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Filtering by: Creator Sinclair, Gaylen Creator Sinclair, Gaylen Rights Statement Copyright Not Evaluated

CarlsonAndersCEOASEarliestHoloceneSouth.pdf

Creator:

Carlson, Anders E., Winsor, Kelsey, Ullman, David J., Brook, Edward J., Sinclair, Gaylen, and et al.

Abstract:

Early Holocene summer warmth drove dramatic Greenland ice sheet (GIS) retreat. Subsequent insolation-driven cooling caused GIS margin readvance to late Holocene maxima, from which ice margins are now retreating. We use ¹⁰Be surface exposure ages from four locations between 69.4°N and 61.2°N to date when in the early Holocene south...

Full Text:

. N. LeGrande, F. S. Anslow, and G. Sinclair (2014), Earliest Holocene south Greenland ice sheet
CarlsonAndersCEOASEarliestHoloceneSouth_AuxiliaryMaterial.zip

Creator:

Carlson, Anders E., Winsor, Kelsey, Ullman, David J., Brook, Edward J., Sinclair, Gaylen, and et al.

Abstract:

Early Holocene summer warmth drove dramatic Greenland ice sheet (GIS) retreat. Subsequent insolation-driven cooling caused GIS margin readvance to late Holocene maxima, from which ice margins are now retreating. We use ¹⁰Be surface exposure ages from four locations between 69.4°N and 61.2°N to date when in the early Holocene south...
Earliest Holocene south Greenland ice sheet retreat within its late Holocene extent

Creator:

Carlson, Anders E., Winsor, Kelsey, Ullman, David J., Brook, Edward J., Hood, Dylan H., Axford, Yarrow, LeGrande, Allegra N., Anslow, Faron S., and Sinclair, Gaylen

Abstract:

Early Holocene summer warmth drove dramatic Greenland ice sheet (GIS) retreat. Subsequent insolation-driven cooling caused GIS margin readvance to late Holocene maxima, from which ice margins are now retreating. We use ¹⁰Be surface exposure ages from four locations between 69.4°N and 61.2°N to date when in the early Holocene south...

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Article

ScholarsArchive@OSU

CarlsonAndersCEOASEarliestHoloceneSouth.pdf

CarlsonAndersCEOASEarliestHoloceneSouth_AuxiliaryMaterial.zip

Earliest Holocene south Greenland ice sheet retreat within its late Holocene extent

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