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Hydrol. Earth Syst. Sci. Discuss., 2, 1359-1404, 2005
www.hydrol-earth-syst-sci-discuss.net/2/1359/2005/
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A distributed continuous simulation model to identify critical source areas of phosphorus at the catchment scale: model description

B. K. Koo, S. M. Dunn, and R. C. Ferrier
The Macaulay Institute, Craigiebuckler, Aberdeen AB15 8QH, UK

Abstract. This paper presents CAMEL (Chemicals from Agricultural Management and Erosion Losses), a distributed continuous simulation model to simulate daily phosphorus (P) transformations and transport at the catchment scale. CAMEL is a process-oriented mass-balance model that is based on both analytical and numerical approaches. In the model, a catchment is represented using a network of square grid cells each of which is comprised of various storages of water, sediment and P. Most of hydrological processes, soil erosion, sediment transport, and P transformations and transport are described using process-based equations. The P transformations between five P storages (active organic, stable organic, labile, active inorganic, and stable organic) are described using first-order kinetic equations. A comprehensive cascade routing scheme is used to simulate P retention and transport along the channel system. Dissolved P is also transported by groundwater flows, described using a two-dimensional Boussinesq equation. CAMEL simulates both surface and subsurface processes explicitly and therefore is suitable for catchment-scale applications. The distributed, process-oriented structure of CAMEL enables the model to be used for identifying critical source areas of P at the catchment-scale. CAMEL is also computationally efficient, allowing for long-term scale applications.

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Citation: Koo, B. K., Dunn, S. M., and Ferrier, R. C.: A distributed continuous simulation model to identify critical source areas of phosphorus at the catchment scale: model description, Hydrol. Earth Syst. Sci. Discuss., 2, 1359-1404, 2005.   Bibtex   EndNote   Reference Manager