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Title: Proxy‐Model Comparison for the Eocene‐Oligocene Transition in Southern High Latitudes
Abstract

The Eocene‐Oligocene transition (EOT) marks the shift from greenhouse to icehouse conditions at 34 Ma, when a permanent ice sheet developed on Antarctica. Climate modeling studies have recently assessed the drivers of the transition globally. Here we revisit those experiments for a detailed study of the southern high latitudes in comparison to the growing number of mean annual sea surface temperature (SST) and mean air temperature (MAT) proxy reconstructions, allowing us to assess proxy‐model temperature agreement and refine estimates for the magnitude of thepCO2forcing of the EOT. We compile and update published proxy temperature records on and around Antarctica for the late Eocene (38–34 Ma) and early Oligocene (34–30 Ma). Compiled SST proxies cool by up to 3°C and MAT by up to 4°C between the timeslices. Proxy data were compared to previous climate model simulations representing pre‐ and post‐EOT, typically forced with a halving ofpCO2. We scaled the model outputs to identify the magnitude ofpCO2change needed to drive a commensurate change in temperature to best fit the temperature proxies. The multi‐model ensemble needs a 30 or 33% decrease inpCO2, to best fit MAT or SST proxies respectively. These proxy‐model intercomparisons identify decliningpCO2as the primary forcing of EOT cooling, with a magnitude (200 or 243 ppmv) approaching that of thepCO2proxies (150 ppmv). However individual model estimates span a decrease of 66–375 ppmv, thus proxy‐model uncertainties are dominated by model divergence.

 
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Award ID(s):
1908548 1844380
NSF-PAR ID:
10395822
Author(s) / Creator(s):
 ;  ;  ;  
Publisher / Repository:
DOI PREFIX: 10.1029
Date Published:
Journal Name:
Paleoceanography and Paleoclimatology
Volume:
38
Issue:
2
ISSN:
2572-4517
Format(s):
Medium: X
Sponsoring Org:
National Science Foundation
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