Articles | Volume 20, issue 9
https://doi.org/10.5194/cp-20-1989-2024
https://doi.org/10.5194/cp-20-1989-2024
Research article
 | Highlight paper
 | 
12 Sep 2024
Research article | Highlight paper |  | 12 Sep 2024

Can we reliably reconstruct the mid-Pliocene Warm Period with sparse data and uncertain models?

James D. Annan, Julia C. Hargreaves, Thorsten Mauritsen, Erin McClymont, and Sze Ling Ho

Viewed

Total article views: 1,468 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,154 252 62 1,468 44 47
  • HTML: 1,154
  • PDF: 252
  • XML: 62
  • Total: 1,468
  • BibTeX: 44
  • EndNote: 47
Views and downloads (calculated since 11 Sep 2023)
Cumulative views and downloads (calculated since 11 Sep 2023)

Viewed (geographical distribution)

Total article views: 1,468 (including HTML, PDF, and XML) Thereof 1,404 with geography defined and 64 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Dec 2024
Download
Co-editor-in-chief
This study presents an interesting attempt to reconstruct global surface temperature by combining sparse SST proxy data and PlioMIP2 simulations using a state-of-the-art data assimilation framework. The work highlights the potential of this method for providing key insights into past warming patterns, and will serve as a good starting point for future investigations.
Short summary
We have created a new global surface temperature reconstruction of the climate of the mid-Pliocene Warm Period, representing the period roughly 3.2 million years before the present day. We estimate that the globally averaged mean temperature was around 3.9 °C warmer than it was in pre-industrial times, but there is significant uncertainty in this value.