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Lookup NU author(s): Dr Renaud Barbero, Professor Hayley Fowler, Dr Stephen Blenkinsop
This is the final published version of an article that has been published in its final definitive form by Blackwell Publishing Ltd, 2017.
For re-use rights please refer to the publisher's terms and conditions.
©2017. American Geophysical Union. All Rights Reserved. Although it has been documented that daily precipitation extremes are increasing worldwide, faster increases may be expected for subdaily extremes. Here after a careful quality control procedure, we compared trends in hourly and daily precipitation extremes using a large network of stations across the United States (U.S.) within the 1950–2011 period. A greater number of significant increasing trends in annual and seasonal maximum precipitation were detected from daily extremes, with the primary exception of wintertime. Our results also show that the mean percentage change in annual maximum daily precipitation across the U.S. per global warming degree is ~6.9% °C−1 (in agreement with the Clausius-Clapeyron rate) while lower sensitivities were observed for hourly extremes, suggesting that changes in the magnitude of subdaily extremes in response to global warming emerge more slowly than those for daily extremes in the climate record.
Author(s): Barbero R, Fowler HJ, Lenderink G, Blenkinsop S
Publication type: Article
Publication status: Published
Journal: Geophysical Research Letters
Year: 2017
Volume: 44
Issue: 2
Pages: 974-983
Print publication date: 28/01/2017
Online publication date: 04/01/2017
Acceptance date: 01/01/2017
Date deposited: 21/06/2017
ISSN (print): 0094-8276
ISSN (electronic): 1944-8007
Publisher: Blackwell Publishing Ltd
URL: https://doi.org/10.1002/2016GL071917
DOI: 10.1002/2016GL071917
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