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WHAT WOULD BE THE IMPACTS OF CLIMATE CHANGE ASSUMING NO, OR SOME, OR MUCH EMISSIONS CONTROL AND SEQUESTRATION?
Martin parryCo-Chair, Working Group II,
IPCC
Global mean temperature predictions
Ensembles of four predictions of global mean temperature resulting from ‘business as usual’ changes in greenhouse gases following on from observed changes since 1860 (orange curves). The addition of sulphate aerosol cooling is shown in the red curves.
Tem
pera
ture
(°C
)
Year
13
14
15
16
17
18
1860 1880 1900 1920 1940 1960 1980 2000 2020 2040 2060 2080 2100
Hadley Centre for Climate Prediction and Research
Global mean precipitation predictions
Ensembles of four predictions of precipitation (rainfall and snowfall) resulting from ‘business as usual’ changes in greenhouse gases following on from observed changes since 1860 (blue curves). The addition of sulphate aerosol cooling is shown in the green curves.
Hadley Centre for Climate Prediction and Research
–21860
8
6
4
2
0
1880 1900 1920 1940 1960 1980 2000 2020 2040 2060 2080 2100
Tota
l pre
cipi
tatio
n (%
cha
nge)
Change in annual temperatures for the 2050s
The change in annual temperatures for the 2050s compared with the present day, when the climate model is driven with an increase in greenhouse gas concentrations equivalent to about a 1% increase per year in CO2. The picture shows the average of four model runs with different starting conditions.
Hadley Centre for Climate Prediction and Research
Observed change in annual precipitation for the 2050s
The change in annual precipitation for the 2050s compared with the present day, when the climate model is driven with an increase in greenhouse gas concentrations equivalent to about a 1% increase per year in CO2. The picture shows the average of four model runs with different starting conditions.
Hadley Centre for Climate Prediction and Research
IMPACTS UNDER NO MITIGATION
Annual runoff
Percentage change in 30-year average annual runoff by the 2080s.
University of Southampton
Population under extreme water stress
Change, due to climate change, in the number of people living in countries with extreme water stress.
0
40
80
120
2020s 2050s 2080s
Popu
latio
n (m
illio
ns)
University of Southampton
Crop yield change 2020s, )2050s,2080s
2020s 2050s 2080s
% c
hang
e in
pric
es fr
om 1
990
base
line
10
8
6
4
2
0
–22020s 2080s 2020s 2080s
40004200
38003600340032003000280026002400
2050s 2050s
Cer
eal p
rodu
ctio
n (m
mt)
Referencescenario
Climate changescenario
2020s 2050s 2080sAddi
tiona
l milli
ons
of p
eopl
e at
risk
of h
unge
r
50454035302520151050
Additional people at risk of hunger under the climate change scenario (0 = Projected reference case).
Projected global cereal production for reference case and the climate change scenario.
Percentage change in global cereal prices under the climate change scenario (0 = Projected reference case).
People at risk from sea-level rise
Percentage change in the number of people at risk under the sea-level rise scenario and constant (1990s) protection (left bar) and the sea-level rise scenario and evolving protection (right bar).
2050s2020s 2080s
700
400
500
600
100
300
200
0
% in
crea
se
Middlesex University / Delft Hydraulics
IMPACTS UNDER SOME/MUCH MITIGATION
Emissions and concentrations of CO2 from unmitigated and stabilising emission scenarios
Unmitigated emissions 750 ppm stabilisation 550 ppm stabilisation
10
5
0
15
20
Ant
hrop
ogen
ic C
O2
emis
sion
s (G
tC/y
r)
2000 2050 2100 2150 2200 2250 2300 2350C
O c
once
ntra
tion
(ppm
)2
1000
950
900
850
800
750
700
650
600
550
500
450
400
3502000 2050 2100 2150 2200 2250 2300 2350
Hadley Centre for Climate Prediction and Research
Global average temperature rise from unmitigated and stabilising emission scenarios
1900 2000 2100 2200
0
2
4
Glo
bal t
empe
ratu
re c
hang
e (°
C)
3
1
Unmitigated emissions 750 ppm stabilisation 550 ppm stabilisation
Hadley Centre for Climate Prediction and Research
Temperature riseAnnual average, from the present day to the 2080s
Hadley Centre for Climate Prediction and Research
cUnmitigated Emissions
c
c Stabilisation of CO2 at 550ppm
Stabilisation of CO2 at 750ppm
Change in precipitationAnnual average, from the present day to the 2080s
cUnmitigated Emissions
c
c Stabilisation of CO2 at 550ppm
Stabilisation of CO2 at 750ppm
Hadley Centre for Climate Prediction and Research
Changes in river runoff from the present day to the 2080s
Unmitigated emissions
Stabilisation of CO2 at 750 ppm Stabilisation of CO2 at 550 ppm
–75 –50 –25 –5 to 5 25 50 75Change in annual runoff (%)
University of Southampton
Changes in water stress from the present day to the 2080s
01 12 23 34 4
Billions of people
Increased water stressDecreased water stress
University of Southampton
Unmitigated Emissions 750 ppm Stabilisation 550 ppm Stabilisation
Changes in crop yieldfrom the present day to the 2080s
Unmitigated emissions
Stabilisation of CO2 at 750 ppm Stabilisation of CO2 at 550 ppm
University of East Anglia
Potential change in cereal yields (%)
10 – 5
0 – -2.5
-5 – -10-2.5 – -5
-10 – -20
2.5 – 05 – 2.5
No data
Global number of people floodedunder three emissions scenarios
100
80
60
40
20
0
Peop
le fl
oode
d (m
illio
ns/y
ear)
2020s 2050s 2080s
Unmitigated emissions 750 ppm stabilisation 550 ppm stabilisation
University of Middlesex
No climate change
People flooded by region60
0
10
20
30
40
50
Southern Mediterranean
West Africa East Africa South Asia SE Asia
Peop
le fl
oode
d (m
illio
ns/y
ear)
Unmitigated emissions 750 ppm stabilisation 550 ppm stabilisation No climate change
University of Middlesex
Island people flooded600
500
400
300
200
100
0Caribbean Indian Ocean
small islandsPacific small islands
Peop
le fl
oode
d (th
ousa
nds/
year
)University of Middlesex
Unmitigated emissions 750 ppm stabilisation 550 ppm stabilisation No climate change
Malaria transmission Change in duration of season, 2080s
Unmitigated emissions
Stabilisation at 750 ppm Stabilisation at 550 ppm
2 to 5 months 1 to 2 months –2 to –1 months –5 to –2 months
London School of Hygiene and
Tropical Medicine
Millions at Risk in the 2080s
0
50
100
150
200
250
300
350
0 0.25 0.5 0.75 1 1.25 1.5 1.75 2 2.25 2.5 2.75 3 3.25Temperature Increase
Addi
tiona
l mill
ions
of p
eopl
e at
ris
k of
hun
ger,
mal
aria
an
d co
asta
l flo
odin
g
0
500
1000
1500
2000
2500
3000
3500
Addi
tiona
l mill
ions
of p
eopl
e at
ris
k of
incr
ease
d w
ater
sho
rtage Risk of water shortage
Risk of malaria
Risk of hunger
Risk of coastal flooding
Legend
Stab
. 550
Stab
. 650
Unm
itiga
ted
emis
sion
s - I
S92a
Stab
. 450
Stab
. 750
Stab
. 100
0
The Cost of Stabilising CO2 Concentrations
The effect of different global economic pathways
Regional enterprise: high pop, mod. growth, (A2)
Local stewardship: ‘semi’-sustainable dev, low pop
(B2)
A2 in 2050s B2
• Pop 11.3 billion• GDP 82 tr $• primary energy 970
GJ/yr• carbon 16 GtC/yr
• Pop 9.3 billion• GDP 110 tr $• primary energy 870
GJ/yr• carbon 11 GtC/yr
0
20
40
60
80
100
120
140
160
180
200
2020 2050 2080
Add
ition
al M
illio
ns o
f Peo
ple
A2 - Regional Enterprise B2 - Local Stewardship
Additional People at Risk of Hunger under the SRES A2 and B2 Scenarios
Costs of 550 Stabilisation assuming different development pathways
($trillion)
Global Non-ann 1 Annex 1
A2 3 - 6 2 - 4 1 - 2
B2 2 - 4 2 - 3 c. 1
Conclusions :
• Stabn at 750 does not avoid most effects. • Stabn at 550 does, but at considerable
cost (= c.20 times Kyoto reductions).• Sustainable development (cf SRES B2
pathway) needs also to be part of the ‘solution’
-200
-180
-160
-140
-120
-100
-80
-60
-40
-20
02020 2050 2080
Mill
ion
Met
ric T
onne
s (m
mt)
A2 - Regional Enterprise B2 - Local Stewardship
The Shortfall in Global Cereal Production for Reference Case and the SRES Scenarios
Millions at Risk in the 2050s
0
50
100
150
200
250
300
350
0 0.25 0.5 0.75 1 1.25 1.5 1.75 2 2.25 2.5 2.75 3 3.25Temperature Increase
Addi
tiona
l mill
ions
of p
eopl
e at
risk
of h
unge
r, m
alar
ia
and
coas
tal f
lood
ing
0
500
1000
1500
2000
2500
3000
3500
Addi
tiona
l mill
ions
of p
eopl
e at
risk
of i
ncre
ased
w
ater
sho
rtage
Stab
ilisa
tion
@ 5
50 p
pmv
Stab
ilisa
tion
@ 7
50 p
pmv
Unm
itiga
ted
emis
sion
s - I
S92a
Risk of water shortage
Risk of malaria
Risk of hunger
Risk of coastal flooding
Legend
Conclusions : 2
• Invest in adaptation, to increase resilience to climate change: technology (eg GM), engineering (eg water use efficiency), institutions. These are ‘win-win’ (eg drought-proofing).
• Invest especially in key vulnerable regions and sectors: Africa, Indian subcont., small islands; water, food, coastal settlement.
• Revise the adaptation/mitigation emphasis:
Change in vegetation biomassfrom present day to the 2230s
–8 –5 –3 –1 1 3 5 8kgC/m2
ITE Edinburgh
c Stabilisation of CO2 at 550ppm
Stabilisation of CO2 at 750ppm
c
Vegetation dieback5
1
2
3
4
02000 21002050 2150 2200 2250
Are
a of
veg
etat
ion
dieb
ack
(mill
ion
km2 )
Years
Unmitigated emissions 750 ppm stabilisation 550 ppm stabilisation
ITE Edinburgh
Uptake of carbon by vegetation
Sink
Source
5
4
3
2
1
0
–1
–2
–31950 20502000 2100 2150 2200 2250
Tran
sfer
of c
arbo
n to
veg
etat
ion
(GtC
/yr)
Unmitigated emissions 750 ppm stabilisation 550 ppm stabilisation
ITE Edinburgh
Changes in vegetation biomassbetween the present day and the 2080s
–8 –5 –3 –1 1 3 5 8kgC/m2
–8 –5 –3 –1 1 3 5 8kgC/m2
–8 –5 –3 –1 1 3 5 8kgC/m2
0 0.1 1 3 5 10 15kgC/m2
ITE Edinburgh
Unmitigated EmissionPresent Day
Stabilisation of CO2 at 750 ppm Stabilisation of CO2 at 550 ppm
Changes in river runofffrom the present day to the 2230s
–75 –50 –25 –5 to 5 25 50 75Change in annual runoff (%)
University of Southampton
c Stabilisation of CO2 at 550ppm
Stabilisation of CO2 at 750ppm
c
Changes in water stressfrom the present day to the 2080s
Unmitigated emissions
Stabilisation of CO2 at 750 ppm Stabilisation of CO2 at 550 ppmStressed country with decrease in stress
Country moves to stressed classStressed country with increase in stress
University of Southampton
Conclusions : 3
• Foster adaptation to avoid increased inequality (autonomous adaptn=more unequal effects of climate change).
• Foster increased resilience (especially in the ‘tail’): a) seek the sub-optimal (eg drought resistant/non-max yield crop varieties); b) (many) small vs (few) large actions; c) promote stability (vs growth?).
Rate of sea-level rise
60
40
20
0 1990 2020s 2050s 2080s 2110s 2140s 2170s 2200s 2230s
Rat
e of
sea
-leve
l ris
e (c
m/c
entu
ry)
Unmitigated emissions 750 ppm stabilisation 550 ppm stabilisation
Global wetland losses
20
15
10
5
02020s 2050s 2080s 2110s 2140s 2170s 2200s 2230s
Frac
tion
of w
etla
nd a
rea
lost
(%)
Unmitigated emissions 750 ppm stabilisation 550 ppm stabilisation
University of Middlesex
Coastal floodingChange from the present day to the 2080s
Unmitigated emissions
Stabilisation at 750 ppm Stabilisation at 550 ppm
University ofMiddlesex
Malaria transmission seasonEstimated for the present day (falciparum)
London School of Hygiene and Tropical Medicine
People at risk of malaria additionally from climate change
350
300
250
200
150
100
50
02020s 2050s 2080s
Add
ition
al p
eopl
e at
risk
(mill
ions
)
Unmitigated emissions 750 ppm stabilisation 550 ppm stabilisation
London School of Hygiene and Tropical Medicine