Temperature fluctuations in a changing climate: an ensemble-based experimental approach

Abstract There is an ongoing debate in the literature about whether the present global warming is increasing local and global temperature variability. The central methodological issues of this debate relate to the proper treatment of normalised temperature anomalies and trends in the studied time se...

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Main Authors: Miklós Vincze, Ion Dan Borcia, Uwe Harlander
Format: Article
Language:English
Published: Nature Publishing Group 2017-03-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-017-00319-0
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spelling doaj-e4d2540917804ac484dfe6df57a76b882020-12-08T00:19:37ZengNature Publishing GroupScientific Reports2045-23222017-03-01711910.1038/s41598-017-00319-0Temperature fluctuations in a changing climate: an ensemble-based experimental approachMiklós Vincze0Ion Dan Borcia1Uwe Harlander2Eötvös University, von Kármán Laboratory for Environmental FlowsBrandenburg University of Technology Cottbus-Senftenberg, Department of Aerodynamics and Fluid MechanicsBrandenburg University of Technology Cottbus-Senftenberg, Department of Aerodynamics and Fluid MechanicsAbstract There is an ongoing debate in the literature about whether the present global warming is increasing local and global temperature variability. The central methodological issues of this debate relate to the proper treatment of normalised temperature anomalies and trends in the studied time series which may be difficult to separate from time-evolving fluctuations. Some argue that temperature variability is indeed increasing globally, whereas others conclude it is decreasing or remains practically unchanged. Meanwhile, a consensus appears to emerge that local variability in certain regions (e.g. Western Europe and North America) has indeed been increasing in the past 40 years. Here we investigate the nature of connections between external forcing and climate variability conceptually by using a laboratory-scale minimal model of mid-latitude atmospheric thermal convection subject to continuously decreasing ‘equator-to-pole’ temperature contrast ΔT, mimicking climate change. The analysis of temperature records from an ensemble of experimental runs (‘realisations’) all driven by identical time-dependent external forcing reveals that the collective variability of the ensemble and that of individual realisations may be markedly different – a property to be considered when interpreting climate records.https://doi.org/10.1038/s41598-017-00319-0
collection DOAJ
language English
format Article
sources DOAJ
author Miklós Vincze
Ion Dan Borcia
Uwe Harlander
spellingShingle Miklós Vincze
Ion Dan Borcia
Uwe Harlander
Temperature fluctuations in a changing climate: an ensemble-based experimental approach
Scientific Reports
author_facet Miklós Vincze
Ion Dan Borcia
Uwe Harlander
author_sort Miklós Vincze
title Temperature fluctuations in a changing climate: an ensemble-based experimental approach
title_short Temperature fluctuations in a changing climate: an ensemble-based experimental approach
title_full Temperature fluctuations in a changing climate: an ensemble-based experimental approach
title_fullStr Temperature fluctuations in a changing climate: an ensemble-based experimental approach
title_full_unstemmed Temperature fluctuations in a changing climate: an ensemble-based experimental approach
title_sort temperature fluctuations in a changing climate: an ensemble-based experimental approach
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2017-03-01
description Abstract There is an ongoing debate in the literature about whether the present global warming is increasing local and global temperature variability. The central methodological issues of this debate relate to the proper treatment of normalised temperature anomalies and trends in the studied time series which may be difficult to separate from time-evolving fluctuations. Some argue that temperature variability is indeed increasing globally, whereas others conclude it is decreasing or remains practically unchanged. Meanwhile, a consensus appears to emerge that local variability in certain regions (e.g. Western Europe and North America) has indeed been increasing in the past 40 years. Here we investigate the nature of connections between external forcing and climate variability conceptually by using a laboratory-scale minimal model of mid-latitude atmospheric thermal convection subject to continuously decreasing ‘equator-to-pole’ temperature contrast ΔT, mimicking climate change. The analysis of temperature records from an ensemble of experimental runs (‘realisations’) all driven by identical time-dependent external forcing reveals that the collective variability of the ensemble and that of individual realisations may be markedly different – a property to be considered when interpreting climate records.
url https://doi.org/10.1038/s41598-017-00319-0
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AT iondanborcia temperaturefluctuationsinachangingclimateanensemblebasedexperimentalapproach
AT uweharlander temperaturefluctuationsinachangingclimateanensemblebasedexperimentalapproach
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