Normalizing Time in Terms of Space: What Drives the Fate of Spring Thaw-Released N in the Sloping Arctic Landscape?
28 Pages Posted: 21 Apr 2022
Abstract
In the Arctic tundra, snowmelt is followed by soil thaw allowing water and dissolved nutrients to move downslope. However, the fate of the released nitrogen (N) remains unclear, which includes the fraction of N that is lost to downslope transport or converted to N gasses.
Keywords: Arctic tundra, snowmelt, topography, structural equation model, nitrogen cycling, N2O emission
Suggested Citation: Suggested Citation
Rasmussen, Laura Helene and Mortensen, Louise H. and Ambus, Per and Michelsen, Anders and Elberling, Bo, Normalizing Time in Terms of Space: What Drives the Fate of Spring Thaw-Released N in the Sloping Arctic Landscape?. Available at SSRN: https://ssrn.com/abstract=4089107 or http://dx.doi.org/10.2139/ssrn.4089107
Do you have a job opening that you would like to promote on SSRN?
Feedback
Feedback to SSRN