Inferring Advective Timescales and Overturning Pathways of the Deep Western Boundary Current in the North Atlantic Through Labrador Sea Water Advection-Reference-Cited by-同舟云学术

Inferring Advective Timescales and Overturning Pathways of the Deep Western Boundary Current in the North Atlantic Through Labrador Sea Water Advection

Published:2022-11-28 Issue:12 Volume:127 Page:
ISSN:2169-9275
Container-title:Journal of Geophysical Research: Oceans
language:en
Short-container-title:JGR Oceans

Author:

Chomiak Leah N.¹²³^ORCID,Yashayaev Igor⁴,Volkov Denis L.²³^ORCID,Schmid Claudia³^ORCID,Hooper James A.²³^ORCID

Affiliation:

1. Rosenstiel School of Marine, Atmospheric, and Earth Science University of Miami Miami FL USA

2. Cooperative Institute for Marine and Atmospheric Studies University of Miami Miami FL USA

3. Atlantic Oceanographic and Meteorological Laboratory National Oceanic and Atmospheric Administration Miami FL USA

4. Bedford Institute of Oceanography Fisheries and Oceans Canada Dartmouth NS Canada

Funder

Cooperative Institute for Marine and Atmospheric Studies, University of Miami

Global Ocean Monitoring and Observing Program

NOAA's Atlantic Oceanographic and Meteorological Laboratory

Bedford Institute of Oceanography

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/10.1029/2022JC018892

Reference80 articles.

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

2. BATS Methods. (1997).Bermuda Institute of Oceanography. Online Report. Retrieved fromhttp://bats.bios.edu/wp-content/uploads/2017/07/report_methods.pdf

3. Interior Pathways of Labrador Sea Water in the North Atlantic From the Argo Perspective

4. The Deep Western Boundary Current and Adjacent Interior Circulation at 24°–30°N: Mean Structure and Mesoscale Variability

5. Historical analogues of the recent extreme minima observed in the Atlantic meridional overturning circulation at 26°N

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