Oceanic link between abrupt changes in the North Atlantic ocean and the African monsoon.
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Coupled model simulations indicate a general warming in the tropical Atlantic, with reduced seasonal cycle and interannual variability, in response to an AMOC weakening.
“Coupled model simulations indicate a general warming in the tropical Atlantic, with reduced seasonal cycle and interannual variability, in response to an AMOC weakening (Chang et al., 2008).”
From The tropical atlantic observing system (2019) · cites this paper as Chang et al., 2008
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Self-citation
- Authors
- Chang, P., Zhang, R., Hazeleger, W., Wen, C., Wan, X., Ji, L., Haarsma, R. J., Breugem, W.-P., & Seidel, H.
- Affiliations
- Texas A&M University (US)
- NOAA Geophysical Fluid Dynamics Laboratory (US)
- Royal Netherlands Meteorological Institute (NL)
- Delft University of Technology (NL)
- Corresponding author
- Chang, Ping
- Venue
- Nature Geoscience
- Published
- 2008-05-30
- Volume
- 1
- Issue
- 7
- Pages
- 444-448
- ISSN
- 1752-0894 (ISSN-L)
- 1752-0908
- OpenAlex
- W2104133937
- Cited by
- 162
- References
- 27
- Citations by year
- 2026: 1 · 2025: 3 · 2024: 14 · 2023: 11 · 2022: 8 · 2021: 7 · 2020: 7 · 2019: 8 · 2018: 10 · 2017: 7 · 2016: 3 · 2015: 9 · 2014: 9 · 2013: 11 · 2012: 11
- FWCI
- 9.08
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature Geoscience (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Keywords
- African monsoon, abrupt climate change, North Atlantic thermohaline circulation, North Brazil Current, ocean-atmosphere interaction, ocean stratification, sea surface temperature, monsoon rainfall, Younger Dryas, Late Pleistocene, Early Holocene
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