Statistical and Physical Significance of Homogeneous Regions in Regional Flood Frequency Analysis

This study investigates formation homogeneous regions in regional flood frequency analysis (RFFA) and compares two RFFA methods, the quantile regression technique (QRT) and the index flood method (IFM). A total of 201 gauged stations from southeast Australia were adopted in this study. Multivariate statistical techniques were applied to form candidate regions. Also, regions are formed in the L-moments space (such as the L coefficient of variation (LCV) and L coefficient of skewness (LCS) of annual maximum flood data). Hosking and Wallis test statistics were used to find discordant sites and for testing the homogeneity of the assumed regions. No homogeneous regions were found in southeast Australia based on catchment characteristics data; however, homogeneous regions can be formed in the space of L-moments. It was found that regions formed in the L-moments space have little link with the catchment characteristics data space. The QRT provides more accurate flood quantile estimates than the IFM.

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Publication Details

Journal
Water
Published
2025-06-16
DOI
https://doi.org/10.3390/w17121799
Citations
10
Primary Topic
Hydrology and Drought Analysis
Type
article
Field-Weighted Citation Impact
11.05

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article

Statistical and Physical Significance of Homogeneous Regions in Regional Flood Frequency Analysis

Ataur Rahman, Zaved Khan, Haider Mannan, Ali Ahmed et al.
10 citations
Water
Hydrology and Drought Analysis
11.05
article

Statistical and Physical Significance of Homogeneous Regions in Regional Flood Frequency Analysis

Ataur Rahman, Zaved Khan, Haider Mannan, Ali Ahmed, Ridwan S. M. H. Rafi
article en
10 citations

Abstract

This study investigates formation homogeneous regions in regional flood frequency analysis (RFFA) and compares two RFFA methods, the quantile regression technique (QRT) and the index flood method (IFM). A total of 201 gauged stations from southeast Australia were adopted in this study. Multivariate statistical techniques were applied to form candidate regions. Also, regions are formed in the L-moments space (such as the L coefficient of variation (LCV) and L coefficient of skewness (LCS) of annual maximum flood data). Hosking and Wallis test statistics were used to find discordant sites and for testing the homogeneity of the assumed regions. No homogeneous regions were found in southeast Australia based on catchment characteristics data; however, homogeneous regions can be formed in the space of L-moments. It was found that regions formed in the L-moments space have little link with the catchment characteristics data space. The QRT provides more accurate flood quantile estimates than the IFM.

WaterVol. 17(12)
Commonwealth Scientific and Industrial Research Organisation (AU), Translational Research Institute (AU), North South University (BD), Western Sydney University (AU)
WaterNSW
Openalex Percentile: Top 1%
Hydrology and Drought Analysis
11.05
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