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Preparing local climate change scenarios for the Netherlands using resampling of climate model output

Dados Bibliográficos

ID15550436
AutoresGeert Lenderink (0000-0002-1572-4867, Royal Netherlands Meteorological Institute), Bart van den Hurk (0000-0003-3726-7086, Royal Netherlands Meteorological Institute), B J J M van den Hurk, Albert Klein Tank (0000-0002-6275-2406, Royal Netherlands Meteorological Institute), A M G Klein Tank, Geert Jan van Oldenborgh (0000-0002-6898-9535, Royal Netherlands Meteorological Institute), Erik van Meijgaard (0000-0003-4657-2904, Royal Netherlands Meteorological Institute), Hylke de Vries (0000-0002-6124-1102, Royal Netherlands Meteorological Institute, autor correspondente), J J Beersma (Royal Netherlands Meteorological Institute)
Ano2014
Volume9
Fascículo11
Páginas115008-115008
Data de publicação2014-11-01
Peer ReviewedSim
Open AccessSim
TipoARTICLE
PeriódicoEnvironmental Research Letters (JOURNAL)
Identificadores do periódicoISSN: 1748-9326 • E-ISSN: 1748-9326
EditoraIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/9/11/115008
OpenAlexW2158332412
IdiomaEN
Citações recebidas4
Referências citadas31

A method to prepare a set of four climate scenarios for the Netherlands is presented. These scenarios for climate change in 2050 and 2085 (compared to present-day) are intended for general use in climate change adaptation in the Netherlands. An ensemble of eight simulations with the global model EC-Earth and the regional climate model RACMO2 (run at 12 km resolution) is used. For each scenario time horizon, two target values of the global mean temperature rise are chosen based on the spread in the CMIP5 simulations. Next, the corresponding time periods in the EC-Earth/RACMO2 simulations are selected in which these target values of the global temperature rise are reached. The model output for these periods is then resampled using blocks of 5 yr periods. The rationale of resampling is that natural variations in the EC-Earth/RACMO2 ensemble are used to represent (part of the) uncertainty in the CMIP5 projections. Samples are then chosen with the aim of reconstructing the spread in seasonal temperature and precipitation changes in CMIP5 for the Netherlands. These selected samples form the basis of the scenarios. The resulting four scenarios represent 50–80% of the CMIP5 spread for summer and winter changes in seasonal means as well as a limited number of monthly statistics (warm, cold, wet and dry months). The strong point of the method—also in relation to the previous set of the climate scenarios for the Netherlands issued in 2006—is that it preserves nearly all physical inter-variable consistencies as they exist in the original model output in both space and time

Climate change · Climate model · Climatology · Coupled model intercomparison project · Geography · Meteorology · Precipitation · Resampling · Statistics · Climate change impacts on agriculture · Climate variability and models · Environmental Science · Mathematics · Meteorological Phenomena and Simulations

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    Open Access•Kevin Schaefer, Hugues Lantuit et al.•Environmental Research Letters•2014

  • Regional differentiation in climate change induced drought trends in the Netherlands

    Open Access•Sjoukje Philip, Sjoukje Y Philip et al.•Environmental Research Letters•2020

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    Open Access•Andreas Sterl, A Bakker et al.•Environmental Research Letters•2015

  • The Changing Character of Precipitation

    Kevin E Trenberth, Aiguo Dai et al.•Bulletin of the American…•2003

  • Uncertainty in climate change projections

    Open Access•Clara Deser, Adam Phillips et al.•Climate Dynamics•2012

  • Evaluation of modeled changes in extreme precipitation in Europe and the Rhine basin

    Open Access•Ronald van Haren, Geert Jan van Oldenborgh et al.•Environmental Research Letters•2013

  • On the role of climate scenarios for adaptation planning

    Open Access•Dessai, Suraje Dessai et al.•Global Environmental Change•2005

Obras citantes distintas4
Citações por ano0,33
Intervalo de citações2014 - 2020 (7)
Velocidade de citaçãohistorical
Altamente citadoNão
Tipos de citaçãoNeutras: 4
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