Atmospheric deposition as a source of carbon and nutrients to an alpine catchment of the Colorado Rocky Mountains
Many alpine areas are experiencing deglaciation, biogeochemical changes driven by temperature rise, and changes in atmospheric deposition. There is mounting evidence that the water quality of alpine streams may be related to these changes, including rising atmospheric deposition of carbon (C) and nu...
Main Authors: | N. Mladenov, M. W. Williams, S. K. Schmidt, K. Cawley |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2012-08-01
|
Series: | Biogeosciences |
Online Access: | http://www.biogeosciences.net/9/3337/2012/bg-9-3337-2012.pdf |
Similar Items
-
Mercury dynamics in the Rocky Mountain, Colorado, snowpack
by: X. Faïn, et al.
Published: (2013-06-01) -
Modeling geogenic and atmospheric nitrogen through the East River Watershed, Colorado Rocky Mountains.
by: Taylor Maavara, et al.
Published: (2021-01-01) -
Summertime Soil-Atmosphere Ammonia Exchange in the Colorado Rocky Mountain Front Range Pine Forest
by: Amy Hrdina, et al.
Published: (2019-02-01) -
New particle formation in the Front Range of the Colorado Rocky Mountains
by: A. Wiedensohler, et al.
Published: (2008-03-01) -
The genus Hebeloma in the Rocky Mountain Alpine Zone
by: Cathy L. Cripps, et al.
Published: (2019-02-01)