Using UNSEEN trends to detect decadal changes in 100-year precipitation extremes

Sample sizes of observed climate extremes are typically too small to reliably constrain return period estimates when there is non-stationary behaviour. To increase the historical record 100-fold, we apply the UNprecedented Simulated Extreme ENsemble (UNSEEN) approach, by pooling ensemble members and...

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Main Authors: Timo Kelder, M. Müller, L.J. Slater, Tim Marjoribanks, Robert Wilby, C. Prudhomme, P. Bohlinger, L. Ferranti, T. Nipen
Format: Other Non-Article Part of Journal/Newspaper
Language:unknown
Published: 2020
Subjects:
Online Access:https://figshare.com/articles/journal_contribution/Using_UNSEEN_trends_to_detect_decadal_changes_in_100-year_precipitation_extremes/13139330
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spelling ftloughboroughun:oai:figshare.com:article/13139330 2023-05-15T18:29:48+02:00 Using UNSEEN trends to detect decadal changes in 100-year precipitation extremes Timo Kelder M. Müller L.J. Slater Tim Marjoribanks Robert Wilby C. Prudhomme P. Bohlinger L. Ferranti T. Nipen 2020-11-27T00:00:00Z https://figshare.com/articles/journal_contribution/Using_UNSEEN_trends_to_detect_decadal_changes_in_100-year_precipitation_extremes/13139330 unknown 2134/13139330.v1 https://figshare.com/articles/journal_contribution/Using_UNSEEN_trends_to_detect_decadal_changes_in_100-year_precipitation_extremes/13139330 CC BY 4.0 CC-BY Uncategorized Atmospheric science Climate change Environmental impact Hydrology Text Journal contribution 2020 ftloughboroughun 2022-01-01T19:15:59Z Sample sizes of observed climate extremes are typically too small to reliably constrain return period estimates when there is non-stationary behaviour. To increase the historical record 100-fold, we apply the UNprecedented Simulated Extreme ENsemble (UNSEEN) approach, by pooling ensemble members and lead times from the ECMWF seasonal prediction system SEAS5. We fit the GEV distribution to the UNSEEN ensemble with a time covariate to facilitate detection of changes in 100-year precipitation values over a period of 35 years (1981–2015). Applying UNSEEN trends to 3-day precipitation extremes over Western Norway substantially reduces uncertainties compared to estimates based on the observed record and returns no significant linear trend over time. For Svalbard, UNSEEN trends suggests there is a significant rise in precipitation extremes, such that the 100-year event estimated in 1981 occurs with a return period of around 40 years in 2015. We propose a suite of methods to evaluate UNSEEN and highlight paths for further developing UNSEEN trends to investigate non-stationarities in climate extremes. Other Non-Article Part of Journal/Newspaper Svalbard Loughborough University: Figshare Norway Svalbard
institution Open Polar
collection Loughborough University: Figshare
op_collection_id ftloughboroughun
language unknown
topic Uncategorized
Atmospheric science
Climate change
Environmental impact
Hydrology
spellingShingle Uncategorized
Atmospheric science
Climate change
Environmental impact
Hydrology
Timo Kelder
M. Müller
L.J. Slater
Tim Marjoribanks
Robert Wilby
C. Prudhomme
P. Bohlinger
L. Ferranti
T. Nipen
Using UNSEEN trends to detect decadal changes in 100-year precipitation extremes
topic_facet Uncategorized
Atmospheric science
Climate change
Environmental impact
Hydrology
description Sample sizes of observed climate extremes are typically too small to reliably constrain return period estimates when there is non-stationary behaviour. To increase the historical record 100-fold, we apply the UNprecedented Simulated Extreme ENsemble (UNSEEN) approach, by pooling ensemble members and lead times from the ECMWF seasonal prediction system SEAS5. We fit the GEV distribution to the UNSEEN ensemble with a time covariate to facilitate detection of changes in 100-year precipitation values over a period of 35 years (1981–2015). Applying UNSEEN trends to 3-day precipitation extremes over Western Norway substantially reduces uncertainties compared to estimates based on the observed record and returns no significant linear trend over time. For Svalbard, UNSEEN trends suggests there is a significant rise in precipitation extremes, such that the 100-year event estimated in 1981 occurs with a return period of around 40 years in 2015. We propose a suite of methods to evaluate UNSEEN and highlight paths for further developing UNSEEN trends to investigate non-stationarities in climate extremes.
format Other Non-Article Part of Journal/Newspaper
author Timo Kelder
M. Müller
L.J. Slater
Tim Marjoribanks
Robert Wilby
C. Prudhomme
P. Bohlinger
L. Ferranti
T. Nipen
author_facet Timo Kelder
M. Müller
L.J. Slater
Tim Marjoribanks
Robert Wilby
C. Prudhomme
P. Bohlinger
L. Ferranti
T. Nipen
author_sort Timo Kelder
title Using UNSEEN trends to detect decadal changes in 100-year precipitation extremes
title_short Using UNSEEN trends to detect decadal changes in 100-year precipitation extremes
title_full Using UNSEEN trends to detect decadal changes in 100-year precipitation extremes
title_fullStr Using UNSEEN trends to detect decadal changes in 100-year precipitation extremes
title_full_unstemmed Using UNSEEN trends to detect decadal changes in 100-year precipitation extremes
title_sort using unseen trends to detect decadal changes in 100-year precipitation extremes
publishDate 2020
url https://figshare.com/articles/journal_contribution/Using_UNSEEN_trends_to_detect_decadal_changes_in_100-year_precipitation_extremes/13139330
geographic Norway
Svalbard
geographic_facet Norway
Svalbard
genre Svalbard
genre_facet Svalbard
op_relation 2134/13139330.v1
https://figshare.com/articles/journal_contribution/Using_UNSEEN_trends_to_detect_decadal_changes_in_100-year_precipitation_extremes/13139330
op_rights CC BY 4.0
op_rightsnorm CC-BY
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