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Comparison of two approaches for generation of daily rainfall data
Authors:R. Srikanthan  T. I. Harrold  A. Sharma  T. A. McMahon
Affiliation:(1) Hydrology Unit, Bureau of Meteorology, Melbourne, Australia;(2) 76 Lawson Avenue, Singleton, NSW, 2330, Australia;(3) School of Civil and Environmental Engineering, The University of New South Wales, Sydney, Australia;(4) Department of Civil and Environmental Engineering, University of Melbourne, Melbourne, Australia;(5) Cooperative Research Centre for Catchment Hydrology, Monash University, Clayton, Australia
Abstract:There has been extensive research on the problem of stochastically generating daily rainfall sequences for use in water management applications. Srikanthan and McMahon [Australia Water Resources Council, Canberra, 1985] proposed a transition probability matrix (TPM) model that performs better for Australian rainfall than many alternative models, particularly where long records (say 100 years) are available. Boughton [Report 99/9, CRC for Catchment Hydrology, Monash University, Melbourne, 21pp, 1999] incorporated an empirical adjustment into the TPM model that allows the model to reproduce the observed variability in the annual rainfall. More recently, Harrold et al. [Water Resour Res 39(10, 12):1300, 1343, 2003a,b] proposed nonparametric models for the generation of daily rainfall occurrences and rainfall amounts on wet days. By conditioning on short, medium and long-term characteristics, this approach is also able to preserve the variability in annual rainfall. In this study, the above two approaches were used to generate daily rainfall data for Sydney and Melbourne, and the results evaluated. Both approaches preserved most of the daily, monthly and annual characteristics that were compared, with the nonparametric approach providing marginally better performance at the cost of greater model complexity. The nonparametric approach was also able to preserve the variability and persistence in the annual number of wet days.
Keywords:Stochastic generation  Daily rainfall  Transition probability matrix  Nonparametric
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