Comparison of two approaches for generation of daily rainfall data

被引:27
|
作者
Srikanthan, R
Harrold, TI
Sharma, A
McMahon, TA
机构
[1] Bur Meteorol, Hydrol Unit, Melbourne, Vic, Australia
[2] Univ New S Wales, Sch Civil & Environm Engn, Sydney, NSW, Australia
[3] Univ Melbourne, Dept Civil & Environm Engn, Melbourne, Vic, Australia
[4] Monash Univ, Cooperat Res Ctr Catchment Hydrol, Clayton, Vic 3168, Australia
关键词
stochastic generation; daily rainfall; transition probability matrix; nonparametric;
D O I
10.1007/s00477-004-0226-0
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
There has been extensive research oil the problem of stochastically generating daily rainfall sequences for use in water management applications. Srikanthan and McMahon [Australia Water Resources Council, Canberra, 19851 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, 2 1 pp. 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 nonpararnetric models for the generation of daily rainfall Occurrences and rainfall amounts oil 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.
引用
收藏
页码:215 / 226
页数:12
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