The Relationship Between U.S. East Coast Sea Level and the Atlantic Meridional Overturning Circulation: A Review-Reference-Cited by-同舟云学术

The Relationship Between U.S. East Coast Sea Level and the Atlantic Meridional Overturning Circulation: A Review

Published:2019-09 Issue:9 Volume:124 Page:6435-6458
ISSN:2169-9275
Container-title:Journal of Geophysical Research: Oceans
language:en
Short-container-title:J. Geophys. Res. Oceans

Author:

Little Christopher M.¹^ORCID,Hu Aixue²^ORCID,Hughes Chris W.³⁴^ORCID,McCarthy Gerard D.⁵^ORCID,Piecuch Christopher G.⁶^ORCID,Ponte Rui M.¹^ORCID,Thomas Matthew D.⁷^ORCID

Affiliation:

1. Atmospheric and Environmental Research, Inc. Lexington MA USA

2. Climate and Global Dynamics Laboratory National Center for Atmospheric Research Boulder CO USA

3. Department of Earth, Ocean and Ecological Sciences University of Liverpool Liverpool UK

4. National Oceanography Centre Liverpool UK

5. ICARUS, Department of Geography Maynooth University Maynooth Ireland

6. Woods Hole Oceanographic Institution Woods Hole MA USA

7. Department of Geology and Geophysics Yale University New Haven CT USA

Funder

Biological and Environmental Research

National Aeronautics and Space Administration

National Center for Atmospheric Research

National Science Foundation

Natural Environment Research Council

U.S. Department of Energy

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019JC015152

Reference186 articles.

1. Interannual sea level variability in the western North Atlantic: Regional forcing and remote response

2. Continuous Flow of Upper Labrador Sea Water around Cape Hatteras

3. Fate of the Atlantic Meridional Overturning Circulation: Strong decline under continued warming and Greenland melting

4. Evaluation of Subtropical North Atlantic Ocean Circulation in CMIP5 Models against the Observational Array at 26.5°N and Its Changes under Continued Warming

5. Eddy formation on a continental slope

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