EVALUATION OF CLUSTER-BASED RECTANGULAR PULSES POINT PROCESS MODELS FOR RAINFALL

Citation
T. Velghe et al., EVALUATION OF CLUSTER-BASED RECTANGULAR PULSES POINT PROCESS MODELS FOR RAINFALL, Water resources research, 30(10), 1994, pp. 2847-2857
Citations number
16
Categorie Soggetti
Limnology,"Environmental Sciences","Water Resources
Journal title
ISSN journal
00431397
Volume
30
Issue
10
Year of publication
1994
Pages
2847 - 2857
Database
ISI
SICI code
0043-1397(1994)30:10<2847:EOCRPP>2.0.ZU;2-9
Abstract
This technical note presents a comparison of cluster-based point rainf all models using the historical hourly rainfall data observed between 1949 and 1976 at Denver, Colorado. The Denver data are used to analyze the performance of three classes of models, namely, the Bartlett-Lewi s model, the geometric Neyman-Scott model and the Poisson Neyman-Scott model. The original formulation of the structure of each model, as we ll as the modified description developed in order to improve the zero depth probability, is considered in this study. Rodriguez-Iturbe et al . (1987a) concluded that it is unlikely that empirical analysis of rai nfall data can be used to choose between the Bartlett-Lewis model and the Neyman-Scott model. In a subsequent paper, Rodriguez-Iturbe et al. (1987b) argued that the choice of the distribution of the number of c ells per storm for the Neyman-Scott model, either geometric or Poisson , has no general bias effect on the stochastic structure. Some investi gators (e.g., Burlando and Rosso, 1991), however, reported results con tradictory to those of the previous authors. In light of these observa tions this note investigates the performance of the cluster-based mode ls. For the Denver data the geometric Neyman-Scott model yields better results compared to the Poisson Neyman-Scott model. Moreover, the Bar tlett-Lewis model is shown to be very sensitive to the sets of moment equations used in the parameter estimation. This sensitivity is not ob served in the Neyman-Scott scheme and is believed to be a drawback for applying the Bartlett-Lewis model in hydrologic simulation studies.