atmospheric co 2 decrease led to greenland glaciation in the late pliocene
DESCRIPTION
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 Experimental Design Results Conclusions Future Work / Implications. The Causes of Northern Hemisphere Glaciation?. Zachos et al, Nature, 2001. - PowerPoint PPT PresentationTRANSCRIPT
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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
![Page 2: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/2.jpg)
Lunt et al., EGU 2008
The Causes of Northern Hemisphere Glaciation?
Zachos et al, Nature, 2001
![Page 3: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/3.jpg)
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: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/4.jpg)
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
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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: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/6.jpg)
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: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/7.jpg)
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: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/8.jpg)
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: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/9.jpg)
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: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/10.jpg)
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: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/11.jpg)
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: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/12.jpg)
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: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/13.jpg)
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: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/14.jpg)
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
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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
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Lunt et al., EGU 2008
Spinup of GCM simulations…
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Lunt et al., EGU 2008
Panama ENSO Rockies CO2
Temp
Precip
GCM results…
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Lunt et al., EGU 2008
Ice sheet model results…
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Lunt et al., EGU 2008
Ice sheet model results…
![Page 20: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/20.jpg)
Lunt et al., EGU 2008
Ice sheet model results…
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Lunt et al., EGU 2008
Ice sheet model results…
![Page 22: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/22.jpg)
Lunt et al., EGU 2008
Ice sheet model results…
![Page 23: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/23.jpg)
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: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/24.jpg)
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: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/25.jpg)
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: Atmospheric CO 2 decrease led to Greenland glaciation in the Late Pliocene](https://reader036.vdocuments.net/reader036/viewer/2022062410/56815a22550346895dc76605/html5/thumbnails/26.jpg)
Lunt et al., EGU 2008
Ice sheet model results…(2)
Extent of ‘cold orbit’ ice sheet
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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.