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Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University [email protected]

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Page 1: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Limits to AdaptationOcean acidification

Congressional Briefing9 November 2009

Ken Caldeira Carnegie Institution & Stanford University [email protected]

Page 2: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Rain, galoshes, and limits to adaptation

To avoid getting wet, you want to bring an umbrella

To avoid climate risk, you want to reduce carbon dioxide emissions

Kasmira,2009

But to keep your feet dry, you might still need galoshes

To diminish damage from the climate change you can’t avoid, you want to improve adaptive resilience

Just wearing galoshes is not enough

emissions reduction

adaptation

Page 3: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Ischia, Italy

Map created by Norman Einstein

Page 4: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

CO2 dissolving shells and skeletonsHall-Spencer / BBC

High CO2 = Invasive grasses

Low CO2

= Native shellfish

Thanks, Jason Hall-Spencer

Page 5: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Chemistry ofocean acidification

Page 6: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Formation of calcium carbonate shells and

skeletons

CO32-

CO O

OCa Ca2+ (dissolved)

H HO

H2O HC

O O

OHCO3

-C

O O

OCO3

2-

Page 7: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Formation of calcium carbonate shells and

skeletons

CO32-

CO O

O

Ca Ca2+ (dissolved)

H HO

H2O HC

O O

OHCO3

-C

O O

OCO3

2-

Page 8: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Formation of calcium carbonate shells and

skeletons

CO32-

CO O

O

Ca Ca2+ (dissolved)

H HO

H2O HC

O O

OHCO3

-C

O O

OCO3

2-

Page 9: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Formation of calcium carbonate shells and

skeletons

CO O

OCa CaCO3 (solid)

H HO

H2O HC

O O

OHCO3

-C

O O

OCO3

2-

Page 10: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Water, dissolved carbon, and shells and skeletons

CaCO3 (solid)C

O O

OCa

H HO

H2O HC

O O

OHCO3

-C

O O

OCO3

2-

Page 11: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Addition of CO2

CaCO3 (solid)C

O O

OCa

H HO

H2O HC

O O

OHCO3

-C

O O

OCO3

2-

CO O CO2

Page 12: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Formation of carbonic acid

CO O

OCa

HC

O O

OHCO3

-C

O O

OCO3

2-HH

CO O

OH2CO3

CaCO3 (solid)

Page 13: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Increasing ocean acidity

CO O

OCa

HC

O O

OHCO3

-C

O O

OCO3

2-H

CO O

OHCO3

-

H H+

CaCO3 (solid)

Page 14: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Increasing ocean acidity

CO O

OCa

HC

O O

OHCO3

-C

O O

OCO3

2-H

CO O

OHCO3

-

H H+

CaCO3 (solid)

Page 15: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Increasing ocean acidity

CO O

OCa

HC

O O

OHCO3

-C

O O

OCO3

2-H

CO O

OHCO3

-

H H+

CaCO3 (solid)

Page 16: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Increasing ocean acidity

CaCO3 (solid)C

O O

OCa

HC

O O

OHCO3

-C

O O

OCO3

2-H

CO O

OHCO3

-

H H+

Page 17: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Attacking a building block for shells and skeletons

CO O

OCa

HC

O O

OHCO3

-C

O O

OCO3

2-H

CO O

OHCO3

-

H H+

CaCO3 (solid)

Page 18: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

H

Attacking a building block for shells and skeletons

CO O

OCa

HC

O O

OHCO3

-C

O O

OHCO3

-H

CO O

OHCO3

-

CaCO3 (solid)

Page 19: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

H

Dissolving shells and skeletons

CO32-

CO O

O

HC

O O

OHCO3

-C

O O

OHCO3

-H

CO O

OHCO3

-

Ca Ca2+ (dissolved)

Page 20: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

H

Dissolving shells and skeletons

CO32-

CO O

O

HC

O O

OHCO3

-C

O O

OHCO3

-H

CO O

OHCO3

-

Ca Ca2+ (dissolved)

Page 21: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

H

Dissolving shells and skeletons

CO32-

CO O

O

HC

O O

OHCO3

-C

O O

OHCO3

-H

CO O

OHCO3

-

Ca Ca2+ (dissolved)

Page 22: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu
Page 23: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Lizard Island

ExpeditionSeptember

2008

Page 24: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

We measured of coral skeletal growth rates 40% lower than in the late 1970’s

Page 25: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Distribution of corals andocean acidification

Page 26: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

0 1 2 3 4 5

Corrosive OptimalΩAragonite

Carbon dioxide level,

Coral reef distribution

,

and chemical

conditions helping

drive reef formation

Cao and Caldeira, 2008

Page 27: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

0 1 2 3 4 5

Corrosive OptimalΩAragoniteCao and Caldeira, 2008

Carbon dioxide level,

Coral reef distribution

,

and chemical

conditions helping

drive reef formation

Page 28: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

0 1 2 3 4 5

Corrosive OptimalΩAragoniteCao and Caldeira, 2008

Carbon dioxide level,

Coral reef distribution

,

and chemical

conditions helping

drive reef formation

Page 29: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

0 1 2 3 4 5

Corrosive OptimalΩAragoniteCao and Caldeira, 2008

Carbon dioxide level,

Coral reef distribution

,

and chemical

conditions helping

drive reef formation

Page 30: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

0 1 2 3 4 5

Corrosive OptimalΩAragoniteCao and Caldeira, 2008

Carbon dioxide level,

Coral reef distribution

,

and chemical

conditions helping

drive reef formation

Page 31: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

0 1 2 3 4 5

Corrosive OptimalΩAragoniteCao and Caldeira, 2008

Carbon dioxide level,

Coral reef distribution

,

and chemical

conditions helping

drive reef formation

Page 32: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu
Page 33: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Rain, galoshes, and limits to adaptation

Kasmira,2009

emissions reduction

adaptation

Adaptation is important, but it is not a substitute for emissions reduction

We need an umbrellaand galoshes

Page 34: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu

Main points

• Few and limited options for adaptation to acidification– Adaptive capacity of ecosystems can be increased by

reducing other stresses on our ocean environment (overfishing, land-based pollution, habitat loss, etc)

– Management and engineering solutions appear to be feasible only in a few isolated cases

To protect our coastal and ocean environments,

we need to greatly reduce our CO2 emissions soon

Page 35: Limits to Adaptation Ocean acidification Congressional Briefing 9 November 2009 Ken Caldeira Carnegie Institution & Stanford University kcaldeira@carnegie.stanford.edu