Articles | Volume 19, issue 7
https://doi.org/10.5194/cp-19-1359-2023
https://doi.org/10.5194/cp-19-1359-2023
Research article
 | 
13 Jul 2023
Research article |  | 13 Jul 2023

Amplified surface warming in the south-west Pacific during the mid-Pliocene (3.3–3.0 Ma) and future implications

Georgia R. Grant, Jonny H. T. Williams, Sebastian Naeher, Osamu Seki, Erin L. McClymont, Molly O. Patterson, Alan M. Haywood, Erik Behrens, Masanobu Yamamoto, and Katelyn Johnson

Viewed

Total article views: 1,874 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,469 338 67 1,874 44 59
  • HTML: 1,469
  • PDF: 338
  • XML: 67
  • Total: 1,874
  • BibTeX: 44
  • EndNote: 59
Views and downloads (calculated since 13 Feb 2023)
Cumulative views and downloads (calculated since 13 Feb 2023)

Viewed (geographical distribution)

Total article views: 1,874 (including HTML, PDF, and XML) Thereof 1,825 with geography defined and 49 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 02 Nov 2024
Download
Short summary
Regional warming will differ from global warming, and climate models perform poorly in the Southern Ocean. We reconstruct sea surface temperatures in the south-west Pacific during the mid-Pliocene, a time 3 million years ago that represents the long-term outcomes of 3 °C warming, which is expected for the future. Comparing these results to climate model simulations, we show that the south-west Pacific region will warm by 1 °C above the global average if atmospheric CO2 remains above 350 ppm.