Articles | Volume 20, issue 18
https://doi.org/10.5194/acp-20-10911-2020
https://doi.org/10.5194/acp-20-10911-2020
Research article
 | 
22 Sep 2020
Research article |  | 22 Sep 2020

Examining the atmospheric radiative and snow-darkening effects of black carbon and dust across the Rocky Mountains of the United States using WRF-Chem

Stefan Rahimi, Xiaohong Liu, Chun Zhao, Zheng Lu, and Zachary J. Lebo

Viewed

Total article views: 2,371 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,572 755 44 2,371 101 53 57
  • HTML: 1,572
  • PDF: 755
  • XML: 44
  • Total: 2,371
  • Supplement: 101
  • BibTeX: 53
  • EndNote: 57
Views and downloads (calculated since 09 Jan 2020)
Cumulative views and downloads (calculated since 09 Jan 2020)

Viewed (geographical distribution)

Total article views: 2,371 (including HTML, PDF, and XML) Thereof 2,371 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 22 Feb 2025
Download
Short summary
Dark particles emitted to the atmosphere can absorb sunlight and heat the air. As these particles settle, they may darken the surface, especially over snow-covered regions like the Rocky Mountains. This darkening of the surface may lead to changes in snowpack, affecting the local meteorology and hydrology. We seek to evaluate whether these light-absorbing particles more prominently affect this region through their atmospheric presence or their on-snow presence.
Share
Altmetrics
Final-revised paper
Preprint