Planetary equatorial trapped waves in the Atlantic Ocean from TOPEX/Poseidon altimetry.
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The mean phase speed calculated for the westward propagation at 10°, 5°, and 2.5°S is −0.5 m s−1, and for the equatorial eastward propagation it is around 3 m s−1, corresponding approximately to the first baroclinic mode.
“The mean phase speed calculated for the westward propagation at 10°, 5°, and 2.5°S is Ϫ0.5 m s Ϫ1 , and for the equatorial eastward propagation it is around 3 m s Ϫ1 , corresponding approximately to the first baroclinic mode (Philander 1990;França et al. 2003).”
From Tropical Atlantic variability modes (1979-2002). Part I: Time-evolving SST modes related to West African rainfall (2008) · cites this paper as França et al. 2003
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References 50 · Cited by 8
- Authors
- França, C., Wainer, I., de Mesquita, A. R., & Goni, G.
- Affiliations
- Universidade de São Paulo (BR)
- National Oceanic and Atmospheric Administration (US)
- Corresponding author
- França, Carlos
- Venue
- Elsevier Oceanography Series
- Publisher
- Elsevier
- Published
- 2003
- Pages
- 213-232
- ISSN
- 0422-9894 (ISSN-L)
- OpenAlex
- W163516584
- Cited by
- 8
- References
- 50
- Citations by year
- 2023: 1 · 2012: 1
- FWCI
- 0.92
- Type
- book chapter
- Language
- en
- Open access
- closed
- Locations
- Elsevier oceanography series (publishedVersion)
- Funders
- Fundação de Amparo à Pesquisa do Estado de São Paulo
- Centre National d’Etudes Spatiales
- 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 Kelvin waves, equatorial Rossby waves, tropical Atlantic, TOPEX/Poseidon altimetry
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