Interannual atmospheric variability forced by the deep equatorial Atlantic Ocean
Abstract
Climate variability in the tropical Atlantic Ocean is determined by large-scale ocean-atmosphere interactions, which particularly affect deep atmospheric convection over the ocean and surrounding continents. Apart from influences from the Pacific El Niño/Southern Oscillation and the North Atlantic Oscillation, the tropical Atlantic variability is thought to be dominated by two distinct ocean-atmosphere coupled modes of variability that are characterized by meridional and zonal sea-surface-temperature gradients and are mainly active on decadal and interannual timescales, respectively. Here we report evidence that the intrinsic ocean dynamics of the deep equatorial Atlantic can also affect sea surface temperature, wind and rainfall in the tropical Atlantic region and constitutes a 4.5-yr climate cycle. Specifically, vertically alternating deep zonal jets of short vertical wavelength with a period of about 4.5 yr and amplitudes of more than 10 cm s(-1) are observed, in the deep Atlantic, to propagate their energy upwards, towards the surface. They are linked, at the sea surface, to equatorial zonal current anomalies and eastern Atlantic temperature anomalies that have amplitudes of about 6 cm s(-1) and 0.4 °C, respectively, and are associated with distinct wind and rainfall patterns. Although deep jets are also observed in the Pacific and Indian oceans, only the Atlantic deep jets seem to oscillate on interannual timescales. Our knowledge of the persistence and regularity of these jets is limited by the availability of high-quality data. Despite this caveat, the oscillatory behaviour can still be used to improve predictions of sea surface temperature in the tropical Atlantic. Deep-jet generation and upward energy transmission through the Equatorial Undercurrent warrant further theoretical study.
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- Authors
- Brandt, P., Funk, A., Hormann, V., Dengler, M., Greatbatch, R. J., & Toole, J. M.
- Affiliations
- GEOMAR Helmholtz Centre for Ocean Research Kiel (DE)
- National Oceanic and Atmospheric Administration (US)
- Corresponding author
- Brandt, Peter
- Venue
- Nature
- Published
- 2011-05
- Volume
- 473
- Issue
- 7348
- Pages
- 497-500
- ISSN
- 0028-0836 (ISSN-L)
- 1476-4687
- OpenAlex
- W2038103745
- Cited by
- 93
- References
- 27
- Citations by year
- 2026: 3 · 2025: 1 · 2024: 4 · 2023: 6 · 2022: 6 · 2021: 7 · 2020: 17 · 2019: 8 · 2018: 7 · 2017: 9 · 2016: 4 · 2015: 8 · 2014: 3 · 2013: 4 · 2012: 6
- FWCI
- 3.56
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature (publishedVersion)
- PubMed (publishedVersion)
- Helmholtz Centre for Ocean Research Kiel (GEOMAR) (acceptedVersion)
- RePEc: Research Papers in Economics (submittedVersion)
- Funders
- Woods Hole Oceanographic Institution
- Met Office
- Bundesministerium für Bildung und Forschung
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Meteorological Phenomena and Simulations
- Keywords
- interannual variability, ocean-atmosphere interaction, sea surface temperature anomalies, rainfall variability, Equatorial Undercurrent, tropical Atlantic climate, climate prediction
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