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(1984)
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A method for drawing slope maps from contour maps by automatic data acquisition and processingComputers & Geosciences, 6
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(1983)
Integrated logging and regeneration in the silvertop ash-stringybark forests of the Eden region -
E. O'Loughlin (1986)
Prediction of Surface Saturation Zones in Natural Catchments by Topographic AnalysisWater Resources Research, 22
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Zaslavsky Zaslavsky, Sinai Sinai (1981)
Surface hydrology: I. Explanation of phenomena, II. Distribution of raindrops, III. Causes of lateral flow, IV. Flow in sloping layered soil, V. In‐surface transient flow’, Proceedings of the American Society of Civil EngineeringJournal of Hydraulics Division, HY1
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( Linsley Jr., R. K. , Kohler, M. A. , and Paulus, J. L. H. 1949 Applied Hydrology, McGraw‐Hill, New York, 252 pp. )
Linsley Jr., R. K. , Kohler, M. A. , and Paulus, J. L. H. 1949 Applied Hydrology, McGraw‐Hill, New York, 252 pp.Linsley Jr., R. K. , Kohler, M. A. , and Paulus, J. L. H. 1949 Applied Hydrology, McGraw‐Hill, New York, 252 pp. , Linsley Jr., R. K. , Kohler, M. A. , and Paulus, J. L. H. 1949 Applied Hydrology, McGraw‐Hill, New York, 252 pp.
- Publisher
- Wiley
- Copyright
- Copyright © 1988 John Wiley & Sons, Ltd
- ISSN
- 0197-9337
- eISSN
- 1096-9837
- DOI
- 10.1002/esp.3290130404
- Publisher site
- See Article on Publisher Site
Abstract
A digital model for discretizing three‐dimensional terrain into small irregularly shaped polygons or elements based on contour lines and their orthogonals is described. From this subdivision the model estimates a number of topographic attributes for each element including the total upslope contributing area, element area, slope, and aspect. This form of discretization of a catchment produces natural units for problems involving water flow as either a surface or subsurface flow phenomenon. The model therefore has wide potential application for representing the three‐dimensionality of natural terrain and water flow processes in the fields of hydrology, sedimentology, and geomorphology. Three example applications are presented and discussed. They are the prediction of zones of surface saturation, the prediction of the distribution of potential daily solar radiation, and the prediction of zones of erosion and deposition in a catchment.
Journal
Earth Surface Processes and Landforms – Wiley
Published: Jun 1, 1988