Articles | Volume 21, issue 1
https://doi.org/10.5194/cp-21-211-2025
https://doi.org/10.5194/cp-21-211-2025
Research article
 | 
28 Jan 2025
Research article |  | 28 Jan 2025

A sub-fossil coral Sr∕Ca record documents northward shifts of the Tropical Convergence Zone in the eastern Indian Ocean

Miriam Pfeiffer, Hideko Takayanagi, Lars Reuning, Takaaki K. Watanabe, Saori Ito, Dieter Garbe-Schönberg, Tsuyoshi Watanabe, Chung-Che Wu, Chuan-Chou Shen, Jens Zinke, Geert-Jan A. Brummer, and Sri Yudawati Cahyarini

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Cited articles

Abram, N. J., Gagan, M. K., McCulloch, M. T., Chappell, J., and Hantoro, W. S.: Coral reef death during the 1997 Indian Ocean Dipole linked to Indonesian wildfires, Science, 301, 952–955, https://doi.org/10.1126/science.1083841, 2003. 
Abram, N. J., Gagan, M. K., Liu, Z., Hantoro, W. S., McCulloch, M. T., and Suwargadi, B. W.: Seasonal characteristics of the Indian Ocean Dipole during the Holocene epoch, Nature, 445, 299–302, https://doi.org/10.1038/nature05477, 2007. 
Abram, N. J., Gagan, M. K., Cole, J. E., Hantoro, W. S., and Mudelsee, M.: Recent intensification of tropical climate variability in the Indian Ocean, Nat. Geosci., 1, 849–853, https://doi.org/10.1038/ngeo357, 2008. 
Abram, N. J., Dixon, B. C., Rosevear, M. G., Plunkett, B., Gagan, M. K., Hantoro, W. S., and Phipps, S. J.: Optimized coral reconstructions of the Indian Ocean Dipole: An assessment of location and length considerations, Paleoceanography, 30, 1391–1405, https://doi.org/10.1002/2015PA002810, 2015. 
Abram, N. J., Wright, N. M., Ellis, B., Dixon, B. C., Wurtzel, J. B., England, M. H., Ummenhofer, C. C., Philibosian, B., Cahyarini, S. Y., Yu, T.-L., Shen, C.-C., Cheng, H., Edwards, R. L., and Heslop, D.: Coupling of Indo-Pacific climate variability over the last millennium, Nature, 579, 385–392, https://doi.org/10.1038/s41586-020-2084-4, 2020. 
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Short summary
A coral reconstruction of past climate shows changes in the seasonal cycle of sea surface temperature in the south-eastern tropical Indian Ocean. An enhanced seasonal cycle suggests that the tropical rainfall belt shifted northwards between 1856–1918. We explain this with greater warming in the north-eastern Indian Ocean relative to the south-east, which strengthens surface winds and coastal upwelling in the eastern Indian Ocean, leading to greater cooling south of the Equator.

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