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The impact of cold North Atlantic sea surface temperatures on climate: implications for the Younger Dryas cooling (11?10 k)

Rind, D, Peteet, D, Broecker, W, McIntyre, A, Ruddiman, W·1986·Climate Dynamics
DOI 10.1007/bf01277044
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  • The sharp decline of spruce 10,000 yr BP and replacement by early successional trees capable of growing on dry, nitrogen-poor soils fit with an interpretation of continuation and intensification of dry, continental conditions with high summer insolation in the late-glacial.

    “The sharp decline of spruce 1 0 000 yr BP and the replacement of spruce woodland by early successional trees capable of growing on dry, nitrogen-poor soils, such as aspen, paper birch, fir, and larch, fit with an interpretation of a continuation and even intensification of dry, continental conditions with high summer insolation common in the late-glacial (Rind et al. 1986).”

    From Late Quaternary History of Low‐ and Mid‐Elevation Vegetation in the White Mountains of New Hampshire (1994) · cites this paper as Rind et al. 1986

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Metadata

Authors
Rind, D., Peteet, D., Broecker, W., McIntyre, A., & Ruddiman, W.
Venue
Climate Dynamics
Publisher
Springer Science and Business Media LLC
Published
1986-09
Volume
1
Issue
1
Pages
3-33
ISSN
  • 0930-7575
  • 1432-0894
DOI
10.1007/bf01277044
Cited by
241
References
1
Language
en
Licence
www.springer.com/tdm (tdm)

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