Abstract

Abstract. This study presents a novel bias correction scheme for regional climate model (RCM) precipitation ensembles. A primary advantage of using model ensembles for climate change impact studies is that the uncertainties associated with the systematic error can be quantified through the ensemble spread. Currently, however, most of the conventional bias correction methods adjust all the ensemble members to one reference observation. As a result, the ensemble spread is degraded during bias correction. Since the observation is only one case of many possible realizations due to the climate natural variability, a successful bias correction scheme should preserve the ensemble spread within the bounds of its natural variability (i.e. sampling uncertainty). To demonstrate a new bias correction scheme conforming to RCM precipitation ensembles, an application to the Thorverton catchment in the south-west of England is presented. For the ensemble, 11 members from the Hadley Centre Regional Climate Model (HadRM3-PPE) data are used and monthly bias correction has been done for the baseline time period from 1961 to 1990. In the typical conventional method, monthly mean precipitation of each of the ensemble members is nearly identical to the observation, i.e. the ensemble spread is removed. In contrast, the proposed method corrects the bias while maintaining the ensemble spread within the natural variability of the observations.

Highlights

  • The growing evidence of global climate change is clear in the past century (Stocker, 2013)

  • The ensemble spread should be maintained to a certain degree after bias correction, which is compatible with the natural variability of the observation

  • The major contribution of this study is the proposal of a new bias correction scheme, which reasonably preserves the spread of the regional climate model (RCM) ensemble members

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Summary

Introduction

The growing evidence of global climate change is clear in the past century (Stocker, 2013). Interest in the impacts of climate change is increasing from water resources managers in the context of the hydrological cycle and water resources (Bates et al, 2008; Arnell et al, 2001). Global climate models (GCMs) are usually used for the projection of future climate and the accuracy of GCMs has been enhanced in simulating large-scale global climate. GCMs have difficulties in providing reliable climate data at local scales due to their coarse resolutions (100–250 km) (Maraun et al, 2010). For regional impact studies, regional climate models (RCMs) have been widely used which are compatible with the catchment scales (25–50 km)

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