Canopy Water Storage Capacity
Canopy water storage capacity (sc) is a key parameter for estimations of rainfall interception using a big-leaf model (blm). this study proposes a simple method for estimating sc. the crucial factor in this method is the canopy drying time (or wet canopy duration) after rainfall.. The corresponding stand water storage capacity of canopy humus was estimated at 0.55 mm in the ogf. only 7 kg ha ?1 of canopy humus were found in the sf and therefore the associated water storage capacity was negligible (0.002 mm). short-term water dynamics of epiphytic bryophyte vegetation and canopy humus. Abstract summarythe capacity of shrub canopy water storage is a key factor in controlling the rainfall interception. thus, it affects a variety of hydrological processes in water-limited arid desert ecosystems..
Canopy storage capacity is influenced by several variables, including canopy surface area, canopy architecture, and wind. different species with the same canopy area, but with differences in leaf hydrophobicity and water droplet retention, may produce different values of canopy storage capacity.. Canopy storage capacity (s) is the amount of water the canopy can hold while saturated. s is a key parameter of rainfall interception and other eco-hydrological processes.. Water storage among species. he bark water storage capacity of northern red oak (quercus rubra l.) was 2.5 times higher than sweet birch (betula lenta l.) (levia and herwitz, 2005). interception has been measured in the ield with natural rainfall using the volume control method (xiao et al., 2000b)..
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