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Controls on the temporal and spatial variability of soil moisture in a mountainous landscape: the signature of snow and complex terrain

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Figure

Fig. 1. Location and instrumentation of the Treeline study site in the Dry Creek Experimental Watershed, near Boise, Idaho, USA.
Fig. 2. Kriged maps (calculated with Surfer 8.0, Golden Software)cent sand contents of the soilfor the changes in the rank of soil moisture mean relative differenceof soil depths (a), snow depths at maximum accumulation (b), per- (c), and the rank change index (RCI, d)measured at 57 points of the Treeline study grid.
Fig. 3. Timing of the precipitationwater year. The curves show soil moisture contents observed at 15,45, 75, and 105 cm depths in a time domain reflectometry (TDR)instrumented soil pit of a deep soil profile
Fig. 5. Relationships of the rank change index (a) and mean relativedifference (MRD) standard deviation (b) with catchment MRD.
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