Robustness of Ensemble Climate Projections Analyzed with Climate Signal Maps: Seasonal and Extreme Precipitation for Germany

Climate signal maps can be used to identify regions where robust climate changes can be derived from an ensemble of climate change simulations. Here, robustness is defined as a combination of model agreement and the significance of the individual model projections. Climate signal maps do not show al...

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Main Authors: Susanne Pfeifer, Katharina Bülow, Andreas Gobiet, Andreas Hänsler, Manfred Mudelsee, Juliane Otto, Diana Rechid, Claas Teichmann, Daniela Jacob
Format: Article
Language:English
Published: MDPI AG 2015-05-01
Series:Atmosphere
Subjects:
Online Access:http://www.mdpi.com/2073-4433/6/5/677
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spelling doaj-3df8864d6cac495980e4bdfb0fdb57b92020-11-24T22:50:13ZengMDPI AGAtmosphere2073-44332015-05-016567769810.3390/atmos6050677atmos6050677Robustness of Ensemble Climate Projections Analyzed with Climate Signal Maps: Seasonal and Extreme Precipitation for GermanySusanne Pfeifer0Katharina Bülow1Andreas Gobiet2Andreas Hänsler3Manfred Mudelsee4Juliane Otto5Diana Rechid6Claas Teichmann7Daniela Jacob8Helmholtz-Zentrum Geesthacht, Climate Service Center 2.0, Fischertwiete 1, 20095 Hamburg, GermanyHelmholtz-Zentrum Geesthacht, Climate Service Center 2.0, Fischertwiete 1, 20095 Hamburg, GermanyWegener Center for Climate and Global Change, University of Graz, 8010 Graz, AustriaHelmholtz-Zentrum Geesthacht, Climate Service Center 2.0, Fischertwiete 1, 20095 Hamburg, GermanyClimate Risk Analysis, 37581 Bad Gandersheim, GermanyHelmholtz-Zentrum Geesthacht, Climate Service Center 2.0, Fischertwiete 1, 20095 Hamburg, GermanyHelmholtz-Zentrum Geesthacht, Climate Service Center 2.0, Fischertwiete 1, 20095 Hamburg, GermanyHelmholtz-Zentrum Geesthacht, Climate Service Center 2.0, Fischertwiete 1, 20095 Hamburg, GermanyHelmholtz-Zentrum Geesthacht, Climate Service Center 2.0, Fischertwiete 1, 20095 Hamburg, GermanyClimate signal maps can be used to identify regions where robust climate changes can be derived from an ensemble of climate change simulations. Here, robustness is defined as a combination of model agreement and the significance of the individual model projections. Climate signal maps do not show all information available from the model ensemble, but give a condensed view in order to be useful for non-climate scientists who have to assess climate change impact during the course of their work. Three different ensembles of regional climate projections have been analyzed regarding changes of seasonal mean and extreme precipitation (defined as the number of days exceeding the 95th percentile threshold of daily precipitation) for Germany, using climate signal maps. Although the models used and the scenario assumptions differ for the three ensembles (representative concentration pathway (RCP) 4.5 vs. RCP8.5 vs. A1B), some similarities in the projections of future seasonal and extreme precipitation can be seen. For the winter season, both mean and extreme precipitation are projected to increase. The strength, robustness and regional pattern of this increase, however, depends on the ensemble. For summer, a robust decrease of mean precipitation can be detected only for small regions in southwestern Germany and only from two of the three ensembles, whereas none of them projects a robust increase of summer extreme precipitation.http://www.mdpi.com/2073-4433/6/5/677regional climate modelsclimate changerobustnessprecipitationGermanyEURO-CORDEXENSEMBLES
collection DOAJ
language English
format Article
sources DOAJ
author Susanne Pfeifer
Katharina Bülow
Andreas Gobiet
Andreas Hänsler
Manfred Mudelsee
Juliane Otto
Diana Rechid
Claas Teichmann
Daniela Jacob
spellingShingle Susanne Pfeifer
Katharina Bülow
Andreas Gobiet
Andreas Hänsler
Manfred Mudelsee
Juliane Otto
Diana Rechid
Claas Teichmann
Daniela Jacob
Robustness of Ensemble Climate Projections Analyzed with Climate Signal Maps: Seasonal and Extreme Precipitation for Germany
Atmosphere
regional climate models
climate change
robustness
precipitation
Germany
EURO-CORDEX
ENSEMBLES
author_facet Susanne Pfeifer
Katharina Bülow
Andreas Gobiet
Andreas Hänsler
Manfred Mudelsee
Juliane Otto
Diana Rechid
Claas Teichmann
Daniela Jacob
author_sort Susanne Pfeifer
title Robustness of Ensemble Climate Projections Analyzed with Climate Signal Maps: Seasonal and Extreme Precipitation for Germany
title_short Robustness of Ensemble Climate Projections Analyzed with Climate Signal Maps: Seasonal and Extreme Precipitation for Germany
title_full Robustness of Ensemble Climate Projections Analyzed with Climate Signal Maps: Seasonal and Extreme Precipitation for Germany
title_fullStr Robustness of Ensemble Climate Projections Analyzed with Climate Signal Maps: Seasonal and Extreme Precipitation for Germany
title_full_unstemmed Robustness of Ensemble Climate Projections Analyzed with Climate Signal Maps: Seasonal and Extreme Precipitation for Germany
title_sort robustness of ensemble climate projections analyzed with climate signal maps: seasonal and extreme precipitation for germany
publisher MDPI AG
series Atmosphere
issn 2073-4433
publishDate 2015-05-01
description Climate signal maps can be used to identify regions where robust climate changes can be derived from an ensemble of climate change simulations. Here, robustness is defined as a combination of model agreement and the significance of the individual model projections. Climate signal maps do not show all information available from the model ensemble, but give a condensed view in order to be useful for non-climate scientists who have to assess climate change impact during the course of their work. Three different ensembles of regional climate projections have been analyzed regarding changes of seasonal mean and extreme precipitation (defined as the number of days exceeding the 95th percentile threshold of daily precipitation) for Germany, using climate signal maps. Although the models used and the scenario assumptions differ for the three ensembles (representative concentration pathway (RCP) 4.5 vs. RCP8.5 vs. A1B), some similarities in the projections of future seasonal and extreme precipitation can be seen. For the winter season, both mean and extreme precipitation are projected to increase. The strength, robustness and regional pattern of this increase, however, depends on the ensemble. For summer, a robust decrease of mean precipitation can be detected only for small regions in southwestern Germany and only from two of the three ensembles, whereas none of them projects a robust increase of summer extreme precipitation.
topic regional climate models
climate change
robustness
precipitation
Germany
EURO-CORDEX
ENSEMBLES
url http://www.mdpi.com/2073-4433/6/5/677
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