Abstract

Abstract. The objective of this paper is to assess the performance of methods that predict low flows and flood runoff in ungauged catchments. The aim is to learn from the similarities and differences between catchments in different places, and to interpret the differences in performance in terms of the underlying climate-landscape controls. The assessment is performed at two levels. The Level 1 assessment is a meta-analysis of 14 low flow prediction studies reported in the literature involving 3112 catchments, and 20 flood prediction studies involving 3023 catchments. The Level 2 assessment consists of a more focused and detailed analysis of individual basins from selected studies from Level 1 in terms of how the leave-one-out cross-validation performance depends on climate and catchment characteristics as well as on the regionalisation method. The results indicate that both flood and low flow predictions in ungauged catchments tend to be less accurate in arid than in humid climates and more accurate in large than in small catchments. There is also a tendency towards a somewhat lower performance of regressions than other methods in those studies that apply different methods in the same region, while geostatistical methods tend to perform better than other methods. Of the various flood regionalisation approaches, index methods show significantly lower performance in arid catchments than regression methods or geostatistical methods. For low flow regionalisation, regional regressions are generally better than global regressions.

Highlights

  • Estimating flood and low flow discharges in ungauged basins are among the most fundamental challenges in catchment hydrology

  • A number of studies are available in the literature that have performed such a comparison and the results are indicated as grey lines in Fig. 3

  • The comparisons clearly show that the regional regressions always perform better than the global regressions

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Summary

Introduction

Estimating flood and low flow discharges in ungauged basins are among the most fundamental challenges in catchment hydrology. The classical approach consists of subdividing the study domain into a number of fixed, contiguous regions which are used to regionalise floods or low flows for all catchments in the area (e.g. as used in the index flood method, Dalrymple, 1960). The assumption of this method is that areas close to each other are characterised by similar climate, topography, geology, soils and land use, which gives rise to similar catchment hydrological response and to similar floods or low flows. These include cluster analysis using catchment characteristics (Nathan and McMahon, 1990), residuals from a Published by Copernicus Publications on behalf of the European Geosciences Union

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