Journal articles

Some of the collaborations in this study were initiated through the PAGES QUIGS workshop 2020. We acknowledge the World Climate Research Programme, which, through its Working Group on Coupled Modelling, coordinated and promoted CMIP6, as well as the Working Group on Climate Models (WGCM) and Past Global Changes (PAGES) for their support of the Paleoclimate Modelling Intercomparison Project. 

We thank the Past Global Changes (PAGES) programme for their financial and logistical support of the working group on Pliocene Climate Variability over glacial-interglacial timescales (PlioVAR), and we thank all workshop participants and members of the PlioVAR steering committee for their discussions.

This publication is a contribution towards PALSEA (Palaeo-Constraints on Sea-Level Rise), a working group of the International Union for Quaternary Sciences (INQUA) and Past Global Changes (PAGES), HOLSEA (Geographic variability of Holocene sea level) and International Geoscience Program (IGCP) Project 725, “Forecasting Coastal Change”. 

The authors acknowledge PALSEA, a working group of the International Union for Quaternary Sciences (INQUA) and Past Global Changes (PAGES).

The authors acknowledge HOLSEA and PALSEA, working groups of the International Union for Quaternary Sciences (INQUA) and Past Global Changes (PAGES).

This research contributes to the DiverseK (a working group of PAGES) initiative.

CoralHydro2k is a contribution to Phases 3 and 4 of the PAGES 2k network. We would like to thank PAGES IPO for providing logistical, technical, and financial support for community-driven projects such as CoralHydro2k. More specifically, we would like to extend our gratitude to Sarah Eggleston, Belen Martrat, Angela Wade, and the PAGES2k coordinators for helping facilitate various aspects of this project over the last 4 years. Most importantly, we would like to thank the original data generators of each coral-based proxy record for making their data publicly available via the World Data Center PANGAEA, the NOAA NCEI World Data Service for Paleoclimatology, or other means, without whom this effort would not be possible.

We would like to thank all the researchers whose publicly archived data were included in the CoralHydro2k database (Appendix A). We would also like to thank the following researchers who provided data that were not previously archived or that were archived in places other than NOAA or PANGAEA and are now included in CoralHydro2k and NOAA: Tianran Chen, Wenfeng Deng, Juan P. D'Olivo, Heitor Evangelista, Jennifer A. Flannery, Eberhard Gischler, Nathalie F. Goodkin, Y. Kawakubo, K. Halimeda Kilbourne, Braddock K. Linsley, Christopher R. Maupin, Hussein R. Sayani, Sujata A. Murty, David Storz, Takaaki K. Watanabe, Henry C. Wu, Hangfang Xiao.

This paper benefitted from discussion at events of the Past Global Changes (PAGES) working group “Volcanic Impacts on Climate and Society” (VICS). We acknowledge the World Climate Research Programme's Working Group on Coupled Modelling, which is responsible for CMIP, and thank all the climate modelling groups for producing and making available their model output. We acknowledge the Northern Hemisphere Tree-Ring Network Development (N-TREND), Past Global Changes (PAGES) project and the other authors of proxy reconstructions for providing publicly available data. We thank Karsten Haustein for developing and sharing the code for his impulse response model.

(This study) includes data compiled by SISAL, a working group of the Past Global Changes (PAGES) project. 

This work is a contribution to IGCP Project 725 ‘Forecasting Coastal Change’ and to PALSEA, a working group of the International Union for Quaternary Sciences (INQUA) and Past Global Changes (PAGES).