Holocene climate variability of the Norwegian Atlantic Current during high and low solar insolation forcing-Reference-Cited by-同舟云学术

Holocene climate variability of the Norwegian Atlantic Current during high and low solar insolation forcing

Published:2011-06 Issue:2 Volume:26 Page:n/a-n/a
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Berner K. S.¹²,Koç N.¹²,Godtliebsen F.¹³,Divine D.¹³

Affiliation:

1. Norwegian Polar Institute; Tromsø Norway

2. Department of Geology; University of Tromsø; Norway

3. Department of Mathematics and Statistics; University of Tromsø; Norway

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Link

http://www.agu.org/journals/pa/pa1102/2010PA002002/2010PA002002.pdf

Reference77 articles.

1. Andersen , C. 2003 Surface oceanic climate development and heat flux variability in the Nordic Seas and the subpolar North Atlantic during the Holocene Univ. of Bergen Bergen, Norway.

2. Nonuniform response of the major surface currents in the Nordic Seas to insolation forcing: Implications for the Holocene climate variability;Andersen;Paleoceanography,2004

3. Multi-proxy records showing significant Holocene environmental variability: The inner N. Iceland shelf (Húnaflói);Andrews;Quat. Sci. Rev.,2003

4. A decadal-scale Holocene sea surface temperature record from the subpolar North Atlantic constructed using diatoms and statistics and its relation to other climate parameters;Berner;Paleoceanography,2008

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