Non-stationary large-scale statistics of precipitation extremes in central Europe ...

Extreme precipitation shows non-stationarity, meaning that its distribution can change with time or other large-scale variables. For a classical frequency-intensity analysis this effect is often neglected. Here, we propose a model including the influence of North Atlantic Oscillation, time, surface...

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Main Authors: Fauer, Felix S., Rust, Henning W.
Format: Text
Language:unknown
Published: Freie Universität Berlin 2023
Subjects:
Online Access:https://dx.doi.org/10.17169/refubium-40060
https://refubium.fu-berlin.de/handle/fub188/40339
id ftdatacite:10.17169/refubium-40060
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spelling ftdatacite:10.17169/refubium-40060 2023-12-03T10:26:56+01:00 Non-stationary large-scale statistics of precipitation extremes in central Europe ... Fauer, Felix S. Rust, Henning W. 2023 https://dx.doi.org/10.17169/refubium-40060 https://refubium.fu-berlin.de/handle/fub188/40339 unknown Freie Universität Berlin https://doi.org/10.1007/s00477-023-02515-z https://dx.doi.org/10.1007/s00477-023-02515-z https://doi.org/10.1007/s00477-023-02515-z Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Extreme precipitation Generalized extreme value distribution Maximum likelihood Non-stationary climate Large scale Intensity-duration-frequency 500 Naturwissenschaften und Mathematik550 Geowissenschaften, Geologie551 Geologie, Hydrologie, Meteorologie ScholarlyArticle Text article-journal Wissenschaftlicher Artikel 2023 ftdatacite https://doi.org/10.17169/refubium-4006010.1007/s00477-023-02515-z 2023-11-03T10:39:01Z Extreme precipitation shows non-stationarity, meaning that its distribution can change with time or other large-scale variables. For a classical frequency-intensity analysis this effect is often neglected. Here, we propose a model including the influence of North Atlantic Oscillation, time, surface temperature and a blocking index. The model features flexibility to use annual maxima as well as seasonal maxima to be fitted in a generalized extreme value setting. To further increase the efficiency of data usage, maxima from different accumulation durations are aggregated so that information for extremes on different time scales can be provided. Our model is trained to individual station data with temporal resolutions ranging from one minute to one day across Germany. Models are chosen with a stepwise BIC model selection and verified with a cross-validated quantile skill index. The verification shows that the new model performs better than a reference model without large-scale information. Also, the new model ... Text North Atlantic North Atlantic oscillation DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Extreme precipitation
Generalized extreme value distribution
Maximum likelihood
Non-stationary climate
Large scale
Intensity-duration-frequency
500 Naturwissenschaften und Mathematik550 Geowissenschaften, Geologie551 Geologie, Hydrologie, Meteorologie
spellingShingle Extreme precipitation
Generalized extreme value distribution
Maximum likelihood
Non-stationary climate
Large scale
Intensity-duration-frequency
500 Naturwissenschaften und Mathematik550 Geowissenschaften, Geologie551 Geologie, Hydrologie, Meteorologie
Fauer, Felix S.
Rust, Henning W.
Non-stationary large-scale statistics of precipitation extremes in central Europe ...
topic_facet Extreme precipitation
Generalized extreme value distribution
Maximum likelihood
Non-stationary climate
Large scale
Intensity-duration-frequency
500 Naturwissenschaften und Mathematik550 Geowissenschaften, Geologie551 Geologie, Hydrologie, Meteorologie
description Extreme precipitation shows non-stationarity, meaning that its distribution can change with time or other large-scale variables. For a classical frequency-intensity analysis this effect is often neglected. Here, we propose a model including the influence of North Atlantic Oscillation, time, surface temperature and a blocking index. The model features flexibility to use annual maxima as well as seasonal maxima to be fitted in a generalized extreme value setting. To further increase the efficiency of data usage, maxima from different accumulation durations are aggregated so that information for extremes on different time scales can be provided. Our model is trained to individual station data with temporal resolutions ranging from one minute to one day across Germany. Models are chosen with a stepwise BIC model selection and verified with a cross-validated quantile skill index. The verification shows that the new model performs better than a reference model without large-scale information. Also, the new model ...
format Text
author Fauer, Felix S.
Rust, Henning W.
author_facet Fauer, Felix S.
Rust, Henning W.
author_sort Fauer, Felix S.
title Non-stationary large-scale statistics of precipitation extremes in central Europe ...
title_short Non-stationary large-scale statistics of precipitation extremes in central Europe ...
title_full Non-stationary large-scale statistics of precipitation extremes in central Europe ...
title_fullStr Non-stationary large-scale statistics of precipitation extremes in central Europe ...
title_full_unstemmed Non-stationary large-scale statistics of precipitation extremes in central Europe ...
title_sort non-stationary large-scale statistics of precipitation extremes in central europe ...
publisher Freie Universität Berlin
publishDate 2023
url https://dx.doi.org/10.17169/refubium-40060
https://refubium.fu-berlin.de/handle/fub188/40339
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation https://doi.org/10.1007/s00477-023-02515-z
https://dx.doi.org/10.1007/s00477-023-02515-z
https://doi.org/10.1007/s00477-023-02515-z
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.17169/refubium-4006010.1007/s00477-023-02515-z
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