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11 IMSC Session Program<br />

Constructing ensembles of climate change scenarios based<br />

on statistical downscaling<br />

Tuesday - Parallel Session 5<br />

Radan Huth 1 , Stanislava Kliegrová 2 and Ladislav Metelka 2<br />

1 Institute of Atmospheric Physics, Prague, Czech Republic<br />

2<br />

Czech Hydrometeorological Institute, Regional Office, Hradec Králové, Czech<br />

Republic<br />

Probabilistic framework is now accepted as a standard for formulating future climate<br />

change scenarios based on global climate model (GCM) outputs. However, the use of<br />

statistical downscaling (SDS) as a tool for transferring climate information from large<br />

to local scales introduces additional uncertainties that should be taken into account in<br />

climate change scenarios. The SDS-related uncertainties arise from a considerable<br />

sensitivity of SDS outputs to the selection of the statistical model and its parametres,<br />

as well as of the set of predictors. In this contribution, we aim to assess the SDS<br />

uncertainty alone, that is, for a single emission scenario of a single GCM, thereby<br />

keeping most of the other uncertainty factors constant. We calculate climate change<br />

response for daily temperature at a network of European stations (data coming from<br />

the ECA&D database) by various SDS methods, including linear regression and<br />

neural networks, and for different sets of predictors. We discuss whether the<br />

individual SDS outputs forming the ensemble should be weighted, and which weights<br />

should be used. We argue that the weights of a particular SDS-based scenario should<br />

reflect (i) the ability of the SDS model to reproduce the predictand, (ii) the ability to<br />

reproduce past climatic trends, (iii) the ability of the driving GCM to reproduce the<br />

SDS predictors, (iv) the multiplicity (or mutual dependence) of SDS models, and (v)<br />

the stability of the predictor-predictand relationship. The <strong>final</strong> pdf of anticipated<br />

temperature change is constructed bz the Gaussian kernal algorithm. Examples of the<br />

probabilistic climate change scenarios constructed in this way are shown.<br />

Abstracts 138

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