Modelling streambank erosion potential using maximum entropy in a central Appalachian watershed
We used maximum entropy to model streambank erosion potential (SEP) in a central Appalachian watershed to help prioritize sites for management. Model development included measuring erosion rates, application of a quantitative approach to locate Target Eroding Areas (TEAs), and creation of maps of bo...
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doaj-546949823c5f4a179463df85a19f23792020-11-24T22:29:08ZengCopernicus PublicationsProceedings of the International Association of Hydrological Sciences2199-89812199-899X2015-03-0136712212710.5194/piahs-367-122-2015Modelling streambank erosion potential using maximum entropy in a central Appalachian watershedJ. Pitchford0M. Strager1A. Riley2L. Lin3J. Anderson4West Virginia University, Division of Forestry and Natural Resources, PO Box 6125, Morgantown, West Virginia 26506-6125, USAWest Virginia University, Division of Forestry and Natural Resources, PO Box 6125, Morgantown, West Virginia 26506-6125, USAWest Virginia University, Division of Forestry and Natural Resources, PO Box 6125, Morgantown, West Virginia 26506-6125, USAWest Virginia University, Department of Civil and Environmental Engineering, PO Box 6103, Morgantown, West Virginia 26506-6125, USAWest Virginia University, Division of Forestry and Natural Resources, PO Box 6125, Morgantown, West Virginia 26506-6125, USAWe used maximum entropy to model streambank erosion potential (SEP) in a central Appalachian watershed to help prioritize sites for management. Model development included measuring erosion rates, application of a quantitative approach to locate Target Eroding Areas (TEAs), and creation of maps of boundary conditions. We successfully constructed a probability distribution of TEAs using the program Maxent. All model evaluation procedures indicated that the model was an excellent predictor, and that the major environmental variables controlling these processes were streambank slope, soil characteristics, bank position, and underlying geology. A classification scheme with low, moderate, and high levels of SEP derived from logistic model output was able to differentiate sites with low erosion potential from sites with moderate and high erosion potential. A major application of this type of modelling framework is to address uncertainty in stream restoration planning, ultimately helping to bridge the gap between restoration science and practice.https://www.proc-iahs.net/367/122/2015/piahs-367-122-2015.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
J. Pitchford M. Strager A. Riley L. Lin J. Anderson |
spellingShingle |
J. Pitchford M. Strager A. Riley L. Lin J. Anderson Modelling streambank erosion potential using maximum entropy in a central Appalachian watershed Proceedings of the International Association of Hydrological Sciences |
author_facet |
J. Pitchford M. Strager A. Riley L. Lin J. Anderson |
author_sort |
J. Pitchford |
title |
Modelling streambank erosion potential using maximum entropy in a central Appalachian watershed |
title_short |
Modelling streambank erosion potential using maximum entropy in a central Appalachian watershed |
title_full |
Modelling streambank erosion potential using maximum entropy in a central Appalachian watershed |
title_fullStr |
Modelling streambank erosion potential using maximum entropy in a central Appalachian watershed |
title_full_unstemmed |
Modelling streambank erosion potential using maximum entropy in a central Appalachian watershed |
title_sort |
modelling streambank erosion potential using maximum entropy in a central appalachian watershed |
publisher |
Copernicus Publications |
series |
Proceedings of the International Association of Hydrological Sciences |
issn |
2199-8981 2199-899X |
publishDate |
2015-03-01 |
description |
We used maximum entropy to model streambank erosion potential (SEP) in a central Appalachian watershed to help prioritize sites for management. Model development included measuring erosion rates, application of a quantitative approach to locate Target Eroding Areas (TEAs), and creation of maps of boundary conditions. We successfully constructed a probability distribution of TEAs using the program Maxent. All model evaluation procedures indicated that the model was an excellent predictor, and that the major environmental variables controlling these processes were streambank slope, soil characteristics, bank position, and underlying geology. A classification scheme with low, moderate, and high levels of SEP derived from logistic model output was able to differentiate sites with low erosion potential from sites with moderate and high erosion potential. A major application of this type of modelling framework is to address uncertainty in stream restoration planning, ultimately helping to bridge the gap between restoration science and practice. |
url |
https://www.proc-iahs.net/367/122/2015/piahs-367-122-2015.pdf |
work_keys_str_mv |
AT jpitchford modellingstreambankerosionpotentialusingmaximumentropyinacentralappalachianwatershed AT mstrager modellingstreambankerosionpotentialusingmaximumentropyinacentralappalachianwatershed AT ariley modellingstreambankerosionpotentialusingmaximumentropyinacentralappalachianwatershed AT llin modellingstreambankerosionpotentialusingmaximumentropyinacentralappalachianwatershed AT janderson modellingstreambankerosionpotentialusingmaximumentropyinacentralappalachianwatershed |
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