Articles | Volume 26, issue 3
https://doi.org/10.5194/acp-26-2209-2026
https://doi.org/10.5194/acp-26-2209-2026
Research article
 | 
12 Feb 2026
Research article |  | 12 Feb 2026

Response of marine post-frontal clouds to Gulf Stream variability

Jingyi Chen, Hailong Wang, Bo Zhang, Hongyu Liu, David Painemal, Armin Sorooshian, Sheng-Lun Tai, and Christiane Voigt

Viewed

Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.

Total article views: 2,299 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,163 109 27 2,299 33 30
  • HTML: 2,163
  • PDF: 109
  • XML: 27
  • Total: 2,299
  • BibTeX: 33
  • EndNote: 30
Views and downloads (calculated since 05 Sep 2025)
Cumulative views and downloads (calculated since 05 Sep 2025)

Viewed (geographical distribution)

Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.

Total article views: 2,299 (including HTML, PDF, and XML) Thereof 2,298 with geography defined and 1 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 24 Mar 2026
Download
Short summary
NASA-validated modeling shows +4K SST (sea surface temperature) & +25 % gradients distinctly alter boundary layer dynamics, cloud physics in cold-air outbreaks. Warmer SST reduces cloud cover; increases size, elongation; hydrometeors shift to ice. Sharper Gradients boost liquid water (cold upwind); reduces ice; disrupts organization. Also, SST changes alter cloud-top properties via entrained airmass origin. Resolving ocean-atmosphere coupling in global models is essential for accurate cloud feedback projections.
Share
Altmetrics
Final-revised paper
Preprint