Dampened predictable decadal North Atlantic climate fluctuations due to ice melting
The oscillatory behaviour of the climate system on decadal timescales before the instrumental record is hard to quantify. However, knowledge of this variability is important for putting current changes in context and for supporting reliable future predictions. Here we investigate the recurrent compo...
| Main Authors: | , , , , , , , , |
|---|---|
| Other Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
2023
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/10261/349251 https://doi.org/10.1038/s41561-023-01145-y https://doi.org/10.13039/501100000265 https://doi.org/10.13039/501100004837 https://api.elsevier.com/content/abstract/scopus_id/85150656696 |
| Summary: | The oscillatory behaviour of the climate system on decadal timescales before the instrumental record is hard to quantify. However, knowledge of this variability is important for putting current changes in context and for supporting reliable future predictions. Here we investigate the recurrent component of Holocene climate variability in the North Atlantic sector from 10,500 to 2,000 years ago by conducting a frequency analysis of both an annually laminated climate record from a lake in England and outputs from a long transient simulation of the Atlantic meridional overturning circulation. We find consistent decadal variability over the past 6,700 years and before 8,500 years before present, probably reflecting predominance of solar and ocean forcings. Between these dates, climate variability was dampened on decadal timescales. Our results suggest that meltwater discharge into the North Atlantic and the subsequent hydrographic changes, from the opening of the Hudson Bay until the final collapse of the Laurentide Ice Sheet, disrupted the decadal cyclic signals for more than a millennium. Given the current acceleration of the Greenland Ice Sheet melting in response to global warming, this study provides long-term evidence of potential challenges predicting future patterns of the climate system. This study was funded by the Royal Society. C.M.-P. is supported by a Royal Society Dorothy Hodgkin Fellowship (ref: DH150185) and a UKRI Future Leaders Fellowship (MR/W009641/1). A.H. is supported by the Spanish Ministry of Science and Innovation through the Ramón y Cajal Scheme (RYC2020-029253-I). We thank P. Ortega and E. Moreno-Chamarro for valuable discussions. We also thank A. Walsh and G. Biddulph for varve counting in some sections of the record, A. Zhao for plotting complementary climate datasets that helped with the interpretation of the proxy record, A. Brauer and his team for lake coring, and the Diss Council for support during fieldwork. Peer reviewed |
|---|