Articles | Volume 22, issue 7
https://doi.org/10.5194/hess-22-3777-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/hess-22-3777-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Future extreme precipitation intensities based on a historic event
Iris Manola
Meteorology and Air Quality, Department of Environmental Sciences,
Wageningen University, Wageningen, the Netherlands
Bart van den Hurk
CORRESPONDING AUTHOR
Institute for Environmental Studies, Vrije Universiteit (VU),
Amsterdam, the Netherlands
The Royal Netherlands Meteorological Institute (KNMI), De Bilt, the
Netherlands
Hans De Moel
Institute for Environmental Studies, Vrije Universiteit (VU),
Amsterdam, the Netherlands
Jeroen C. J. H. Aerts
Institute for Environmental Studies, Vrije Universiteit (VU),
Amsterdam, the Netherlands
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- Observed and Projected Scaling of Daily Extreme Precipitation with Dew Point Temperature at Annual and Seasonal Scales across the Northeast United Sates S. Steinschneider & N. Najibi 10.1175/JHM-D-21-0183.1
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- Modeling the Scaling of Short‐Duration Precipitation Extremes With Temperature H. Van de Vyver et al. 10.1029/2019EA000665
- Linking Total Precipitable Water to Precipitation Extremes Globally S. Kim et al. 10.1029/2021EF002473
- A Temperature-Scaling Approach for Projecting Changes in Short Duration Rainfall Extremes from GCM Data R. Dahm et al. 10.3390/w11020313
- Automating rainfall recording: Ensuring homogeneity when instruments change C. Wasko et al. 10.1016/j.jhydrol.2022.127758
- Estimating design hydrologic extremes in a warming climate: alternatives, uncertainties and the way forward A. Sharma et al. 10.1098/rsta.2019.0623
- Review: Can temperature be used to inform changes to flood extremes with global warming? C. Wasko 10.1098/rsta.2019.0551
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- Uncovering the shortcomings of a weather typing method E. Van Uytven et al. 10.5194/hess-24-2671-2020
- The local dependency of precipitation on historical changes in temperature C. Wasko & R. Nathan 10.1007/s10584-019-02523-5
- Application of the non-stationary peak-over-threshold methods for deriving rainfall extremes from temperature projections O. Lee et al. 10.1016/j.jhydrol.2019.124318
- Incorporating non-stationarity from climate change into rainfall frequency and intensity-duration-frequency (IDF) curves K. Schlef et al. 10.1016/j.jhydrol.2022.128757
- How can event attribution science underpin financial decisions on Loss and Damage? D. Coumou et al. 10.1093/pnasnexus/pgae277
- Observed and Projected Scaling of Daily Extreme Precipitation with Dew Point Temperature at Annual and Seasonal Scales across the Northeast United Sates S. Steinschneider & N. Najibi 10.1175/JHM-D-21-0183.1
- Uncertainty of Rate of Change in Korean Future Rainfall Extremes Using Non-Stationary GEV Model J. Seo et al. 10.3390/atmos12020227
- Pyraingen: A python package for constrained continuous rainfall generation C. Dykman et al. 10.1016/j.envsoft.2024.105984
- A Methodological Approach to Improving Extreme Precipitation Reanalysis Data Using the Clausius-Clapeyron Relationship: A Case Study in a Mediterranean City A. Papadopoulos-Zachos & C. Anagnostopoulou 10.3390/atmos15101195
- Characterizing past and future trend and frequency of extreme rainfall in urban catchments: a case study P. Mzava et al. 10.2166/h2oj.2020.009
- Increasing Trends in Discharge Maxima of a Mediterranean River during Early Autumn G. Varlas et al. 10.3390/w15061022
- Past and projected climate change impacts on rainfall erosivity: Advancing our knowledge for the eastern Mediterranean island of Crete M. Grillakis et al. 10.1016/j.catena.2020.104625
- Analysis of urban rainfall from hourly to seasonal scales using high‐resolution radar observations in the Netherlands I. Manola et al. 10.1002/joc.6241
- Hydrological simple water balance modeling for increasing geographically isolated doline wetland functions and its application to climate change O. Lee et al. 10.1016/j.ecoleng.2020.105812
- Urban flood regulating ecosystem services under climate change: how can Nature-based Solutions contribute? T. Wübbelmann et al. 10.3389/frwa.2023.1081850
- Assessing differences in the response of forest aboveground biomass and composition under climate change in subtropical forest transition zone Z. Wu et al. 10.1016/j.scitotenv.2019.135746
- A universal multifractal approach to assessment of spatiotemporal extreme precipitation over the Loess Plateau of China J. Zhang et al. 10.5194/hess-24-809-2020
- Challenges in the attribution of river flood events P. Scussolini et al. 10.1002/wcc.874
- Updating intensity–duration–frequency curves for urban infrastructure design under a changing environment L. Yan et al. 10.1002/wat2.1519
- Fighting big data and ensemble fatigue in climate change impact studies: Can we turn the ensemble cascade upside down? E. Van Uytven et al. 10.1002/joc.6696
3 citations as recorded by crossref.
- Overview of Observed Clausius-Clapeyron Scaling of Extreme Precipitation in Midlatitudes M. Martinkova & J. Kysely 10.3390/atmos11080786
- Increase in flood risk resulting from climate change in a developed urban watershed – the role of storm temporal patterns S. Hettiarachchi et al. 10.5194/hess-22-2041-2018
- Sensitivity of Australian roof drainage structures to design rainfall variability and climatic change L. Verstraten et al. 10.1016/j.buildenv.2019.106230
Latest update: 24 Dec 2024
Short summary
In a warmer climate, it is expected that precipitation intensities will increase and form a considerable risk of high-impact precipitation extremes. We investigate how observed extreme precipitation events would look like if they took place in a future warmer climate. This study applies three methods to transform a historic extreme precipitation event in the Netherlands to a similar event in a future warmer climate, thus compiling a
future weatherscenario.
In a warmer climate, it is expected that precipitation intensities will increase and form a...