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Although the long-term average MTT (LAMTT) in each catchment was correlated with mean slope, coverage of forest (or conversely, other land use types), coverage of sand shale conglomerate, and groundwater storage, the multiple linear regression revealed that inter-catchment variation of LAMTT is principally controlled by the amount of groundwater storage.
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Catchment properties, including the vegetation coverage, portion of karst landform (POK), drainage area, surface roughness, mean topographic wetness index, mean slope, and mean aspect, were selected to test the influencing factors for the elasticity of actual evapotranspiration.
Lower slope snow is at times wet but upper slope coverage offers excellent conditions in most Alpine resorts.
Mean slope.
For each basin, a basin-wide mean slope was calculated using the ArcGIS slope tool.
The DEM data also reveal a relation between mean slope and mean local relief.
The fEPSP slope was expressed as a percentage of mean slope value before the tetanic stimulation.
Including MBSSD slopes from families with a PMB ≥0.8 and FBSSD slopes from families with a PMB ≤0.2 supports the previous results (mean slope, FBSSD species: 1.01, 95% C.I.: 0.98 1.03; mean slope, MBSSD species: 0.94, 95% C.I.: 91 97; difference between means, F1, 42 = 19.7, P = 0.00001; all means, C.I.s and tests weighted by 1/s.e. of the slope estimates).
The mean slope of the patients' bed was 29.5 ± 0.4°.
However, the mean slope for group 2 did not differ significantly from the mean slope for group 1 (p=0.12).
The model assumes that these comparison-specific regression slopes follow a common normal distribution, with mean slope β and common between-slopes variance σ.
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