Experimental investigation of the predictive capabilities of data driven modeling techniques in hydrology - Part 2: Application

Created by W.Langdon from gp-bibliography.bib Revision:1.7615

@Article{Elshorbagy:2010a:HESS,

• title = "Experimental investigation of the predictive capabilities of data driven modeling techniques in hydrology - Part 2: Application",
• author = "A. Elshorbagy and G. Corzo and S. Srinivasulu and D. P. Solomatine",
• journal = "Hydrology and Earth System Sciences",
• year = "2010",
• volume = "14",
• number = "10",
• pages = "1943--1961",
• month = "14 " # oct,
• keywords = "genetic algorithms, genetic programming",
• ISSN = "10275606",
• bibsource = "OAI-PMH server at www.doaj.org",
• language = "eng",
• oai = "oai:doaj-articles:0b5621edb6cf47d7aee8cedce805592b",
• source = "Hydrology and Earth System Sciences",
• URL = "http://www.hydrol-earth-syst-sci.net/14/1943/2010/hess-14-1943-2010.pdf",
• size = "19 pages",
• abstract = "In this second part of the two-part paper, the data driven modeling (DDM) experiment, presented and explained in the first part, is implemented. Inputs for the five case studies (half-hourly actual evapotranspiration, daily peat soil moisture, daily till soil moisture, and two daily rainfall-runoff datasets) are identified, either based on previous studies or using the mutual information content. Twelve groups (realisations) were randomly generated from each data set by randomly sampling without replacement from the original data set. Neural networks (ANNs), genetic programming (GP), evolutionary polynomial regression (EPR), Support vector machines (SVM), M5 model trees (M5), K-nearest neighbors (K-nn), and multiple linear regression (MLR) techniques are implemented and applied to each of the 12 realizations of each case study. The predictive accuracy and uncertainties of the various techniques are assessed using multiple average overall error measures, scatter plots, frequency distribution of model residuals, and the deterioration rate of prediction performance during the testing phase. Gamma test is used as a guide to assist in selecting the appropriate modeling technique. Unlike two nonlinear soil moisture case studies, the results of the experiment conducted in this research study show that ANNs were a sub-optimal choice for the actual evapotranspiration and the two rainfall-runoff case studies. GP is the most successful technique due to its ability to adapt the model complexity to the model ed data. EPR performance could be close to GP with datasets that are more linear than nonlinear. SVM is sensitive to the kernel choice and if appropriately selected, the performance of SVM can improve. M5 performs very well with linear and semi linear data, which cover wide range of hydrological situations. In highly nonlinear case studies, ANNs, K-nn, and GP could be more successful than other modelling techniques. K-nn is also successful in linear situations, and it should not be ignored as a potential modelling technique for hydrological applications.",
• notes = "See also \cite{Elshorbagy:2010:HESS}",

}

Genetic Programming entries for Amin Elshorbagy Gerald Corzo Perez Sanaga Srinivasulu Dimitri P Solomatine

Citations