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차동현

Cha, Dong-Hyun
High-impact Weather Prediction Lab.
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dc.citation.number 3 -
dc.citation.startPage 034007 -
dc.citation.title ENVIRONMENTAL RESEARCH LETTERS -
dc.citation.volume 18 -
dc.contributor.author Kim, Young-Hyun -
dc.contributor.author Ahn, Joong-Bae -
dc.contributor.author Suh, Myoung-Seok -
dc.contributor.author Cha, Dong-Hyun -
dc.contributor.author Chang, Eun-Chul -
dc.contributor.author Min, Seung-Ki -
dc.contributor.author Byun, Young-Hwa -
dc.contributor.author Kim, Jin-Uk -
dc.date.accessioned 2023-12-21T12:47:58Z -
dc.date.available 2023-12-21T12:47:58Z -
dc.date.created 2023-03-28 -
dc.date.issued 2023-03 -
dc.description.abstract An extreme heatwave, in terms of intensity and duration, is projected to occur at the end of the 21st century (2071-2100) over the whole of East Asia. The projection is calculated using daily maximum temperature data of 25 km horizontal resolution produced by 12 general circulation model-regional climate model chains participating in the CORDEX-East Asia Phase 2 project. An 'extreme' heatwave is defined as one in which the heatwave magnitude (HWM), which is the accumulated daily intensity of a heatwave during the heatwave period, is higher than the 95th percentile of the HWM for the reference period (1981-2005). In historical simulations, heatwaves have occurred mainly from April to June in India, in April and May in Indochina, from June to August in China and Mongolia, and in July and August in the Korean Peninsula and Japan; most heatwaves last three to four days. In India and Indochina, long-lasting and intense heatwaves occur more often than in other regions. In future, heatwave intensity will increase, the average duration of heatwaves will be approximately two to three weeks, and the heatwave season will be lengthened. Therefore, extreme heatwaves will occur more frequently and strongly. Under two representative concentration pathway scenarios (RCP2.6 and RCP8.5) and two shared socioeconomic pathway scenarios (SSP1-2.6 and SSP5-8.5), the proportion of extreme heatwaves to all heatwave events will increase from 5.0% (historical) to 8.0%, 20.8%, 19.3%, and 36.3%, and the HWM of the extreme heatwave will be 1.4, 3.5, 3.0, and 9.0 times stronger, respectively. The main reason for the increase in the HWM of extreme heatwaves is the increased duration rather than the daily intensity of the heatwaves. In East Asia, the temporal and regional disparities of heatwave damage will be much more prominent as extreme heatwaves become stronger and more frequent in these regions and during the periods that are more affected by heatwaves in the present day. -
dc.identifier.bibliographicCitation ENVIRONMENTAL RESEARCH LETTERS, v.18, no.3, pp.034007 -
dc.identifier.doi 10.1088/1748-9326/acb727 -
dc.identifier.issn 1748-9326 -
dc.identifier.scopusid 2-s2.0-85148738172 -
dc.identifier.uri https://scholarworks.unist.ac.kr/handle/201301/62450 -
dc.identifier.wosid 000932169400001 -
dc.language 영어 -
dc.publisher IOP Publishing Ltd -
dc.title Future changes in extreme heatwaves in terms of intensity and duration over the CORDEX-East Asia Phase Two domain using multi-GCM and multi-RCM chains -
dc.type Article -
dc.description.isOpenAccess TRUE -
dc.relation.journalWebOfScienceCategory Environmental Sciences; Meteorology & Atmospheric Sciences -
dc.relation.journalResearchArea Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences -
dc.type.docType Article -
dc.description.journalRegisteredClass scie -
dc.description.journalRegisteredClass scopus -
dc.subject.keywordAuthor heatwaves -
dc.subject.keywordAuthor multi-GCM and multi-RCM chains -
dc.subject.keywordAuthor representative concentration pathways (RCPs) -
dc.subject.keywordAuthor shared socioeconomic pathways (SSPs) -
dc.subject.keywordAuthor CMIP5 -
dc.subject.keywordAuthor CMIP6 -
dc.subject.keywordAuthor CORDEX-east Asia phase 2 -
dc.subject.keywordPlus HEAT WAVES -
dc.subject.keywordPlus CHINA -

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