Projected seasonal changes in large-scale global precipitation and temperature extremes based on the cmip5 ensemble
Projected seasonal changes in large-scale global precipitation and temperature extremes based on the cmip5 ensemble
Over the past decades, significant changes in temperature and precipitation have been observed, including changes in the mean and extremes. It is critical to understand the trends in hydroclimatic extremes and how they may change in the future as they pose substantial threats to society through impacts on agricultural production, economic losses, and human casualties. In this study, we analyzed projected changes in the characteristics, including frequency, seasonal timing, and maximum spatial and temporal extent, as well as severity, of extreme temperature and precipitation events, using the severity-area-duration (SAD) method and based on a suite of 37 climate models archived in phase 5 of the Coupled Model Intercomparison Project (CMIP5). Comparison between the CMIP5 model estimated extreme events and an observation-based dataset [Princeton Global Forcing (PGF)] indicates that climate models have moderate success in reproducing historical statistics of extreme events. Results from the twenty-first-century projections suggest that, on top of the rapid warming indicated by a significant increase in mean temperature, there is an overall wetting trend in the Northern Hemisphere with increasing wet extremes and decreasing dry extremes, whereas the Southern Hemisphere will have more intense wet extremes. The timing of extreme precipitation events will change at different spatial scales, with the largest change occurring in southern Asia. The probability of concurrent dry/hot and wet/hot extremes is projected to increase under both RCP4.5 and RCP8.5 scenarios, whereas little change is detected in the probability of concurrent dry/cold events and only a slight decrease of the joint probability of wet/cold extremes is expected in the future.
5651-5671
Zhan, Wang
cfbebb9a-95c6-4e7d-a3b6-360c3d222db8
He, Xiaogang
5fd2fdc9-b14e-4010-8490-c02950d0a62a
Sheffield, Justin
dd66575b-a4dc-4190-ad95-df2d6aaaaa6b
Wood, Eric F.
8352c1b4-4fd3-42fe-bd23-46619024f1cf
1 July 2020
Zhan, Wang
cfbebb9a-95c6-4e7d-a3b6-360c3d222db8
He, Xiaogang
5fd2fdc9-b14e-4010-8490-c02950d0a62a
Sheffield, Justin
dd66575b-a4dc-4190-ad95-df2d6aaaaa6b
Wood, Eric F.
8352c1b4-4fd3-42fe-bd23-46619024f1cf
Zhan, Wang, He, Xiaogang, Sheffield, Justin and Wood, Eric F.
(2020)
Projected seasonal changes in large-scale global precipitation and temperature extremes based on the cmip5 ensemble.
Journal of Climate, 33 (13), .
(doi:10.1175/JCLI-D-19-0311.1).
Abstract
Over the past decades, significant changes in temperature and precipitation have been observed, including changes in the mean and extremes. It is critical to understand the trends in hydroclimatic extremes and how they may change in the future as they pose substantial threats to society through impacts on agricultural production, economic losses, and human casualties. In this study, we analyzed projected changes in the characteristics, including frequency, seasonal timing, and maximum spatial and temporal extent, as well as severity, of extreme temperature and precipitation events, using the severity-area-duration (SAD) method and based on a suite of 37 climate models archived in phase 5 of the Coupled Model Intercomparison Project (CMIP5). Comparison between the CMIP5 model estimated extreme events and an observation-based dataset [Princeton Global Forcing (PGF)] indicates that climate models have moderate success in reproducing historical statistics of extreme events. Results from the twenty-first-century projections suggest that, on top of the rapid warming indicated by a significant increase in mean temperature, there is an overall wetting trend in the Northern Hemisphere with increasing wet extremes and decreasing dry extremes, whereas the Southern Hemisphere will have more intense wet extremes. The timing of extreme precipitation events will change at different spatial scales, with the largest change occurring in southern Asia. The probability of concurrent dry/hot and wet/hot extremes is projected to increase under both RCP4.5 and RCP8.5 scenarios, whereas little change is detected in the probability of concurrent dry/cold events and only a slight decrease of the joint probability of wet/cold extremes is expected in the future.
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Accepted/In Press date: 6 December 2019
Published date: 1 July 2020
Additional Information:
Funding Information:
Acknowledgments. This research was supported through NOAA Grant number NA14OAR4310218 (Development of a global flood and drought catalogue for the 20th and early 21st centuries based on improved assessment of the global terrestrial water cycle and its extremes).
Publisher Copyright:
© 2020 American Meteorological Society.
Identifiers
Local EPrints ID: 474358
URI: http://eprints.soton.ac.uk/id/eprint/474358
ISSN: 0894-8755
PURE UUID: aa6f5aa1-e9b4-499f-a819-acd9c9c5b8c1
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Date deposited: 20 Feb 2023 18:12
Last modified: 18 Mar 2024 03:33
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Author:
Wang Zhan
Author:
Xiaogang He
Author:
Eric F. Wood
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