Seasonal Eddy Variability in the Northwestern Tropical Atlantic Ocean

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Author(s)Huang, Minghai
Author(s)Yang, Yang
Author(s)Liang, Xinfeng
Date Accessioned2023-05-16T14:25:56Z
Date Available2023-05-16T14:25:56Z
Publication Date2023-04-01
DescriptionThis article was originally published in Journal of Physical Oceanography. The version of record is available at: https://doi.org/10.1175/JPO-D-22-0200.1. This article will be embargoed until 10/01/2023. © Copyright 2023 American Meteorological Society (AMS). For permission to reuse any portion of this Work, please contact permissions@ametsoc.org. Any use of material in this Work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act (17 U.S. Code § 107) or that satisfies the conditions specified in Section 108 of the U.S. Copyright Act (17 USC § 108) does not require the AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, requires written permission or a license from the AMS. All AMS journals and monograph publications are registered with the Copyright Clearance Center (https://www.copyright.com). Additional details are provided in the AMS Copyright Policy statement, available on the AMS website (https://www.ametsoc.org/PUBSCopyrightPolicy).
AbstractEddies in the northwestern tropical Atlantic Ocean play a crucial role in transporting the South Atlantic Upper Ocean Water to the North Atlantic and connect the Atlantic and the Caribbean Sea. Although surface characteristics of those eddies have been well studied, their vertical structures and governing mechanisms are much less known. Here, using a time-dependent energetics framework based on the multiscale window transform, we examine the seasonal variability of the eddy kinetic energy (EKE) in the northwestern tropical Atlantic. Both altimeter-based data and ocean reanalyses show a substantial EKE seasonal cycle in the North Brazil Current Retroflection (NBCR) region that is mostly trapped in the upper 200 m. In the most energetic NBCR region, the EKE reaches its minimum in April–June and maximum in July–September. By analyzing six ocean reanalysis products, we find that barotropic instability is the controlling mechanism for the seasonal eddy variability in the NBCR region. Nonlocal processes, including advection and pressure work, play opposite roles in the EKE seasonal cycle. In the eastern part of the NBCR region, the EKE seasonal evolution is similar to the NBCR region. However, it is the nonlocal processes that control the EKE seasonality. In the western part of the NBCR region, the EKE magnitude is one order of magnitude smaller than in the NBCR region and shows a different seasonal cycle, which peaks in March and reaches its minimum in October–November. Our results highlight the complex mechanisms governing eddy variability in the northwestern tropical Atlantic and provide insights into their potential changes with changing background conditions.
SponsorWe thank two anonymous reviewers who provided constructive comments and suggestions and helped us greatly improve this paper. The work was supported in part by National Science Foundation through Grant OCE-2122507.
CitationHuang, Minghai, Yang Yang, and Xinfeng Liang. "Seasonal Eddy Variability in the Northwestern Tropical Atlantic Ocean", Journal of Physical Oceanography 53, 4 (2023): 1069-1085, doi: https://doi.org/10.1175/JPO-D-22-0200.1
ISSN1520-0485
URLhttps://udspace.udel.edu/handle/19716/32748
Languageen_US
PublisherJournal of Physical Oceanography
Keywordseddies
Keywordsinstability
Keywordsmesoscale processes
TitleSeasonal Eddy Variability in the Northwestern Tropical Atlantic Ocean
TypeArticle
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