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Recent Southern Hemisphere (SH) atmospheric circulation, predominantly driven by stratospheric ozone depletion over Antarctica, has caused changes in climate across the extratropics. We present evidence that the Brazilian coast may have been impacted from both wind and sea surface temperature changes derived from this process. Skeleton analysis of massive coral species living in shallow waters off Brazil are very sensitive to air–sea interactions and seem to record this process.
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Articles | Volume 13, issue 8
Biogeosciences, 13, 2379–2386, 2016
https://doi.org/10.5194/bg-13-2379-2016
Biogeosciences, 13, 2379–2386, 2016
https://doi.org/10.5194/bg-13-2379-2016

Ideas and perspectives 25 Apr 2016

Ideas and perspectives | 25 Apr 2016

Ideas and perspectives: Southwestern tropical Atlantic coral growth response to atmospheric circulation changes induced by ozone depletion in Antarctica

Heitor Evangelista et al.

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Agosta, E. A and Compagnucci, R. H.: The 1976/77 Austral summer climate transition effects on the atmospheric circulation and climate in southern South America, J. Climate, 21, 4365–4383, 2008.
Albritton, D. and Kuijpers, L.: Synthesis of the Reports of the Scientific, Environmental Effects, and Technology and Economic Assessment Panels of the Montreal Protocol: a Decade of Assessments For Decision Makers Regarding the Protection of the Ozone Layer: 1988–1999, UNEP/Earthprint, Nairobi, Kenya, 1999.
Arblaster, J. and Meehl, G.: Contributions of external forcings to southern annular mode trends, J. Climate, 19, 2896–2905, 2006.
Baldwin, M., and Dameris, M.: Climate-ozone connections, Chapter 5, Scientific Assessment of Ozone Depletion: 2006, World Meteorological Organization Global Ozone Research and Monitoring Project, Report No. 50, Geneva, WHO, 5.1–5.49, 2007.
Belkin, I. M.: Rapid warming of large marine ecosystems, Prog. Oceanogr., 81, 207–213, 2009.
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Short summary
Recent Southern Hemisphere (SH) atmospheric circulation, predominantly driven by stratospheric ozone depletion over Antarctica, has caused changes in climate across the extratropics. We present evidence that the Brazilian coast may have been impacted from both wind and sea surface temperature changes derived from this process. Skeleton analysis of massive coral species living in shallow waters off Brazil are very sensitive to air–sea interactions and seem to record this process.
Citation
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Final-revised paper
Preprint