2018
DOI: 10.1016/j.jhydrol.2018.01.025
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Influence of meteorological variables on rainfall partitioning for deciduous and coniferous tree species in urban area

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Cited by 86 publications
(98 citation statements)
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“…A previous study suggests that rainfall properties are a greater factor than crown characteristics in the interception of shrubs [30], but the canopy structure is less important for rainfall interception predictions, as indicated by the reformulated Gash Analytical Model [31]. Rainfall amount is found to be the most influential and direct factor [13,32]. The power function models fitted in our study can well define the relationship of canopy interception with rainfall amount (0.4 mm ≤ P ≤ 31.0 mm).…”
Section: Effects Of Rainfall Properties On Canopy Interceptionmentioning
confidence: 85%
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“…A previous study suggests that rainfall properties are a greater factor than crown characteristics in the interception of shrubs [30], but the canopy structure is less important for rainfall interception predictions, as indicated by the reformulated Gash Analytical Model [31]. Rainfall amount is found to be the most influential and direct factor [13,32]. The power function models fitted in our study can well define the relationship of canopy interception with rainfall amount (0.4 mm ≤ P ≤ 31.0 mm).…”
Section: Effects Of Rainfall Properties On Canopy Interceptionmentioning
confidence: 85%
“…The precipitation (P) was monitored during the growing seasons (May to September) in 2010 and 2011 with a tipping-bucket rain gauge (0.2 mm/tip) and a data logger (Model: JDZ02-1, Nanjing, China), which was extended above the forest canopy and mounted on an observation tower (45 m high and 50 m away from the sample area). When the adjacent rainfall interval time exceed 4 h, then it is divided into different rainfall events [13].…”
Section: Study Sitementioning
confidence: 99%
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“…A much smaller proportion of incident precipitation is directed along the stem and bole architecture of the trees, travelling directly down the tree trunk as stemflow. This portion can range from insignificant amounts (Bryant, Bhat, & Jacobs, ) to nearly 10% of incident rain (Tang, ), with fluxes highly dependent of tree species and characteristics, forest structure, and event dynamics (Carlyle‐Moses & Schooling, ; Levia, Van Stann, Mage, & Kelley‐Hauske, ; Zabret, Rakovec, & Šraj, ). The remaining water from a precipitation event is held in the canopy as interception, which will subsequently evaporate back to the atmosphere without reaching the forest floor (Carlyle‐Moses & Gash, ).…”
Section: Introductionmentioning
confidence: 99%