Phasing of millennial-scale climate variability in the Pacific and Atlantic Oceans

Author:

Walczak Maureen H.12ORCID,Mix Alan C.1,Cowan Ellen A.3ORCID,Fallon Stewart2ORCID,Fifield L. Keith2ORCID,Alder Jay R.14ORCID,Du Jianghui15ORCID,Haley Brian1,Hobern Tim2ORCID,Padman June1,Praetorius Summer K.6ORCID,Schmittner Andreas1ORCID,Stoner Joseph S.1,Zellers Sarah D.7ORCID

Affiliation:

1. College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR, USA.

2. Australian National University, Canberra ACT.

3. Department of Geological and Environmental Sciences, Appalachian State University, Boone, NC, USA.

4. United States Geological Survey, Corvallis, OR, USA.

5. Department of Earth Sciences, Institute of Geochemistry and Petrology, ETH Zurich, Zurich, Switzerland.

6. United States Geological Survey, Menlo Park, CA, USA.

7. University of Central Missouri, Warrensburg, MO, USA.

Abstract

Calving cousins Walczak et al. report that increases in Pacific Ocean ventilation and periods of rapid production of icebergs from the Cordilleran Ice Sheet during the last glacial period preceded episodic iceberg discharges into the Atlantic Ocean (see the Perspective by Jaeger and Shevenell). Marine sediments from the Gulf of Alaska show that increases in vertical mixing of the ocean there correspond with intense iceberg calving from the ice sheet that covered much of high-latitude western North America and that these changes occurred before the analogous Heinrich events in the North Atlantic. Thus, these Pacific climate system reorganizations may have been an early part of a cascade of dynamic climate events with global repercussions. Science , this issue p. 716 ; see also p. 662

Funder

American Australian Association

Australian Research Council

National Science Foundation

Australian and New Zealand International Ocean Discovery Program Consortium

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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