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contributor authorSchmith, Torben
date accessioned2017-06-09T16:23:19Z
date available2017-06-09T16:23:19Z
date copyright2008/09/01
date issued2008
identifier issn0894-8755
identifier otherams-66963.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208357
description abstractThe performance of a statistical downscaling model is usually evaluated for its ability to explain a large fraction of predictand variance. In this note, it is shown that although this fraction may be high, the longest time scales, including trends, may not be explained by the model. This implies that the model is nonstationary over the training period of the model, and it questions the basic stationarity assumption of statistical downscaling. This is exemplified by using a simple regression model for downscaling European precipitation and surface temperature where appropriate Monte Carlo?based field significance tests are developed, taking into account the intercorrelation between predictand series. Based on this test, it is concluded that care is needed in selecting predictors to avoid this form of nonstationarity. Even though this is illustrated for a simple regression-type statistical downscaling model, the main conclusions may also be valid for more complicated models.
publisherAmerican Meteorological Society
titleStationarity of Regression Relationships: Application to Empirical Downscaling
typeJournal Paper
journal volume21
journal issue17
journal titleJournal of Climate
identifier doi10.1175/2008JCLI1910.1
journal fristpage4529
journal lastpage4537
treeJournal of Climate:;2008:;volume( 021 ):;issue: 017
contenttypeFulltext


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