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Evaporation and storage of intercepted rain analysed by comparing two models applied to a boreal forest
Lunds universitet.
Luleå University of Technology, Department of Civil, Environmental and Natural Resources Engineering, Geosciences and Environmental Engineering.
Lunds universitet.
Lunds universitet.
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1999 (English)In: Agricultural and Forest Meteorology, ISSN 0168-1923, E-ISSN 1873-2240, Vol. 98-99, p. 595-604Article in journal (Refereed) Published
Abstract [en]

Rainfall and throughfall were measured during the summer of 1995. Rainfall interception is often simulated by a version of the well-known Rutter-Gash analytical model. In this study this model was compared to a model based on an exponential saturation equation. The concept of the ‘minimum method' for deriving canopy storage capacity and free throughfall coefficient by the Leyton-analysis, is compared to the concept of maximum storage capacity by reversing the models. Measured evaporation rate during rain events was found to be lower than simulated by the Penman equation using different known formulations for aerodynamic resistance. The concept of a high internal canopy resistance and decoupling of the canopy from the atmosphere should be analysed further in order to explain low evaporation during rainfall.

Place, publisher, year, edition, pages
1999. Vol. 98-99, p. 595-604
National Category
Geochemistry
Research subject
Applied Geology
Identifiers
URN: urn:nbn:se:ltu:diva-10158DOI: 10.1016/S0168-1923(99)00126-4ISI: 000085025900040Scopus ID: 2-s2.0-0033621423Local ID: 8e9c9ea0-b2e7-11db-bf9d-000ea68e967bOAI: oai:DiVA.org:ltu-10158DiVA, id: diva2:983098
Note
Godkänd; 1999; 20070202 (ysko)Available from: 2016-09-29 Created: 2016-09-29 Last updated: 2018-07-10Bibliographically approved

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Lundberg, Angela

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