Articles | Volume 12, issue 23
https://doi.org/10.5194/bg-12-7349-2015
https://doi.org/10.5194/bg-12-7349-2015
Research article
 | 
15 Dec 2015
Research article |  | 15 Dec 2015

The influence of warm-season precipitation on the diel cycle of the surface energy balance and carbon dioxide at a Colorado subalpine forest site

S. P. Burns, P. D. Blanken, A. A. Turnipseed, J. Hu, and R. K. Monson

Viewed

Total article views: 3,581 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,960 1,450 171 3,581 311 117 127
  • HTML: 1,960
  • PDF: 1,450
  • XML: 171
  • Total: 3,581
  • Supplement: 311
  • BibTeX: 117
  • EndNote: 127
Views and downloads (calculated since 16 Jun 2015)
Cumulative views and downloads (calculated since 16 Jun 2015)

Cited

Saved (final revised paper)

Latest update: 15 Nov 2024
Download
Short summary
The effect of warm-season precipitation on environmental conditions and ecosystem-scale fluxes at a high-elevation subalpine forest site was investigated. As would be expected (based on the surface energy balance), precipitation caused an increase in latent heat flux (evapotranspiration) and a decrease in sensible heat flux. The evaporative component of evapotranspiration was, on average, estimated to be around 6% in dry conditions and between 15-25% in partially wet conditions.
Altmetrics
Final-revised paper
Preprint