Overturning circulation, nutrient limitation, and warming in the Glacial North Pacific-Reference-Cited by-同舟云学术

Overturning circulation, nutrient limitation, and warming in the Glacial North Pacific

Published:2020-12-11 Issue:50 Volume:6 Page:
ISSN:2375-2548
Container-title:Science Advances
language:en
Short-container-title:Sci. Adv.

Author:

Rae J. W. B.¹^ORCID,Gray W. R.¹²^ORCID,Wills R. C. J.³^ORCID,Eisenman I.⁴^ORCID,Fitzhugh B.⁵^ORCID,Fotheringham M.¹,Littley E. F. M.¹^ORCID,Rafter P. A.⁶^ORCID,Rees-Owen R.¹,Ridgwell A.⁷^ORCID,Taylor B.¹,Burke A.¹^ORCID

Affiliation:

1. School of Earth and Environmental Sciences, University of St Andrews, St Andrews, UK.

2. Laboratoire des Sciences du Climat et de l’Environnement (LSCE/IPSL), Université Paris-Saclay, Gif-sur-Yvette, France.

3. Department of Atmospheric Sciences, University of Washington, Seattle, WA 98195, USA.

4. Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093, USA.

5. Department of Anthropology, University of Washington, Seattle, WA 98195, USA.

6. Department of Earth System Science, University of California, Irvine, Irvine, CA 92697, USA.

7. Department of Earth Sciences, University of California, Riverside, Riverside, CA 92521, USA.

Abstract

Enhanced overturning circulation in the glacial North Pacific caused warming, nutrient limitation, and lower atmospheric CO 2 .

Funder

Natural Environment Research Council

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference168 articles.

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2. Why is no deep water formed in the North Pacific?

3. Warren revisited: Atmospheric freshwater fluxes and “Why is no deep water formed in the North Pacific”

4. Atlantic-Pacific Asymmetry in Deep Water Formation

5. High-latitude controls of thermocline nutrients and low latitude biological productivity

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