Articles | Volume 16, issue 3
https://doi.org/10.5194/acp-16-1303-2016
https://doi.org/10.5194/acp-16-1303-2016
Research article
 | 
05 Feb 2016
Research article |  | 05 Feb 2016

Observed high-altitude warming and snow cover retreat over Tibet and the Himalayas enhanced by black carbon aerosols

Y. Xu, V. Ramanathan, and W. M. Washington

Viewed

Total article views: 5,087 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,778 2,156 153 5,087 436 117 162
  • HTML: 2,778
  • PDF: 2,156
  • XML: 153
  • Total: 5,087
  • Supplement: 436
  • BibTeX: 117
  • EndNote: 162
Views and downloads (calculated since 10 Jul 2015)
Cumulative views and downloads (calculated since 10 Jul 2015)

Cited

Saved (preprint)

Latest update: 21 Nov 2024
Download
Short summary
We show that black carbon aerosol pollution is likely the dominant factor in causing the accelerated retreat of snowpack in Himalayas. The simulated snow fraction and surface albedo change at the surface, as well as the enhanced warming at higher elevations, are remarkably similar to observations in past decades. The reason for the model's ability to simulate the observed trends is that we replace the model-simulated black carbon forcing with one that is constrained by observations.
Altmetrics
Final-revised paper
Preprint