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: 2,080 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,354 687 39 2,080 94 43 48
  • HTML: 1,354
  • PDF: 687
  • XML: 39
  • Total: 2,080
  • Supplement: 94
  • BibTeX: 43
  • EndNote: 48
Views and downloads (calculated since 09 Jan 2020)
Cumulative views and downloads (calculated since 09 Jan 2020)

Viewed (geographical distribution)

Total article views: 2,080 (including HTML, PDF, and XML) Thereof 2,089 with geography defined and -9 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 26 Jul 2024
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.
Altmetrics
Final-revised paper
Preprint