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Lunt et al., EGU 2008 Atmospheric CO2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation Experimental Design Results Conclusions Future Work / Implications

Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

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Page 1: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

Atmospheric CO2 decrease led to Greenland glaciation in the Late Pliocene

D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone

Motivation

Experimental Design

Results

Conclusions

Future Work / Implications

Page 2: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

The Causes of Northern Hemisphere Glaciation?

Zachos et al, Nature, 2001

Page 3: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

The Causes of Northern Hemisphere Glaciation?

5 main hypotheses

(1) Closure of Panama Seaway

(2) Tectonic Uplift

(3) Termination of ‘Permanent El Nino’

(4) Decrease in CO2

(5) Oribital variations

Page 4: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

The Causes of Northern Hemisphere Glaciation?

5 main hypotheses

(1) Closure of Panama Seaway

(2) Tectonic Uplift

(3) Termination of ‘Permanent El Nino’

(4) Decrease in CO2

(5) Oribital variations

Ruddiman, p163

Page 5: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

The Causes of Northern Hemisphere Glaciation?

5 main hypotheses

(1) Closure of Panama Seaway

(2) Tectonic Uplift

(3) Termination of ‘Permanent El Nino’

(4) Decrease in CO2

(5) Oribital variations

Bartoli et al, 2005

Page 6: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

The Causes of Northern Hemisphere Glaciation?

5 main hypotheses

(1) Closure of Panama Seaway

(2) Tectonic Uplift

(3) Termination of ‘Permanent El Nino’

(4) Decrease in CO2

(5) Oribital variations

Page 7: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

The Causes of Northern Hemisphere Glaciation?

5 main hypotheses

(1) Closure of Panama Seaway

(2) Tectonic Uplift

(3) Termination of ‘Permanent El Nino’

(4) Decrease in CO2

(5) Oribital variations

Ruddiman and Kutzbach, 1989

Page 8: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

The Causes of Northern Hemisphere Glaciation?

5 main hypotheses

(1) Closure of Panama Seaway

(2) Tectonic Uplift

(3) Termination of ‘Permanent El Nino’

(4) Decrease in CO2

(5) Oribital variations

Japsen and Chalmers, 2000

Parrish et al, 2007

Page 9: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

The Causes of Northern Hemisphere Glaciation?

5 main hypotheses

(1) Closure of Panama Seaway

(2) Tectonic Uplift

(3) Termination of ‘Permanent El Nino’

(4) Decrease in CO2

(5) Oribital variations

Page 10: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

The Causes of Northern Hemisphere Glaciation?

5 main hypotheses

(1) Closure of Panama Seaway

(2) Uplift of Rockies

(3) Termination of ‘Permanent El Nino’

(4) Decrease in CO2

(5) Oribital variations

Molnar and Cane, 2002

Page 11: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

The Causes of Northern Hemisphere Glaciation?

5 main hypotheses

(1) Closure of Panama Seaway

(2) Uplift of Rockies

(3) Termination of ‘Permanent El Nino’

(4) Decrease in CO2

(5) Oribital variations

e.g. Wara et al, 2005

Page 12: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

The Causes of Northern Hemisphere Glaciation?

5 main hypotheses

(1) Closure of Panama Seaway

(2) Uplift of Rockies

(3) Termination of ‘Permanent El Nino’

(4) Decrease in CO2

(5) Oribital variations

Page 13: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

The Causes of Northern Hemisphere Glaciation?

5 main hypotheses

(1) Closure of Panama Seaway

(2) Uplift of Rockies

(3) Termination of ‘Permanent El Nino’

(4) Decrease in CO2

(5) Oribital variations

Page 14: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

The Causes of Northern Hemisphere Glaciation?

5 main hypotheses

(1) Closure of Panama Seaway

(2) Uplift of Rockies

(3) Termination of ‘Permanent El Nino’

(4) Decrease in CO2

(5) Oribital variations

Raymo et al, 1996

380ppmv mean, 425ppmv max

Page 15: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

The Causes of Northern Hemisphere Glaciation?

5 main hypotheses

(1) Closure of Panama Seaway

(2) Uplift of Rockies

(3) Termination of ‘Permanent El Nino’

(4) Decrease in CO2

(5) Oribital variations

400ppmv to 280ppmv

Page 16: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

Spinup of GCM simulations…

Page 17: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

Panama ENSO Rockies CO2

Temp

Precip

GCM results…

Page 18: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

Ice sheet model results…

Page 19: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

Ice sheet model results…

Page 20: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

Ice sheet model results…

Page 21: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

Ice sheet model results…

Page 22: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

Ice sheet model results…

Page 23: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

(1) Closure of Panama Seaway

(2) Uplift of Rockies

(3) Termination of ‘Permanent El Nino’

(4) Decrease in CO2

(5) Oribital variations

From Berger and Loutre, 1991

The Causes of Northern Hemisphere Glaciation?

5 main hypotheses

Page 24: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

(1) Closure of Panama Seaway

(2) Uplift of Rockies

(3) Termination of ‘Permanent El Nino’

(4) Decrease in CO2

(5) Oribital variations

Maslin et al, 1998

The Causes of Northern Hemisphere Glaciation?

5 main hypotheses

Page 25: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

(1) Closure of Panama Seaway

(2) Uplift of Rockies

(3) Termination of ‘Permanent El Nino’

(4) Decrease in CO2

(5) Oribital variations

The Causes of Northern Hemisphere Glaciation?

5 main hypotheses

Page 26: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

Ice sheet model results…(2)

Extent of ‘cold orbit’ ice sheet

Page 27: Lunt et al., EGU 2008 Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene D.J. Lunt, G.L. Foster, A.M. Haywood, E.J. Stone Motivation

Lunt et al., EGU 2008

Conclusions

Future Work / Implications

Enhancement of Greenland glaciation in the late Pliocene driven by decrease in atmospheric CO2

Greenland ice sheet waxed and waned on orbital timescales prior to 3 Ma.

ENSO and tectonic forcing factors, with or without orbital trigger, did not play an important role in Greenland glaciation.

Improvement of CO2 records of the pre-ice core era.

Improvement of IRD records in North Atlantic (including provenance).

Need for transient model simulations (using fully coupled Earth System Models).

Strong dependence on CO2 has obvious implications for future ice sheet stability.