This paper gives details of how the spatially variable rainfall partitioning model, presented in Davie and Durocher, (1997) [Hydrol. Process., 11, 1509±1523], is parameterized, and the testing of its capabilities. A majority of the input parameters required for running the model can be derived from
A model to consider the spatial variability of rainfall partitioning within deciduous canopy. I. Model description
✍ Scribed by T. J. A. DAVIE; M. G. DUROCHER
- Publisher
- John Wiley and Sons
- Year
- 1997
- Tongue
- English
- Weight
- 256 KB
- Volume
- 11
- Category
- Article
- ISSN
- 0885-6087
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✦ Synopsis
In this ®rst paper of two, a numerical simulation model capable of simulating the spatial variability of rainfall partitioning within a canopy is presented. The second paper details how the model is parameterized, and some testing of its capabilities.
The ®rst stage of the model is to derive the mature canopy structure. This is achieved through simpli®ed individual tree structures and a random placement routine based on a modi®ed Poisson distribution. Following this the spatial discretization for throughfall is attained as a series of layers of triangles with a tree trunk at every apex. The number of layers is derived from the leaf area index through a modi®ed Poisson distribution. Seasonal variation in the deciduous canopy is simulated through a time vector routine. The rainfall partitioning section of the model is based upon the Rutter model which has been modi®ed to each individual triangle layer. The main feature of this model is that it oers a method of simulating rainfall partitioning at a scale that is a function of the size of the elementary physical components (tree and leaf scale). This can be used to investigate soil moisture variations under a canopy, or to study the variations within the forest hydrological processes themselves.
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