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Modeling rainfall interception loss components of forests
Journal of Hydrology, 2020Abstract Interception loss, I, the amount of precipitation intercepted by forests and evaporated back to the atmosphere plays important roles in the water balance and the climate system by removing approximately one quarter of the annual precipitation from the terrestrial hydrologic cycle.
José Navar
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Ecohydrology, 2016 Interception loss accounts for a substantial portion of incident precipitation and evapotranspiration in forest ecosystems. Hence, identifying its magnitude is crucial for our understanding of biogeochemical cycling and related hydrological processes. In
Zongqiang Xie, Lei Su, Changming Zhao
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Journal of Geophysical Research, 1960
Field studies were conducted for the purpose of measuring interception loss from an actively transpiring grass cover. Continuous records of evapotranspiration were obtained from a pair of floating lysimeters in a grass field. The grass cover on and around each lysimeter was sprinkled alternately.
W. D. McMillan, R. H. Burgy
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Field studies were conducted for the purpose of measuring interception loss from an actively transpiring grass cover. Continuous records of evapotranspiration were obtained from a pair of floating lysimeters in a grass field. The grass cover on and around each lysimeter was sprinkled alternately.
W. D. McMillan, R. H. Burgy
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Effects of fire on interception loss in a coniferous and broadleaved mixed forest
Journal of Hydrology, 2022Lei Su, Yuan Miao
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Modelling of rainfall interception loss in agroforestry systems
Agroforestry Systems, 1991Two models of interception loss have been tested against new field data obtained in widely-spaced stands of Sitka spruce trees. The Gash model and a modified version of the Rutter model, have been used with data from an automatic weather station, to predict interception loss using parameters obtained from observations made in 1988 and 1989.
P G Jarvis
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Annual interception loss estimation with a simple equation
2012 IEEE Symposium on Humanities, Science and Engineering Research, 2012This study was designed to evaluate a simple equation to estimate an annual interception lost. To design the equation, the input of the equation was modified to a very high resolution data. Statistical relationship between precipitation, temporal resolution and rainfall intensity was determined.
Abu Bakar, Azinoor Azida +5 more
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Journal of Arid Environments, 1999
Abstract In a semi-arid plant community dominated by the Tamaulipan matorral of north-eastern Mexico the quantitative importance of interception loss and the applicability of the Gash analytical rainfall interception loss model were evaluated. Interception loss was estimated from measurements of incident precipitation and throughfall.
José Návar +2 more
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Abstract In a semi-arid plant community dominated by the Tamaulipan matorral of north-eastern Mexico the quantitative importance of interception loss and the applicability of the Gash analytical rainfall interception loss model were evaluated. Interception loss was estimated from measurements of incident precipitation and throughfall.
José Návar +2 more
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A note on the interception loss equation
Journal of Geophysical Research, 1960Interception is the process in which precipitation is caught by a vegetative canopy and redistributed to the ground, to the atmosphere, or into the plant. Interception loss is that portion of the precipitation which is returned to the atmosphere through evaporation from plant surfaces or is absorbed into the plant.
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Rainfall Interception Loss by Forest Canopies
2011When rain falls onto a forest a proportion is intercepted by the canopy and evaporates back into the atmosphere, playing no further part in the terrestrial portion of the hydrologic cycle. This canopy interception loss, I c, can be appreciable (Table 20.1).
Darryl E. Carlyle-Moses, John H. C. Gash
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Research on Interception Losses and Soil Moisture Relationships
1988Few scientists understand better than H. L. Penman (1963) the complexity of finding out what happens to the rain: “With few exceptions, they [i.e., field measurements] involve small differences between large quantities (of water) that cannot be measured with precision—rainfall, interception, surface runoff, streamflow, soil water content, stored ...
J. D. Helvey, J. H. Patric
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