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Advective transport of CO2in permeable media induced by atmospheric pressure fluctuations: 2. Observational evidence under snowpacks
2006
Journal of Geophysical Research
1] Meadow and forest CO 2 amounts sampled beneath an approximately meter deep (steady state) snowpack at a subalpine site in southern Rocky Mountains of Wyoming are observed to vary by nearly 200 ppm over periods ranging from 4 to 15 days. This work employs the model of periodic, pressure-induced, advective transport in permeable media developed in part 1 of this study to investigate these CO 2 fluctuations. With the aid of this physically based model, inferences are made about the nature of
doi:10.1029/2006jg000164
fatcat:n32xm3ngk5amhpjwhprrbpiuyu