Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/100715
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dc.contributorDepartment of Land Surveying and Geo-Informaticsen_US
dc.creatorZhu, Jen_US
dc.creatorWang, Sen_US
dc.creatorHuang, Gen_US
dc.date.accessioned2023-08-11T03:12:53Z-
dc.date.available2023-08-11T03:12:53Z-
dc.identifier.issn2169-897Xen_US
dc.identifier.urihttp://hdl.handle.net/10397/100715-
dc.language.isoenen_US
dc.publisherWiley-Blackwellen_US
dc.rights©2019. American Geophysical Union. All Rights Reserved.en_US
dc.titleAssessing climate change impacts on human‐perceived temperature extremes and underlying uncertaintiesen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage3800en_US
dc.identifier.epage3821en_US
dc.identifier.volume124en_US
dc.identifier.issue7en_US
dc.identifier.doi10.1029/2018JD029444en_US
dcterms.abstractIt has been suggested that global warming impacts on human thermal comfort will cause an increase in the heat stress and a decrease in the cold stress in the future. A recent study has shown elevated increases in human-perceived equivalent temperature (HPET) by using a single index for summer and winter seasons (Li et al., 2018, https://doi.org/10.1038/s41558-017-0036-2). However, they have not considered multiple indices with combined effects on deriving HPET, which can result in large uncertainties in assessing climate change impacts on HPET and related extremes. Therefore, we develop a new framework with high-resolution projections and an ensemble of 10 indices to quantify the impacts of climate change on HPET and related perceived extremes as well as to address uncertainties in both empirical indices and emission scenarios over China. Our findings reveal that different combinations of climatic variables can lead to two opposite conclusions for both normal and extreme conditions. For example, by using indices only considering the combined effect of temperature and relative humidity, China is projected to have an elevated increase in the HPET and in the frequency of high-temperature extremes. By taking into account wind speed, the country expects to have the HPET even lower than the surface air temperature and an increase in the frequency of low-temperature extremes. In addition, the resulting range of HPET due to uncertainty in indices is greater than the uncertainty range derived from different emission scenarios for the entire country. Therefore, it is necessary to conduct a comprehensive assessment that explicitly addresses uncertainties in the HPET in order to improve the robustness and reliability of assessing climate change impacts on human-perceived temperature extremes.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationJournal of geophysical research. Atmospheres, 16 Apr. 2019, v. 124, no. 7, p. 3800-3821en_US
dcterms.isPartOfJournal of geophysical research. Atmospheresen_US
dcterms.issued2019-04-16-
dc.identifier.scopus2-s2.0-85063889836-
dc.identifier.eissn2169-8996en_US
dc.description.validate202305 bckwen_US
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberLSGI-0215-
dc.description.fundingSourceOthersen_US
dc.description.fundingTextHong Kong Polytechnic University Start‐up Granten_US
dc.description.pubStatusPublisheden_US
dc.identifier.OPUS28573038-
dc.description.oaCategoryVoR alloweden_US
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