{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1390282680200714880.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2151/sola.2007-005"}},{"identifier":{"@type":"URI","@value":"http://www.jstage.jst.go.jp/article/sola/3/0/3_0_17/_pdf"}},{"identifier":{"@type":"NAID","@value":"130004448423"}},{"identifier":{"@type":"NAID","@value":"30025515176"}}],"dc:title":[{"@language":"en","@value":"Characteristics of Extreme Climate Sequences over Korea Using a Regional Climate Change Scenario"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"We investigate the characteristics and potential future change of extreme climate phenomena based on daily statistical properties. To assess the fine-scale climate change projection over Korea, an ECHO-G B2 scenario simulation has been dynamically downscaled by using the RegCM3 nesting system. Two sets of multi-decadal simulations are performed for the present day (1971-2000) and future climate (2021-2050). We analyze four categories of weather spells in terms of the sequences of dry/wet and frost/hot days from the nested domain simulation of 20 km grid spacing. In the validation of the reference scenario, the model shows a reasonable performance of reproducing both observed climatological and distinct characteristics of each spell. Regarding the projected extreme climate events, the results indicate not only a significant change in frequency and intensity, but also substantial change in the fine scale detail of the regional distribution of temperature-based as well as precipitation-based extreme events. A substantial increase of hot spells is found along with increasing of maximum temperature. Longer-period frost spells are projected to decrease, whereas relatively short-period frost spells are likely to increase due to breaks of long spells by greenhouse warming. Wet spells of long periods tend to be more frequent, showing a distinct variation across regions."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410282680200714880","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000257827453"}],"foaf:name":[{"@language":"en","@value":"Kwon Won-Tae"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Climate Research Lab., METRI, KMA"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282680200714881","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000257827452"}],"foaf:name":[{"@language":"en","@value":"Eun-Soon Im"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Climate Research Lab., METRI, KMA"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"13496476"}],"prism:publicationName":[{"@language":"en","@value":"SOLA"},{"@language":"en","@value":"SOLA"}],"dc:publisher":[{"@language":"en","@value":"Meteorological Society of Japan"},{"@language":"ja","@value":"公益社団法人 日本気象学会"}],"prism:publicationDate":"2007","prism:volume":"3","prism:startingPage":"17","prism:endingPage":"20"},"reviewed":"false","url":[{"@id":"http://www.jstage.jst.go.jp/article/sola/3/0/3_0_17/_pdf"}],"availableAt":"2007","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011144694842240","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Downscaling of Daily Rainfall Occurrence over Northeast Brazil Using a Hidden Markov Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619533572352","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Multi-decadal scenario simulation over Korea using a one-way double-nested regional climate model system. Part 2: future climate projection (2021–2050)"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518551714304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Response of global warming on regional climate change over Korea: An experiment with the MM5 model"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519120168576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Pacific Northwest Climate Sensitivity Simulated by a Regional Climate Model Driven by a GCM. Part I: Control Simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519227290112","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Projected changes in mean and extreme precipitation over the Mediterranean region from a high resolution double nested RCM simulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419123500672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Role of an Advanced Land Model in Seasonal Dynamical Downscaling for Crop Model Application"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894949841152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Change of extreme events of temperature and precipitation over Korea using regional projection of future climate change"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895317690368","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Multi-decadal scenario simulation over Korea using a one-way double-nested regional climate model system. Part 1: recent climate simulation (1971–2000)"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368930012288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seasonal Predictions Using a Regional Spectral Model Embedded within a Coupled Ocean–Atmosphere Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370432896768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Response of the East Asian summer monsoon to doubled atmospheric CO2: Coupled climate model simulations and projections under IPCC AR4"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319359133056","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the capability of RegCM to capture extremes in long term regional climate simulation – comparison with the observations for Czech Republic"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320185261824","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the role of resolution and topography in the simulation of East Asia precipitation"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951796214799232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Internal variability in a 1000-yr control simulation with the coupled climate model ECHO-G - I. Near-surface temperature, precipitation and mean sea level pressure"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270055936128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Present climate simulation over Korea with a regional climate model using a one-way double-nested system"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205221449856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Changes in Extremes Indices over Japan Due to Global Warming Projected by a Global 20-km-mesh Atmospheric Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206505267072","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Projected Change in Mean and Extreme Climate over Korea from a Double-Nested Regional Climate Model Simulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680198079104","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Projected Changes in Precipitation Characteristics around Japan under the Global Warming"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681477659392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Regional Climate Simulation for Korea using Dynamic Downscaling and Statistical Adjustment"},{"@value":"Regional Climate Simulation for Korea using Dynamic Downscaling and Statistical Adjustment(<Special Edition>Regional Climate Modeling for Monsoon System)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681480334336","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"On the Elevation Dependency of Present-day Climate and Future Change over Korea from a High Resolution Regional Climate Simulation"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:0028951668"},{"@type":"CROSSREF","@value":"10.2151/sola.2007-005"},{"@type":"CIA","@value":"130004448423"},{"@type":"CIA","@value":"30025515176"},{"@type":"CROSSREF","@value":"10.2151/jmsj.2011-106_references_DOI_FqUtIOhDy7unbgXl1kt2loOxozI"},{"@type":"CROSSREF","@value":"10.2151/jmsj.85.717_references_DOI_FqUtIOhDy7unbgXl1kt2loOxozI"}]}