EGU26-20994, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-20994
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Tuesday, 05 May, 08:30–10:15 (CEST), Display time Tuesday, 05 May, 08:30–12:30
 
Hall X4, X4.21
Tropical Climate Variability and Coral Reefs
Thomas Felis1, Jessica A. Hargreaves1, Miriam Pfeiffer2, and the SPP 2299 Team*
Thomas Felis et al.
  • 1MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
  • 2Institute of Geosciences, Kiel University (CAU), Kiel, Germany
  • *A full list of authors appears at the end of the abstract

Climate change, in particular the rise in tropical sea surface temperature, is the greatest threat to coral reef ecosystems today with associated climatic extremes affecting the livelihood of tropical societies. The interaction between the tropical ocean basins plays a key role in modulating climate variability on interannual to decadal timescales. These timescales are of strong relevance to societies and ecosystems, because they control the time interval for recovery between extreme events. Throughout the tropical oceans, a key archive for reconstructions of temperature and hydrology are massive shallow-water corals. Annually to monthly resolved coral proxy records are critical for our understanding of tropical ocean-atmosphere interactions. The DFG Priority Programme “Tropical Climate Variability and Coral Reefs” (SPP 2299) aims to enhance our understanding of tropical marine climate variability and its impact on coral reef ecosystems in a warming world, by quantifying climatic and environmental changes during both the ongoing warming and past warm periods on timescales relevant for society. Ultra-high resolution (monthly to weekly) geochemistry of the coral skeleton is a valuable tool to understand the temporal response of corals to ongoing climate change. Developing reconstructions of past tropical climate and environmental variability, in conjunction with advanced statistical methods, earth system modelling and observed ecosystem responses allows improved projections of future changes in tropical climate and coral reef ecosystems. We present examples (1) for modes of tropical climate variability affecting coral reef ecosystems, such as interactions of the IOD and ENSO, (2) for thermal stress signatures in coral geochemical and isotopic records, and (3) highlight knowledge gaps and future directions in this emerging field, contributing to a better understanding of the response of coral reef ecosystems and tropical climate variability to ongoing and future climate change.

SPP 2299 Team:

Thomas Felis, Jessica A. Hargreaves, Miriam Pfeiffer, Eleni Anagnostou, Sonia Bejarano, Patrick Boyden, Thomas Brachert, Hana Camelia, Diana Diers, Juan Pablo D'Olivo, Andrew Dolman, Nicolas Duprey, Jan Fietzke, Martin Frank, Norbert Frank, Daniel Frick, Dieter Garbe-Schönberg, Eberhard Gischler, Sahra Greve, Ed Hathorne, Michael Henehan, Saori (Sally) Ito, Oliver Knebel, Martin Kölling, Laura Lehnhoff, Donghao Li, Hannah Manns, Alfredo Martínez-García, Catarina Martins, Luisa Meiritz, Ute Merkel, Regina Mertz, Phyllis Mono, Manfred Mudelsee, Alessio Rovere, Christian R. Voolstra, Marlene Wall, Sophie Warken, Takaaki (Konabe) Watanabe, Merlin Weichler, Christian Wild, Yang Yu, Maren Ziegler

How to cite: Felis, T., Hargreaves, J. A., and Pfeiffer, M. and the SPP 2299 Team: Tropical Climate Variability and Coral Reefs, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-20994, https://doi.org/10.5194/egusphere-egu26-20994, 2026.