 0.5
50 to 277
0.4 to 2.0
80 to 351
0.6 to 2.5
B2 2085
5 to 35
0 to 0.3
27 to 66
0.3 to 0.6
32 to 101
0.3 to 1.0
B1 2085
2 to 5
0 to 0.1
3 to 34
0 to 0.5
5 to 39
0 to 0.5
Source: R. J. Nicholls, "Coastal Flooding and Wetland Loss in the 21st Century: Changes under the SRES Climate and Socio-Economic Scenarios," Global
Environmental Change 14, no. 1 (2004).
by a storm surge in 2085 with and without cli-
warmest (and richest) scenario has the least
mate change, assuming that populations
total water stress.
would be attracted preferentially to the coast
This is all the more striking given that the
and that some adaptations would occur with a
calculations informing Table 3 assume zero
30-year lag time.40 The low and high end of the
adaptation despite the ready availability of
time-tested adaptive responses on both the
ranges for populations at risk for each entry in
supply and demand side (e.g., water storage
Table 4 assume low and high subsidence due
facilities to augment water supplies during
to non-climate-change-related human causes,
drier periods, or water pricing and other con-
respectively.
servation measures).39 Thus it overestimates
The main conclusion one draws from
Table 4 is that the warmest and richest sce-
the populations at risk in all scenarios. These
nario (A1FI) produces only slightly larger
overestimates, however, are greatest for the
coastal flooding damages than the coolest
A1FI (richest) scenario and lowest for the A2
scenario (B1). This conclusion is at least par-
(poorest) scenario. Although the ranking
tially due to the fact that although the calcu-
among the scenarios would not change, the
lations in Table 4 make a creditable effort to
differences in the populations at risk
incorporate improvements in adaptive capac-
between the various scenarios would have
ity due to increasing wealth, some of the
been magnified had adaptation been consid-
underlying assumptions are questionable.
ered.
For instance, the scenarios in Table 4 allow
societies to implement measures to reduce the
Coastal Flooding
risk of coastal flooding in response to 1990
The FTA's estimates of the population at
surge conditions, but ignore such changes due
risk for coastal flooding with and without any
to subsequent sea level rise.41 But one would
climate change between 1990 and 2085 are
shown in Table 4. Note that sea level will rise
expect that whenever any measures are imple-
relative to the land not only because of climate
mented, society would consider the latest
change but also because the land may subside
available data and information on the surge
for a variety of reasons not related to climate
situation at the time the measures are initiat-
change (e.g., extraction of water, gas, or oil
ed. That is, if the measure is initiated in, say,
under the coastline). In this table, population
2050, the measure's design would at least con-
at risk is measured by the average number of
sider sea level and sea level trends as of 2050,
people who would experience coastal flooding
rather than merely the 1990 level.
9