A Persistent Norwegian Atlantic Current Through the Pleistocene Glacials-Reference-Cited by-同舟云学术

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A Persistent Norwegian Atlantic Current Through the Pleistocene Glacials

Published:2018-06-05 Issue:11 Volume:45 Page:5599-5608
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Newton A. M. W.¹²³^ORCID,Huuse M.¹²^ORCID,Brocklehurst S. H.¹²^ORCID

Affiliation:

1. School of Earth and Environmental Sciences, Williamson BuildingUniversity of Manchester Manchester UK

2. Cryosphere Research at Manchester (CRAM) Manchester UK

3. School of Natural and Built Environment, Elmwood BuildingQueen's University Belfast Belfast UK

Funder

Natural Environment Research Council

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL077819

Reference50 articles.

1. An alternative suggestion for the Pliocene onset of major northern hemisphere glaciation based on the geochemical provenance of North Atlantic Ocean ice-rafted debris

2. Quaternary evolution of the northern North Sea margin through glacigenic debris-flow and contourite deposition

3. Variations in Surface Water Mass Conditions in the Norwegian-Greenland Sea: Evidence from Pliocene/Pleistocene Calcareous Plankton Records (Sites 644, 907, 909)

4. Variability in temperature and geometry of the Norwegian Current over the past 600 yr; stable isotope and grain size evidence from the Norwegian margin

5. Sensitivity of the North Atlantic circulation to break-up of the marine sectors of the NW European ice sheets during the last Glacial: A synthesis of modelling and palaeoceanography

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