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Expert Meeting on the Assessment of Expert Meeting on the Assessment of Contributions to Climate Change Contributions to Climate Change Takanobu KOSUGI, Toshimasa TOMODA, Keigo AKIMOTO Research Institute of Innovative Technology for the Earth (R ITE) Expert Meeting on the Assessment of Expert Meeting on the Assessment of Contributions to Climate Change Contributions to Climate Change UK Met Office, UK September 25 - 27, 2002 DNE21 Results for Phases 1 & 2 DNE21 Results for Phases 1 & 2

Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

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DNE21 Results for Phases 1 & 2. DNE21 Results for Phases 1 & 2. Expert Meeting on the Assessment of Contributions to Climate Change UK Met Office, UK September 25 - 27, 2002. Expert Meeting on the Assessment of Contributions to Climate Change. - PowerPoint PPT Presentation

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Page 1: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Expert Meeting on the Assessment ofExpert Meeting on the Assessment ofContributions to Climate ChangeContributions to Climate Change

Takanobu KOSUGI, Toshimasa TOMODA, Keigo AKIMOTOResearch Institute of Innovative Technology for the Earth (RITE)

Expert Meeting on the Assessment ofExpert Meeting on the Assessment ofContributions to Climate ChangeContributions to Climate Change

UK Met Office, UKSeptember 25 - 27, 2002

DNE21Results for Phases 1 & 2

DNE21Results for Phases 1 & 2

Page 2: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Interrelations in DNE21ModelInterrelations in DNE21Model

E nergy S ystem sM odel

M acro-E cono m icM odel

C lim ate C hangeM odel

C O E m iss ionsS O x E m iss ions

2

F in a l E n e rg yD e m a n d s E nergy S ystem s

C osts

#Population#R ef. G D P#R ef. F inal Energy

e tc .

#Energy R esources#Supply C osts

e tc .

#O ther G H G s Em issionse tc .

Page 3: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Outline of the Climate Change ModelOutline of the Climate Change Model

Simple climate change model was constructed based on MAGICC (Model for the Assessment of Greenhouse gas Induced Climate Change).

Carbon circulation (both oceanic and terrestrial), atmospheric concentrations of other GHGs, their radiative forcings, temperature rises of 4 representative points (north and south hemispheres, ocean and land), sea level changes of north and south hemispheres (energy balance of upwelling stream among one dimensional 40 layers) etc. are calculated.

Cooling effect of SOx aerosol is taken into account.

Page 4: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Calculating Steps in Climate Change ModelCalculating Steps in Climate Change Model

CO Em issio n2

SO x Em ission

M ethaneEm ission

N O Em issio n2

Halocarbo ns(27 types)Em issions

Atm osph eric Co ncentration

CO 2

O c ean s LandSurface

RadiativeFo rcing of CO 2

M e th a n eC o n c e n tra t io n

N OCo ncentration

2

Halocarbo ns (27 types)

Co ncentration

R a d ia tiv e F o rc in go f M e th a n e

RadiativeFo rcing of N O2

Radiative Forcin gof H alocarb ons

(20 types)

RadiativeFo rcing of SO x

RadiativeFo rcing of H O2

RadiativeFo rcing of O zon e

G lob al M eanTem peratu re

Rise

Sea LevelCh an ge

Total R ad ia tiveF orcin g

Page 5: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Phase 1 StudyPhase 1 Study

• Assumptions / Conditions– Historical emissions data: CDIAC database

– Future emissions scenario: A2 of the IPCC SRES

– Timeframe: 1765 to 2100– Model parameters:

Reference case as specified in “TERMS

OF REFERENCE”

Cumulative CO2 emissions

Page 6: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Results for Phase 1Results for Phase 1CO2 concentration CH4 and N2O concentrations

Radiative forcing (relative to 1990) Global-average surface air temperature change

Page 7: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Phase 2 StudyPhase 2 Study

• Assumptions / Conditions:– Historical emissions data: CDIAC database

– Future emissions scenarios: A2, B1 and A1FI, of the IPCC SRES (For CO2 emissions only. Non-CO2 GHGs emissions are assumed to be zero.)

– Emissions start year: 1991

– Emissions end years: 2010, 2050 and 2100

– Countries/regions: OECD90, REF, ASIA and ALM used in the IPCC SRES.

– Model parameters: Reference case only (same as Phase 1)

Page 8: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Methodology of Attribution CalculationMethodology of Attribution Calculation

1. Calculate emission effect V(t) (e.g., temperature change) of year t assuming that all the regions emit anthropogenic CO2 according to Scenarios.

2. Calculate emission effect VR (t) assuming that one of the regions R does not emit anthropogenic CO2 during the period between the emissions start year and an emissions end year.

3. Contribution of the region R’s emissions for the period is the difference: V(t) – VR (t).

Phase 2:

• Minimization of non-linearity error• Avoidance of non-anthropogenic emission effect

NOTE

Page 9: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

COCO22 Emissions Accumulated in Atmosphere Emissions Accumulated in Atmosphere

• A2 ScenarioA2 Scenario

Attribution (%) in 2100OECD90 REF ASIA ALM

Emissions end year

2010 45 14 26 152050 35 11 33 212100 28 10 36 26

Phase 2 results:

0

10

20

30

40

50

60

70

80

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

ribut

ion

of C

O2 e

mis

sion

s

accu

mul

ated

in t

he a

tmos

pher

e (G

tC)

OECD90REFASIAALM

(1) Emissions end year: 2010

0

20

40

60

80

100

120

140

160

180

200

220

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f C

O2 e

mis

sio

ns

acc

um

ula

ted

in t

he

atm

osp

he

re (

GtC

) OECD90REFASIAALM

(2) Emissions end year: 2050

0

100

200

300

400

500

600

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f C

O2 e

mis

sio

ns

acc

um

ula

ted

in t

he

atm

osp

he

re (

GtC

) OECD90REFASIAALM

(3) Emissions end year: 2100

Page 10: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

COCO22 Concentration Concentration

• A2 ScenarioA2 Scenario

Phase 2 results:

Attribution (%) in 2100OECD90 REF ASIA ALM

Emissions end year

2010 45 14 26 152050 35 11 33 212100 28 9 36 27

0

5

10

15

20

25

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f C

O2 c

on

cen

tra

tion

(pp

mv)

OECD90REFASIAALM

0

10

20

30

40

50

60

70

80

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f C

O2

con

cen

tra

tion

(pp

mv)

OECD90REFASIAALM

0

20

40

60

80

100

120

140

160

180

200

220

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f C

O2

con

cen

tra

tion

(pp

mv)

OECD90REFASIAALM

(1) Emissions end year: 2010

(3) Emissions end year: 2100(2) Emissions end year: 2050

Page 11: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Radiative Forcing of CORadiative Forcing of CO22

• A2 ScenarioA2 Scenario

Phase 2 results:

Attribution (%) in 2100OECD90 REF ASIA ALM

Emissions end year

2010 45 14 26 152050 35 11 33 212100 27 9 37 27

0.00

0.05

0.10

0.15

0.20

0.25

0.30

0.35

0.40

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f ra

dia

tive

fo

rcin

g o

f C

O2

(W/m

2)

OECD90REFASIAALM

0.0

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1.0

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f ra

dia

tive

fo

rcin

g o

f C

O2

(W/m

2)

OECD90REFASIAALM

0.0

0.2

0.4

0.6

0.8

1.0

1.2

1.4

1.6

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f ra

dia

tive

fo

rcin

g o

f C

O2

(W/m

2)

OECD90REFASIAALM

(1) Emissions end year: 2010

(3) Emissions end year: 2100(2) Emissions end year: 2050

Page 12: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Global-Average Temperature ChangeGlobal-Average Temperature Change

• A2 ScenarioA2 Scenario

Phase 2 results:

Attribution (%) in 2100OECD90 REF ASIA ALM

Emissions end year

2010 45 14 26 152050 35 11 33 212100 27 9 37 27

0.00

0.02

0.04

0.06

0.08

0.10

0.12

0.14

0.16

0.18

0.20

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e

tem

pe

ratu

re c

ha

ng

e (

o C)

OECD90REFASIAALM

0.0

0.1

0.2

0.3

0.4

0.5

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e

tem

pe

ratu

re c

ha

ng

e (

o C)

OECD90REFASIAALM

0.0

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1.0

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e

tem

pe

ratu

re c

ha

ng

e (

o C)

OECD90REFASIAALM

(1) Emissions end year: 2010

(3) Emissions end year: 2100(2) Emissions end year: 2050

Page 13: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Global-Average Sea Level RiseGlobal-Average Sea Level Rise

• A2 ScenarioA2 Scenario

Phase 2 results:

Attribution (%) in 2100OECD90 REF ASIA ALM

Emissions end year

2010 45 14 26 152050 35 11 33 212100 30 9 36 25

0.0

0.2

0.4

0.6

0.8

1.0

1.2

1.4

1.6

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e s

ea

leve

l ris

e (

cm)

OECD90REFASIAALM

0.0

0.5

1.0

1.5

2.0

2.5

3.0

3.5

4.0

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e s

ea

leve

l ris

e (

cm)

OECD90REFASIAALM

0.0

1.0

2.0

3.0

4.0

5.0

6.0

7.0

8.0

9.0

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e s

ea

leve

l ris

e (

cm)

OECD90REFASIAALM

(1) Emissions end year: 2010

(3) Emissions end year: 2100(2) Emissions end year: 2050

Page 14: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

COCO22 Emissions Accumulated in Atmosphere Emissions Accumulated in Atmosphere

• B1 ScenarioB1 Scenario

Attribution (%) in 2100OECD90 REF ASIA ALM

Emissions end year

2010 44 14 26 162050 30 9 31 302100 24 9 30 37

Phase 2 results:

0.0

10.0

20.0

30.0

40.0

50.0

60.0

70.0

80.0

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

ribut

ion

of C

O2 e

mis

sion

s

accu

mul

ated

in t

he a

tmos

pher

e (G

tC)

OECD90REFASIAALM

0

20

40

60

80

100

120

140

160

180

200

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f C

O2 e

mis

sio

ns

acc

um

ula

ted

in t

he

atm

osp

he

re (

GtC

) OECD90REFASIAALM

0

50

100

150

200

250

300

350

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f C

O2 e

mis

sio

ns

acc

um

ula

ted

in t

he

atm

osp

he

re (

GtC

) OECD90REFASIAALM

(2) Emissions end year: 2050 (3) Emissions end year: 2100

(1) Emissions end year: 2010

Page 15: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

COCO22 Concentration Concentration

• B1 ScenarioB1 Scenario

Phase 2 results:

Attribution (%) in 2100OECD90 REF ASIA ALM

Emissions end year

2010 44 14 26 162050 29 9 31 312100 23 8 30 39

0

5

10

15

20

25

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f C

O2 c

on

cen

tra

tion

(pp

mv)

OECD90REFASIAALM

0

10

20

30

40

50

60

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f C

O2

con

cen

tra

tion

(pp

mv)

OECD90REFASIAALM

0

20

40

60

80

100

120

140

160

180

200

220

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f C

O2

con

cen

tra

tion

(pp

mv)

OECD90REFASIAALM

(1) Emissions end year: 2010

(3) Emissions end year: 2100(2) Emissions end year: 2050

Page 16: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Radiative Forcing of CORadiative Forcing of CO22

• B1 ScenarioB1 Scenario

Phase 2 results:

Attribution (%) in 2100OECD90 REF ASIA ALM

Emissions end year

2010 44 13 26 172050 29 9 31 312100 23 8 29 40

0.00

0.05

0.10

0.15

0.20

0.25

0.30

0.35

0.40

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f ra

dia

tive

fo

rcin

g o

f C

O2

(W/m

2)

OECD90REFASIAALM

0.0

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f ra

dia

tive

fo

rcin

g o

f C

O2

(W/m

2)

OECD90REFASIAALM

0.0

0.2

0.4

0.6

0.8

1.0

1.2

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f ra

dia

tive

fo

rcin

g o

f C

O2

(W/m

2)

OECD90REFASIAALM

(1) Emissions end year: 2010

(3) Emissions end year: 2100(2) Emissions end year: 2050

Page 17: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Global-Average Temperature ChangeGlobal-Average Temperature Change

• B1 ScenarioB1 Scenario

Phase 2 results:

0.00

0.02

0.04

0.06

0.08

0.10

0.12

0.14

0.16

0.18

0.20

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e

tem

pe

ratu

re c

ha

ng

e (

o C)

OECD90REFASIAALM

0.0

0.1

0.2

0.3

0.4

0.5

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e

tem

pe

ratu

re c

ha

ng

e (

o C)

OECD90REFASIAALM

0.0

0.1

0.2

0.3

0.4

0.5

0.6

0.7

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e

tem

pe

ratu

re c

ha

ng

e (

o C)

OECD90REFASIAALM

(1) Emissions end year: 2010

(3) Emissions end year: 2100(2) Emissions end year: 2050

Attribution (%) in 2100OECD90 REF ASIA ALM

Emissions end year

2010 44 14 26 162050 29 9 31 312100 23 8 30 39

Page 18: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Global-Average Sea Level RiseGlobal-Average Sea Level Rise

• B1 ScenarioB1 Scenario

Phase 2 results:

0.0

0.2

0.4

0.6

0.8

1.0

1.2

1.4

1.6

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e s

ea

leve

l ris

e (

cm)

OECD90REFASIAALM

0.0

0.5

1.0

1.5

2.0

2.5

3.0

3.5

4.0

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e s

ea

leve

l ris

e (

cm)

OECD90REFASIAALM

0.0

1.0

2.0

3.0

4.0

5.0

6.0

7.0

8.0

9.0

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e s

ea

leve

l ris

e (

cm)

OECD90REFASIAALM

(1) Emissions end year: 2010

(3) Emissions end year: 2100(2) Emissions end year: 2050

Attribution (%) in 2100OECD90 REF ASIA ALM

Emissions end year

2010 44 14 26 162050 30 9 31 302100 25 9 30 36

Page 19: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

COCO22 Emissions Accumulated in Atmosphere Emissions Accumulated in Atmosphere

• A1FI ScenarioA1FI Scenario

Attribution (%) in 2100OECD90 REF ASIA ALM

Emissions end year

2010 44 14 26 162050 30 9 31 302100 24 9 30 37

Phase 2 results:

0

10

20

30

40

50

60

70

80

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

ribut

ion

of C

O2 e

mis

sion

s

accu

mul

ated

in t

he a

tmos

pher

e (G

tC)

OECD90REFASIAALM

0

50

100

150

200

250

300

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f C

O2 e

mis

sio

ns

acc

um

ula

ted

in t

he

atm

osp

he

re (

GtC

) OECD90REFASIAALM

0

100

200

300

400

500

600

700

800

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f C

O2 e

mis

sio

ns

acc

um

ula

ted

in t

he

atm

osp

he

re (

GtC

) OECD90REFASIAALM

(2) Emissions end year: 2050 (3) Emissions end year: 2100

(1) Emissions end year: 2010

Page 20: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

COCO22 Concentration Concentration

• A1FI ScenarioA1FI Scenario

Phase 2 results:

Attribution (%) in 2100OECD90 REF ASIA ALM

Emissions end year

2010 45 14 27 142050 30 12 39 192100 25 10 38 27

0

5

10

15

20

25

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f C

O2 c

on

cen

tra

tion

(pp

mv)

OECD90REFASIAALM

0

10

20

30

40

50

60

70

80

90

100

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f C

O2

con

cen

tra

tion

(pp

mv)

OECD90REFASIAALM

0

50

100

150

200

250

300

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f C

O2

con

cen

tra

tion

(pp

mv)

OECD90REFASIAALM

(1) Emissions end year: 2010

(3) Emissions end year: 2100(2) Emissions end year: 2050

Page 21: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Radiative Forcing of CORadiative Forcing of CO22

• A1FI ScenarioA1FI Scenario

Phase 2 results:

Attribution (%) in 2100OECD90 REF ASIA ALM

Emissions end year

2010 45 14 27 142050 30 12 39 192100 24 10 39 27

0.00

0.05

0.10

0.15

0.20

0.25

0.30

0.35

0.40

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f ra

dia

tive

fo

rcin

g o

f C

O2

(W/m

2)

OECD90REFASIAALM

0.0

0.2

0.4

0.6

0.8

1.0

1.2

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f ra

dia

tive

fo

rcin

g o

f C

O2

(W/m

2)

OECD90REFASIAALM

0.0

0.2

0.4

0.6

0.8

1.0

1.2

1.4

1.6

1.8

2.0

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f ra

dia

tive

fo

rcin

g o

f C

O2

(W/m

2)

OECD90REFASIAALM

(1) Emissions end year: 2010

(3) Emissions end year: 2100(2) Emissions end year: 2050

Page 22: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Global-Average Temperature ChangeGlobal-Average Temperature Change

• A1FI ScenarioA1FI Scenario

Phase 2 results:

0.00

0.02

0.04

0.06

0.08

0.10

0.12

0.14

0.16

0.18

0.20

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e

tem

pe

ratu

re c

ha

ng

e (

o C)

OECD90REFASIAALM

0.0

0.1

0.2

0.3

0.4

0.5

0.6

0.7

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e

tem

pe

ratu

re c

ha

ng

e (

o C)

OECD90REFASIAALM

0.0

0.2

0.4

0.6

0.8

1.0

1.2

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e

tem

pe

ratu

re c

ha

ng

e (

o C)

OECD90REFASIAALM

(1) Emissions end year: 2010

(3) Emissions end year: 2100(2) Emissions end year: 2050

Attribution (%) in 2100OECD90 REF ASIA ALM

Emissions end year

2010 45 14 27 142050 30 12 39 192100 25 10 38 27

Page 23: Takanobu KOSUGI , Toshimasa TOMODA, Keigo AKIMOTO

Global-Average Sea Level RiseGlobal-Average Sea Level Rise

• A1FI ScenarioA1FI Scenario

0.0

0.2

0.4

0.6

0.8

1.0

1.2

1.4

1.6

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e s

ea

leve

l ris

e (

cm)

OECD90REFASIAALM

0.0

0.5

1.0

1.5

2.0

2.5

3.0

3.5

4.0

4.5

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e s

ea

leve

l ris

e (

cm)

OECD90REFASIAALM

0

2

4

6

8

10

12

1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100Year

Att

rib

utio

n o

f g

lob

al-

ave

rag

e s

ea

leve

l ris

e (

cm)

OECD90REFASIAALM

Phase 2 results:

(1) Emissions end year: 2010

(3) Emissions end year: 2100(2) Emissions end year: 2050

Attribution (%) in 2100OECD90 REF ASIA ALM

Emissions end year

2010 45 14 27 142050 31 12 39 182100 26 10 39 25