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Dynamic Ocean-Atmosphere Coupling: A Thermostat for the Tropics
Abstract
The ocean currents connecting the western tropical Pacific Ocean with the eastern tropical Pacific Ocean are driven by surface winds. The surface winds are in turn driven by the sea-surface temperature (SST) differences between these two regions. This dynamic coupling between the atmosphere and ocean may limit the SST in the tropical Pacific Ocean to below 305 kelvin even in the absence of cloud feedbacks.
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Citations
Cited by
The Double-ITCZ Problem in IPCC AR4 Coupled GCMs: Ocean–Atmosphere Feedback Analysis
Lin, J.-L. (2007) · Journal of Climate · doi:10.1175/jcli4272.1 · Cited by 594
Suppression of El Niño during the Mid‐Holocene by changes in the Earth's orbit
Clement, A. C., Seager, R., & Cane, M. A. (2000) · Paleoceanography · doi:10.1029/1999pa000466 · Cited by 405
Metadata
- Authors
- Sun, D.-Z., & Liu, Z.
- Venue
- Science
- Published
- 1996-05-24
- Volume
- 272
- Issue
- 5265
- Pages
- 1148-1150
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2078030647
- Cited by
- 195
- References
- 0
- FWCI
- 21.57
- Type
- journal article
- Language
- en
- Open access
- closed
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- CoChat. (2026). Citation check: Dynamic Ocean-Atmosphere Coupling: A Thermostat for the Tropics. https://app.cochat.ai/papers/10.1126/science.272.5265.1148
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- Sun, D.-Z., & Liu, Z. (1996). Dynamic Ocean-Atmosphere Coupling: A Thermostat for the Tropics. Science. https://doi.org/10.1126/science.272.5265.1148
Data sources
Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.