Abstract

Abstract. Rainfall is the most important input for rainfall–runoff models. It is usually measured at specific sites on a daily or sub-daily timescale and requires interpolation for further application. This study aims to evaluate whether a higher temporal and spatial resolution of rainfall can lead to improved model performance. Four different gridded hourly and daily rainfall datasets with a spatial resolution of 1 km × 1 km for the state of Baden-Württemberg in Germany were constructed using a combination of data from a dense network of daily rainfall stations and a less dense network of sub-daily stations. Lumped and spatially distributed HBV models were used to investigate the sensitivity of model performance to the spatial resolution of rainfall. The four different rainfall datasets were used to drive both lumped and distributed HBV models to simulate daily discharges in four catchments. The main findings include that (1) a higher temporal resolution of rainfall improves the model performance if the station density is high; (2) a combination of observed high temporal resolution observations with disaggregated daily rainfall leads to further improvement in the tested models; and (3) for the present research, the increase in spatial resolution improves the performance of the model insubstantially or only marginally in most of the study catchments.

Highlights

  • Rainfall is a primary driver of hydrological models and can impact catchment runoff response significantly (Obled et al, 1994; Ly et al, 2013)

  • The results show that all four datasets can reproduce relatively accurate historical daily streamflow series for all selected catchments

  • We investigated the impacts of temporal and spatial variability of rainfall in model simulation and parameter estimation

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Summary

Introduction

Rainfall is a primary driver of hydrological models and can impact catchment runoff response significantly (Obled et al, 1994; Ly et al, 2013). Kobold and Brilly (2006) derived hourly areal rainfall interpolated from various numbers of rain gauges to quantitatively assess the sensitivity of peak flow to the uncertainty of rainfall data using an HBV model. They found that the error in rainfall may lead to even greater error in flood peaks. Bárdossy and Das (2008) studied the impact of spatial variability of rainfall by varying the distribution of raingauge networks They found that the transferabilities of model parameters calibrated based on sparse and dense rainfall information are very different. They suggested that the lack of spatial information is responsible for the low efficiency of the distributed model

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