Articles | Volume 19, issue 2
https://doi.org/10.5194/nhess-19-421-2019
https://doi.org/10.5194/nhess-19-421-2019
Research article
 | 
01 Mar 2019
Research article |  | 01 Mar 2019

Projected intensification of sub-daily and daily rainfall extremes in convection-permitting climate model simulations over North America: implications for future intensity–duration–frequency curves

Alex J. Cannon and Silvia Innocenti

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (11 Jan 2019) by Ricardo Trigo
AR by Alex Cannon on behalf of the Authors (15 Jan 2019)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (16 Jan 2019) by Ricardo Trigo
RR by Anonymous Referee #2 (23 Jan 2019)
RR by Anonymous Referee #3 (01 Feb 2019)
ED: Publish subject to minor revisions (review by editor) (11 Feb 2019) by Ricardo Trigo
AR by Alex Cannon on behalf of the Authors (18 Feb 2019)  Author's response   Manuscript 
ED: Publish as is (19 Feb 2019) by Ricardo Trigo
AR by Alex Cannon on behalf of the Authors (19 Feb 2019)  Manuscript 
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Short summary
Rainfall intensity–duration–frequency (IDF) curves are used as the basis for water resource infrastructure design. Given intensification of the hydrological cycle with global warming, quantitative information on the future extreme rainfall hazard is needed by practitioners. Projected changes in annual maximum rainfall in high-resolution regional climate model simulations result in IDF curves that shift upward and steepen, with greater intensification at short durations and long return periods.
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