Ta. Rahn et al., FLUX CHAMBER MEASUREMENTS OF ANOMALOUS CO2 EMISSION FROM THE FLANKS OF MAMMOTH MOUNTAIN, CALIFORNIA, Geophysical research letters, 23(14), 1996, pp. 1861-1864
The CO2 fluxes involved in the mass mortality of large stands of timbe
r on the flanks of Mammoth Mountain in California's Sierra Nevada were
measured and spatial and temporal inhomogeneities observed. Our estim
ate of the integrated nux over the total area of tree-kill is on the o
rder of 400 t day(-1). Small scale spatial variability most likely ref
lects varying degrees of shallow bedrock fracture and soil compaction.
Temporal variability suggests a fast response to subsurface condition
s such as seismically induced crack propagation, degassing of intruded
magma, or changing groundwater/soil moisture conditions.