Cited by 72Oceanographic and Atmospheric ProcessesClimate variability and modelsOcean Waves and Remote Sensing

A description of the seasonal cycle of the equatorial Atlantic from altimeter data

Schouten, Mathijs W., Matano, Ricardo P., Strub, Ted P.·2005·Deep Sea Research Part I: Oceanographic Research Papers

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Crossref · 10.1016/j.dsr.2004.10.007

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  • Sea surface height propagates eastward at the equator and westward off the equator.

    “One is that sea surface height propagates eastward at the equator and westward off the equator, as shown by Schouten et al. [2005].”

    From Seasonal cycle in the upper equatorial Atlantic Ocean (2009) · cites this paper as Schouten et al., 2005

  • At eastern and western boundaries, Kelvin and Rossby wave contributions are in phase with each other, indicating the importance of boundary reflections.

    “At eastern and western boundaries, Kelvin and Rossby wave contributions are in phase with each other, indicating the importance of boundary reflections [Schouten et al., 2005].”

    From Seasonal cycle in the upper equatorial Atlantic Ocean (2009) · cites this paper as Schouten et al., 2005

  • The seasonal cycle contributes to over a half of the total variability in sea surface height.

    “The seasonal cycle contributes to over a half of the total variability in SSH [Schouten et al., 2005].”

    From Seasonal cycle in the upper equatorial Atlantic Ocean (2009) · cites this paper as Schouten et al., 2005

  • Schouten et al. (2005) found that sea level variations have the same westward phase speed as the first meridional mode Rossby of the second baroclinic mode at 4°N and 4°S.

    “Schouten et al. [2005] found that sea level variations have the same westward phase speed as the first meridional mode Rossby of the second baroclinic mode at 4°N and 4°S.”

    From Seasonal cycle in the upper equatorial Atlantic Ocean (2009) · cites this paper as Schouten et al., 2005

  • They are reflected as a Kelvin wave on the western boundary and propagate eastward through the whole basin in September and October at the equator.

    “They are reflected as a Kelvin wave on the western boundary and propagate eastward through the whole basin in September and October at the equator.”

    From Seasonal cycle in the upper equatorial Atlantic Ocean (2009) · cites this paper as Schouten et al., 2005

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Authors
Schouten, M. W., Matano, R. P., & Strub, T. P.
Affiliations
Oregon State University (US)
Corresponding author
Schouten, Mathijs W.
Venue
Deep Sea Research Part I: Oceanographic Research Papers
Publisher
Elsevier BV
Published
2005-03
Volume
52
Issue
3
Pages
477-493
ISSN
0967-0637 (ISSN-L)
OpenAlex
W2093425524
Cited by
72
References
0
Citations by year
2026: 3 · 2025: 1 · 2024: 1 · 2023: 3 · 2021: 1 · 2020: 1 · 2019: 5 · 2018: 5 · 2017: 2 · 2016: 2 · 2015: 5 · 2014: 3 · 2013: 6 · 2012: 8
FWCI
4.27
Type
journal article
Language
en
Open access
closed
Locations
Deep Sea Research Part I Oceanographic Research Papers (publishedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
  • Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Ocean Waves and Remote Sensing
Keywords
equatorial Atlantic, seasonal cycle, sea surface height, Kelvin waves, Rossby waves, wind stress forcing, North Brazil Current, ENSO, interannual variability, sea surface topography

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