Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/109259
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dc.contributorDepartment of Land Surveying and Geo-Informatics-
dc.contributorResearch Institute for Land and Space-
dc.contributorOtto Poon Charitable Foundation Smart Cities Research Institute-
dc.creatorYou, Jen_US
dc.creatorWang, Sen_US
dc.creatorZhang, Ben_US
dc.creatorRaymond, Cen_US
dc.creatorMatthews, Ten_US
dc.date.accessioned2024-10-03T08:17:30Z-
dc.date.available2024-10-03T08:17:30Z-
dc.identifier.issn0094-8276en_US
dc.identifier.urihttp://hdl.handle.net/10397/109259-
dc.language.isoenen_US
dc.publisherWiley-Blackwell Publishing, Inc.en_US
dc.rights© 2023. The Authors. This is an open access article under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits use, distribution and reproduction in any medium, provided the original work is properly cited.en_US
dc.rightsThe following publication You, J., Wang, S., Zhang, B., Raymond, C., & Matthews, T. (2023). Growing threats from swings between hot and wet extremes in a warmer world. Geophysical Research Letters, 50, e2023GL104075 is available at https://doi.org/10.1029/2023GL104075.en_US
dc.titleGrowing threats from swings between hot and wet extremes in a warmer worlden_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume50en_US
dc.identifier.issue14en_US
dc.identifier.doi10.1029/2023GL104075en_US
dcterms.abstractThe abrupt alternation between hot and wet extremes can lead to more severe societal impacts than isolated extremes. However, despite an understanding of hot and wet extremes separately, their temporally compounding characteristics are not well examined yet. Our study presents a comprehensive assessment of successive heat-pluvial and pluvial-heat events globally. We find that these successive extremes within a week occur every 6–7 years on average within warm seasons during 1956–2015, about 15% more often than would be expected by chance, and that they have a significant increase in frequency of about 22% per decade due to warming. We further investigate the role of vapor pressure deficit (VPD) and find that heat-pluvial (pluvial-heat) events are linked to negative (positive) VPD anomalies. Our results are statistically significant based on moving-blocks bootstrap resampling and field significance tests, highlighting these methods' importance in robustly identifying compound events under autocorrelation and multiple-testing conditions.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationGeophysical research letters, 28 July 2023, v. 50, no. 14, e2023GL104075en_US
dcterms.isPartOfGeophysical research lettersen_US
dcterms.issued2023-07-28-
dc.identifier.scopus2-s2.0-85165449157-
dc.identifier.eissn1944-8007en_US
dc.identifier.artne2023GL104075en_US
dc.description.validate202410 bcch-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Scopus/WOS-
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextHong Kong Polytechnic University; National Aeronautics and Space Administrationen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryCCen_US
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