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dc.contributor.authorLu, C
dc.contributor.authorLott, FC
dc.contributor.authorSun, Y
dc.contributor.authorStott, PA
dc.contributor.authorChristidis, N
dc.date.accessioned2020-07-28T13:29:33Z
dc.date.issued2020-05-26
dc.description.abstractIn China, summer precipitation contributes a major part of the total precipitation amount in a year and has major impacts on society and human life. Whether any changes in summer precipitation are affected by external forcing on the climate system is an important issue. In this study, an optimal fingerprinting method was used to compare the observed changes of total, heavy, moderate, and light precipitation in summer derived from newly homogenized observation data with the simulations from multiple climate models participating in phase 5 of the Coupled Model Intercomparison Project (CMIP5). The results demonstrate that the anthropogenic forcing signal can be detected and separated from the natural forcing signal in the observed increase of seasonal accumulated precipitation amount for heavy precipitation in summer in China and eastern China (EC). The simulated changes in heavy precipitation are generally consistent with observed change in China but are underestimated in EC. When the changes in precipitation of different intensities are considered simultaneously, the human influence on simultaneous changes in moderate and light precipitation can be detected in China and EC in summer. Changes attributable to anthropogenic forcing explain most of the observed regional changes for all categories of summer precipitation, and natural forcing contributes little. In the future, with increasing anthropogenic influence, the attribution-constrained projection suggests that heavy precipitation in summer will increasemore than that from the model raw outputs. Society may therefore face a higher risk of heavy precipitation in the future.en_GB
dc.description.sponsorshipNational Key R&D Program of Chinaen_GB
dc.description.sponsorshipNational Natural Science Foundation of Chinaen_GB
dc.description.sponsorshipUK‐China Research & Innovation Partnership Fund, Newton Funden_GB
dc.description.sponsorshipMet Office Hadley Centre Climate Programmeen_GB
dc.identifier.citationVol. 33 (13), pp. 5357 - 5369en_GB
dc.identifier.doi10.1175/JCLI-D-19-0285.1
dc.identifier.grantnumber2018YFC1507702en_GB
dc.identifier.grantnumber41775082en_GB
dc.identifier.grantnumber41675074en_GB
dc.identifier.urihttp://hdl.handle.net/10871/122203
dc.language.isoenen_GB
dc.publisherAmerican Meteorological Societyen_GB
dc.rights.embargoreasonUnder embargo until 26 November 2020 in compliance with publisher policyen_GB
dc.rights© 2020 American Meteorological Societyen_GB
dc.subjectAtmosphereen_GB
dc.subjectAsiaen_GB
dc.subjectrainfallen_GB
dc.subjectanthropogenic effectsen_GB
dc.subjectclimate changeen_GB
dc.subjectforcingen_GB
dc.titleDetectable anthropogenic influence on changes in summer precipitation in Chinaen_GB
dc.typeArticleen_GB
dc.date.available2020-07-28T13:29:33Z
dc.identifier.issn0894-8755
dc.descriptionThis is the final version. Available from the American Meteorological Society via the DOI in this recorden_GB
dc.identifier.journalJournal of Climateen_GB
dc.rights.urihttp://www.rioxx.net/licenses/all-rights-reserveden_GB
dcterms.dateAccepted2020-03-28
rioxxterms.versionVoRen_GB
rioxxterms.licenseref.startdate2020-05-26
rioxxterms.typeJournal Article/Reviewen_GB
refterms.dateFCD2020-07-28T13:26:02Z
refterms.versionFCDVoR
refterms.dateFOA2020-11-26T00:00:00Z
refterms.panelBen_GB


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