Articles | Volume 5, issue 3
https://doi.org/10.5194/wcd-5-985-2024
https://doi.org/10.5194/wcd-5-985-2024
Research article
 | 
31 Jul 2024
Research article |  | 31 Jul 2024

Circulation responses to surface heating and implications for polar amplification

Peter Yu Feng Siew, Camille Li, Stefan Pieter Sobolowski, Etienne Dunn-Sigouin, and Mingfang Ting

Viewed

Total article views: 1,164 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
896 220 48 1,164 62 28 31
  • HTML: 896
  • PDF: 220
  • XML: 48
  • Total: 1,164
  • Supplement: 62
  • BibTeX: 28
  • EndNote: 31
Views and downloads (calculated since 04 Jan 2024)
Cumulative views and downloads (calculated since 04 Jan 2024)

Viewed (geographical distribution)

Total article views: 1,164 (including HTML, PDF, and XML) Thereof 1,178 with geography defined and -14 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 01 Nov 2024
Download
Short summary
The atmospheric circulation response to surface heating at various latitudes was investigated within an idealized framework. We confirm previous results on the importance of temperature advection for balancing heating at lower latitudes. Further poleward, transient eddies become increasingly important, and eventually radiative cooling also contributes. This promotes amplified surface warming for high-latitude heating and has implications for links between sea ice loss and polar amplification.