The role of atmospheric CO2 in controlling patterns of sea surface temperature change during the Pliocene

We present the role of CO 2 forcing in controlling patterns of Late Pliocene sea surface temperature (SST) using seven models from Phase 2 of the Pliocene Model Intercomparison Project (PlioMIP2) and palaeoclimate proxy data from the PlioVAR working group. At a global scale, SST change in the Late P...

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Bibliographic Details
Main Authors: Burton, Lauren E., Haywood, Alan M., Tindall, Julia C., Dolan, Aisling M., Hill, Daniel J., McClymont, Erin L., Ho, Sze Ling, Ford, Heather L.
Format: Text
Language:English
Published: 2023
Subjects:
North Atlantic
Online Access:https://doi.org/10.5194/cp-2023-98
https://cp.copernicus.org/preprints/cp-2023-98/
Description
Summary:We present the role of CO 2 forcing in controlling patterns of Late Pliocene sea surface temperature (SST) using seven models from Phase 2 of the Pliocene Model Intercomparison Project (PlioMIP2) and palaeoclimate proxy data from the PlioVAR working group. At a global scale, SST change in the Late Pliocene relative to the pre-industrial is predominantly driven by CO 2 forcing in the low and mid-latitudes and non-CO 2 forcing in the high latitudes. We find that CO 2 is the dominant driver of SST change at the vast majority of proxy data sites assessed (17 out of 19), but the relative dominance of this forcing varies between all proxy sites, with CO 2 forcing accounting for between 27 % and 82 % of the total change seen. The dearth of proxy data sites in the high latitudes means that only two sites assessed here are predominantly forced by non-CO 2 forcing (such as changes to ice sheets and orography), both of which are in the North Atlantic Ocean. We extend the analysis to show the seasonal patterns of SST change and its drivers at a global scale and at a site-specific level for three chosen proxy data sites. We also present a new estimate of Late Pliocene climate sensitivity using site-specific proxy data values. This is the first assessment of site-specific drivers of SST change in the Late Pliocene and highlights the strengths of using palaeoclimate proxy data alongside model outputs to further develop our understanding of the Late Pliocene. We use the best-available proxy and model data, but the sample sizes remain limited and the confidence in our results would be improved with greater data availability.

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