Articles | Volume 23, issue 17
https://doi.org/10.5194/acp-23-9963-2023
https://doi.org/10.5194/acp-23-9963-2023
Research article
 | 
07 Sep 2023
Research article |  | 07 Sep 2023

Constraints on simulated past Arctic amplification and lapse rate feedback from observations

Olivia Linke, Johannes Quaas, Finja Baumer, Sebastian Becker, Jan Chylik, Sandro Dahlke, André Ehrlich, Dörthe Handorf, Christoph Jacobi, Heike Kalesse-Los, Luca Lelli, Sina Mehrdad, Roel A. J. Neggers, Johannes Riebold, Pablo Saavedra Garfias, Niklas Schnierstein, Matthew D. Shupe, Chris Smith, Gunnar Spreen, Baptiste Verneuil, Kameswara S. Vinjamuri, Marco Vountas, and Manfred Wendisch

Viewed

Total article views: 3,485 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,647 796 42 3,485 57 55
  • HTML: 2,647
  • PDF: 796
  • XML: 42
  • Total: 3,485
  • BibTeX: 57
  • EndNote: 55
Views and downloads (calculated since 09 Jan 2023)
Cumulative views and downloads (calculated since 09 Jan 2023)

Viewed (geographical distribution)

Total article views: 3,485 (including HTML, PDF, and XML) Thereof 3,372 with geography defined and 113 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 18 Jul 2024
Download
Short summary
Lapse rate feedback (LRF) is a major driver of the Arctic amplification (AA) of climate change. It arises because the warming is stronger at the surface than aloft. Several processes can affect the LRF in the Arctic, such as the omnipresent temperature inversion. Here, we compare multimodel climate simulations to Arctic-based observations from a large research consortium to broaden our understanding of these processes, find synergy among them, and constrain the Arctic LRF and AA.
Altmetrics
Final-revised paper
Preprint