Errors in climate model daily precipitation and temperature output: time invariance and implications for bias correction

When correcting for biases in general circulation model (GCM) output, for example when statistically downscaling for regional and local impacts studies, a common assumption is that the GCM biases can be characterized by comparing model simulations and observations for a historical period. We demonst...

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Main Authors: E. P. Maurer, T. Das, D. R. Cayan
Format: Article
Language:English
Published: Copernicus Publications 2013-06-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/17/2147/2013/hess-17-2147-2013.pdf
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spelling doaj-d72e7ea3d4df443386b11898e1a606362020-11-24T20:53:11ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382013-06-011762147215910.5194/hess-17-2147-2013Errors in climate model daily precipitation and temperature output: time invariance and implications for bias correctionE. P. MaurerT. DasD. R. CayanWhen correcting for biases in general circulation model (GCM) output, for example when statistically downscaling for regional and local impacts studies, a common assumption is that the GCM biases can be characterized by comparing model simulations and observations for a historical period. We demonstrate some complications in this assumption, with GCM biases varying between mean and extreme values and for different sets of historical years. Daily precipitation and maximum and minimum temperature from late 20th century simulations by four GCMs over the United States were compared to gridded observations. Using random years from the historical record we select a "base" set and a 10 yr independent "projected" set. We compare differences in biases between these sets at median and extreme percentiles. On average a base set with as few as 4 randomly-selected years is often adequate to characterize the biases in daily GCM precipitation and temperature, at both median and extreme values; 12 yr provided higher confidence that bias correction would be successful. This suggests that some of the GCM bias is time invariant. When characterizing bias with a set of consecutive years, the set must be long enough to accommodate regional low frequency variability, since the bias also exhibits this variability. Newer climate models included in the Intergovernmental Panel on Climate Change fifth assessment will allow extending this study for a longer observational period and to finer scales.http://www.hydrol-earth-syst-sci.net/17/2147/2013/hess-17-2147-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. P. Maurer
T. Das
D. R. Cayan
spellingShingle E. P. Maurer
T. Das
D. R. Cayan
Errors in climate model daily precipitation and temperature output: time invariance and implications for bias correction
Hydrology and Earth System Sciences
author_facet E. P. Maurer
T. Das
D. R. Cayan
author_sort E. P. Maurer
title Errors in climate model daily precipitation and temperature output: time invariance and implications for bias correction
title_short Errors in climate model daily precipitation and temperature output: time invariance and implications for bias correction
title_full Errors in climate model daily precipitation and temperature output: time invariance and implications for bias correction
title_fullStr Errors in climate model daily precipitation and temperature output: time invariance and implications for bias correction
title_full_unstemmed Errors in climate model daily precipitation and temperature output: time invariance and implications for bias correction
title_sort errors in climate model daily precipitation and temperature output: time invariance and implications for bias correction
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2013-06-01
description When correcting for biases in general circulation model (GCM) output, for example when statistically downscaling for regional and local impacts studies, a common assumption is that the GCM biases can be characterized by comparing model simulations and observations for a historical period. We demonstrate some complications in this assumption, with GCM biases varying between mean and extreme values and for different sets of historical years. Daily precipitation and maximum and minimum temperature from late 20th century simulations by four GCMs over the United States were compared to gridded observations. Using random years from the historical record we select a "base" set and a 10 yr independent "projected" set. We compare differences in biases between these sets at median and extreme percentiles. On average a base set with as few as 4 randomly-selected years is often adequate to characterize the biases in daily GCM precipitation and temperature, at both median and extreme values; 12 yr provided higher confidence that bias correction would be successful. This suggests that some of the GCM bias is time invariant. When characterizing bias with a set of consecutive years, the set must be long enough to accommodate regional low frequency variability, since the bias also exhibits this variability. Newer climate models included in the Intergovernmental Panel on Climate Change fifth assessment will allow extending this study for a longer observational period and to finer scales.
url http://www.hydrol-earth-syst-sci.net/17/2147/2013/hess-17-2147-2013.pdf
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