Explaining CO<sub>2</sub> fluctuations observed in snowpacks
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Published:2018-02-09
Issue:3
Volume:15
Page:847-859
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ISSN:1726-4189
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Container-title:Biogeosciences
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language:en
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Short-container-title:Biogeosciences
Author:
Graham Laura,Risk David
Abstract
Abstract. Winter soil carbon dioxide (CO2) respiration is a significant
and understudied component of the global carbon (C) cycle. Winter soil CO2
fluxes can be surprisingly variable, owing to physical factors such as
snowpack properties and wind. This study aimed to quantify the effects of
advective transport of CO2 in soil–snow systems on the subdiurnal to
diurnal (hours to days) timescale, use an enhanced diffusion model to
replicate the effects of CO2 concentration depletions from persistent
winds, and use a model–measure pairing to effectively explore what is
happening in the field. We took continuous measurements of CO2
concentration gradients and meteorological data at a site in the Cape Breton
Highlands of Nova Scotia, Canada, to determine the relationship between wind
speeds and CO2 levels in snowpacks. We adapted a soil CO2 diffusion
model for the soil–snow system and simulated stepwise changes in transport
rate over a broad range of plausible synthetic cases. The goal was to mimic
the changes we observed in CO2 snowpack concentration to help elucidate
the mechanisms (diffusion, advection) responsible for observed variations. On
subdiurnal to diurnal timescales with varying winds and constant snow
levels, a strong negative relationship between wind speed and CO2
concentration within the snowpack was often identified. Modelling clearly
demonstrated that diffusion alone was unable to replicate the high-frequency
CO2 fluctuations, but simulations using above-atmospheric snowpack
diffusivities (simulating advective transport within the snowpack) reproduced
snow CO2 changes of the observed magnitude and speed. This confirmed that
wind-induced ventilation contributed to episodic pulsed emissions from the
snow surface and to suppressed snowpack concentrations. This study improves
our understanding of winter CO2 dynamics to aid in continued
quantification of the annual global C cycle and demonstrates a preference
for continuous wintertime CO2 flux measurement systems.
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics
Reference32 articles.
1. Barry, R. G.: Climate-ice interactions, in: Encyclopedia of Earth System
Science, edited by: Nierenberg, W. A., Academic Press, San Diego, CA,
517–524, 1992. a 2. Bowling, D. R. and Massman, W. J.: Persistent wind-induced enhancement of
diffusive CO2 transport in a mountain forest snowpack, J. Geophys Res.,
116, G04006, https://doi.org/10.1029/2011JG001722, 2011. a, b, c, d, e, f, g 3. Bowling, D. R., Massman, W. J., Schaeffer, S. M., Burns, S. P., Monson, R.
K., and Williams, M. W.: Biological and physical influences on the carbon
isotope content of CO2 in a subalpine forest snowpack, Niwot Ridge,
Colorado, Biogeochemistry, 95, 37–59, https://doi.org/10.1007/s10533-008-9233-4, 2009. a 4. Brooks, P. D., Williams, M. W., and Schmidt, S. K.: Microbial activity under
alpine snow packs, Niwot Ridge, Colorado, Biogeochemistry, 32, 93–113, 1996. a, b 5. Coxson, D. S. and Parkinson, D.: Winter respiratory activity in aspen
woodland forest floor litter and soils, Soil Biol. Biochem., 19, 49–59,
1987. a, b
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