the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Atlantic Multidecadal Variability since 1850 is largely externally forced
Abstract. Whether observed Atlantic Multidecadal variability (AMV) is truly an intrinsic internal mode of climate variability or an externally forced response remains contentious, with conflicting literature that North Atlantic SST variability arises from internal dynamics or external forcing. The availability of several single model initial-condition large ensembles (SMILEs) and new insights into potential biases in sea surface temperature (SST) variations offer a fresh opportunity to reassess this question. We show that SMILE ensembles provide strong evidence that AMV-like variability is largely externally forced. New insights into potential SST biases also raise questions about apparent early 20th Century oscillatory behaviour. SMILE models with stronger multidecadal variability show weaker agreement with observed AMV phasing, even in the best performing individual ensemble members, suggesting that large internal model variability may obscure the forced signal. We conclude that future variations in North Atlantic SST will very likely be driven primarily by future anthropogenic activities.
- Preprint
(2042 KB) - Metadata XML
-
Supplement
(1701 KB) - BibTeX
- EndNote
Status: open (until 23 Apr 2026)
- RC1: 'Comment on egusphere-2026-699', Anonymous Referee #1, 27 Mar 2026 reply
Viewed
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 171 | 121 | 14 | 306 | 37 | 15 | 23 |
- HTML: 171
- PDF: 121
- XML: 14
- Total: 306
- Supplement: 37
- BibTeX: 15
- EndNote: 23
Viewed (geographical distribution)
| Country | # | Views | % |
|---|
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
This manuscript addresses a highly relevant and still unresolved question: whether the observed Atlantic Multidecadal Variability (AMV) since 1850 is primarily an internally generated mode of variability or largely an externally forced response. The paper argues that AMV-like variability is largely externally forced and that future North Atlantic SST evolution will therefore be driven mainly by anthropogenic forcing. A major strength of the paper is the use of several SMILEs together with a large CMIP6 ensemble, as well as the inclusion of observational uncertainty through different SST datasets. However, I find that the main conclusion is currently stronger than the supporting analysis. Overall, I think the manuscript has clear potential, but substantial revisions are needed. I therefore recommend major revisions. Specific comments are provided below:
Specific comments:
Â
Bellomo, K., Murphy, L. N., Cane, M. A., Clement, A. C., & Polvani, L. M. (2018). Historical forcings as main drivers of the Atlantic multidecadal variability in the CESM large ensemble. Climate Dynamics, 50(9–10). https://doi.org/10.1007/s00382-017-3834-3
Bretherton, C. S., Widmann, M., Dymnikov, V. P., Wallace, J. M., & Bladé, I. (1999). The effective number of spatial degrees of freedom of a time-varying field. Journal of Climate, 12(7). https://doi.org/10.1175/1520-0442(1999)012<1990:TENOSD>2.0.CO;2
Deser, C., Alexander, M. A., Xie, S.-P., & Phillips, A. S. (2010). Sea Surface Temperature Variability: Patterns and Mechanisms. Annual Review of Marine Science. https://doi.org/10.1146/annurev-marine-120408-151453
Otterå, O. H., Bentsen, M., Drange, H., & Suo, L. (2010). External forcing as a metronome for Atlantic multidecadal variability. Nature Geoscience, 3(10). https://doi.org/10.1038/ngeo955
Ruprich-Robert, Y., Msadek, R., Castruccio, F., Yeager, S., Delworth, T., & Danabasoglu, G. (2017). Assessing the climate impacts of the observed atlantic multidecadal variability using the GFDL CM2.1 and NCAR CESM1 global coupled models. Journal of Climate, 30(8). https://doi.org/10.1175/JCLI-D-16-0127.1