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Atmospheric deposition as a source of carbon and nutrients to barren, alpine soils of the Colorado Rocky Mountains
2012
Biogeosciences Discussions
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Many alpine areas are experiencing intense 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 nutrients. Given that bar-BGD 9,
doi:10.5194/bgd-9-2375-2012
fatcat:agoemc24ifhqzhukn3jrefogji