An empirical evaluation of bias correction methods for palaeoclimate simulations

<p>Even the most sophisticated global climate models are known to have significant biases in the way they simulate the climate system. Correcting model biases is therefore an essential step towards realistic palaeoclimatologies, which are important for many applications such as modelling long-...

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Main Authors: R. Beyer, M. Krapp, A. Manica
Format: Article
Language:English
Published: Copernicus Publications 2020-08-01
Series:Climate of the Past
Online Access:https://cp.copernicus.org/articles/16/1493/2020/cp-16-1493-2020.pdf
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spelling doaj-b6467081c54b4dafbc03b65f1c01cc462020-11-25T03:07:26ZengCopernicus PublicationsClimate of the Past1814-93241814-93322020-08-01161493150810.5194/cp-16-1493-2020An empirical evaluation of bias correction methods for palaeoclimate simulationsR. BeyerM. KrappA. Manica<p>Even the most sophisticated global climate models are known to have significant biases in the way they simulate the climate system. Correcting model biases is therefore an essential step towards realistic palaeoclimatologies, which are important for many applications such as modelling long-term ecological dynamics. Here, we evaluate three widely used bias correction methods – the delta method, generalised additive models (GAMs), and quantile mapping – against a large global dataset of empirical temperature and precipitation records from the present, the mid-Holocene (<span class="inline-formula">∼</span>&thinsp;6000 years BP), the Last Glacial Maximum (<span class="inline-formula">∼21 000</span> years BP), and the last interglacial period (<span class="inline-formula">∼125 000</span> years BP). In most cases, the differences between the bias reductions achieved by the three methods are small. Overall, the delta method performs slightly better, albeit not always to a statistically significant degree, at minimising the median absolute bias between empirical data and debiased simulations for both temperature and precipitation than GAMs and quantile mapping; however, there is considerable spatial and temporal variation in the performance of each of the three methods. Our data also indicate that it could soon be possible to use empirical reconstructions of past climatic conditions not only for the evaluation of bias correction methods but for fitting statistical relationships between empirical and simulated data through time that can inform more effective bias correction methods.</p>https://cp.copernicus.org/articles/16/1493/2020/cp-16-1493-2020.pdf
collection DOAJ
language English
format Article
sources DOAJ
author R. Beyer
M. Krapp
A. Manica
spellingShingle R. Beyer
M. Krapp
A. Manica
An empirical evaluation of bias correction methods for palaeoclimate simulations
Climate of the Past
author_facet R. Beyer
M. Krapp
A. Manica
author_sort R. Beyer
title An empirical evaluation of bias correction methods for palaeoclimate simulations
title_short An empirical evaluation of bias correction methods for palaeoclimate simulations
title_full An empirical evaluation of bias correction methods for palaeoclimate simulations
title_fullStr An empirical evaluation of bias correction methods for palaeoclimate simulations
title_full_unstemmed An empirical evaluation of bias correction methods for palaeoclimate simulations
title_sort empirical evaluation of bias correction methods for palaeoclimate simulations
publisher Copernicus Publications
series Climate of the Past
issn 1814-9324
1814-9332
publishDate 2020-08-01
description <p>Even the most sophisticated global climate models are known to have significant biases in the way they simulate the climate system. Correcting model biases is therefore an essential step towards realistic palaeoclimatologies, which are important for many applications such as modelling long-term ecological dynamics. Here, we evaluate three widely used bias correction methods – the delta method, generalised additive models (GAMs), and quantile mapping – against a large global dataset of empirical temperature and precipitation records from the present, the mid-Holocene (<span class="inline-formula">∼</span>&thinsp;6000 years BP), the Last Glacial Maximum (<span class="inline-formula">∼21 000</span> years BP), and the last interglacial period (<span class="inline-formula">∼125 000</span> years BP). In most cases, the differences between the bias reductions achieved by the three methods are small. Overall, the delta method performs slightly better, albeit not always to a statistically significant degree, at minimising the median absolute bias between empirical data and debiased simulations for both temperature and precipitation than GAMs and quantile mapping; however, there is considerable spatial and temporal variation in the performance of each of the three methods. Our data also indicate that it could soon be possible to use empirical reconstructions of past climatic conditions not only for the evaluation of bias correction methods but for fitting statistical relationships between empirical and simulated data through time that can inform more effective bias correction methods.</p>
url https://cp.copernicus.org/articles/16/1493/2020/cp-16-1493-2020.pdf
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