The DOI matches its Crossref record; 15 of the 15 references it cites were found in a registry or an index.
Modeling subsurface stormflow on steeply sloping forested watersheds
Abstract
Five mathematical models for predicting subsurface flow were compared to discharge measurements made by Hewlett and Hibbert (1963) on a uniform sloping soil trough at the Coweeta Hydrologic Laboratory. The models included one‐ and two‐dimensional finite element models based on the Richards equation, a kinematic wave model, and two simple storage‐discharge models based on the kinematic wave and Boussinesq assumptions. The simple models simulated the subsurface response and water table positions as well as the more complex models based on the Richards equation and were much more economical to use from the point of view of computational costs. Such models have features that would allow them to be incorporated into more complex watershed models, thus placing hydrologic prediction on a more physically correct and less empirical footing.
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Cites
Macropores and water flow in soils
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The Rôle of infiltration in the hydrologic cycle
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Partial Area Contributions to Storm Runoff in a Small New England Watershed
Dunne, T., & Black, R. D. (1970) · Water Resources Research · doi:10.1029/wr006i005p01296 · Cited by 1,152
Streamflow generation in a forested watershed, New Zealand
Mosley, M. P. (1979) · Water Resources Research · doi:10.1029/wr015i004p00795 · Cited by 416
THROUGHFLOW, OVERLAND FLOW AND EROSION
Kirkby, M. J., & Chorley, R. J. (1967) · International Association of Scientific Hydrology Bulletin · doi:10.1080/02626666709493533 · Cited by 386
Role of subsurface flow in generating surface runoff: 2. Upstream source areas
Freeze, R. A. (1972) · Water Resources Research · doi:10.1029/wr008i005p01272 · Cited by 366
Moisture and energy conditions within a sloping soil mass during drainage
Hewlett, J. D., & Hibbert, A. R. (1963) · Journal of Geophysical Research · doi:10.1029/jz068i004p01081 · Cited by 354
SUBSURFACE STORMFLOW FROM FORESTED SLOPES
WHIPKEY, R. Z. (1965) · International Association of Scientific Hydrology Bulletin · doi:10.1080/02626666509493392 · Cited by 335
Kinematic subsurface stormflow
Beven, K. (1981) · Water Resources Research · doi:10.1029/wr017i005p01419 · Cited by 244
Clarke, R. T. (1973) · Journal of Hydrology · doi:10.1016/0022-1694(73)90089-9 · Cited by 237
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Sutanudjaja, E. H., van Beek, R., Wanders, N., Wada, Y., Bosmans, J. H. C., Drost, N., van der Ent, R. J., de Graaf, I. E. M., Hoch, J. M., de Jong, K., et al. (2018) · Geoscientific Model Development · doi:10.5194/gmd-11-2429-2018 · Cited by 667
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van Beek, L. P. H., Wada, Y., & Bierkens, M. F. P. (2011) · Water Resources Research · doi:10.1029/2010wr009791 · Cited by 555
Eckhardt, K., & Ulbrich, U. (2003) · Journal of Hydrology · doi:10.1016/j.jhydrol.2003.08.005 · Cited by 465
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Metadata
- Authors
- Sloan, P. G., & Moore, I. D.
- Venue
- Water Resources Research
- Publisher
- American Geophysical Union (AGU)
- Published
- 1984-12
- Volume
- 20
- Issue
- 12
- Pages
- 1815-1822
- ISSN
- 0043-1397 (ISSN-L)
- 1944-7973
- OpenAlex
- W2161334450
- Cited by
- 294
- References
- 15
- FWCI
- 4.96
- Type
- journal article
- Language
- en
- Open access
- closed
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Data sources
Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.
