{"@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/1390004222630916736.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.20965/jdr.2020.p0726"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"030656397"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/030656397"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I030656397"}},{"identifier":{"@type":"URI","@value":"https://www.fujipress.jp/main/wp-content/themes/Fujipress/phyosetsu.php?ppno=DSSTR001500060005"}},{"identifier":{"@type":"NAID","@value":"130007921734"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@language":"en","@value":"What Factors Contributed to the Torrential Rainfall of Hurricane Harvey over Texas?"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"<p>In August 2017, Hurricane Harvey brought an unprecedented amount of rainfall and catastrophic flooding to the Houston metropolitan area, as it stalled near the coast of Texas for several days after weakening to a tropical storm intensity. The present study examines the relationship between tropical cyclone rainfall totals over Texas and the track, residence time, rainfall intensity, and rainfall area coverage of past tropical cyclones that approached Texas after 1979. The most significant factor affecting rainfall totals over Texas is whether a tropical cyclone makes landfall on the central coast of Texas and travel inland. Another significant factor is the length of time a tropical cyclone resides near Texas. Rainfall intensity also contributes in part to rainfall totals over Texas, whereas contribution of rainfall area coverage is not significant. The track of a tropical cyclone traveling near Texas is controlled by the steering winds over Texas, while its residence time near Texas is related partly to the meandering of the subtropical jets. Rainfall rate depends on the intensity of tropical cyclone. No significant relationship between rainfall intensity and environmental moisture in the lower atmosphere is found in the present analysis. Furthermore, the extreme rainfall totals over Texas induced by Harvey can be attributed to the combined effect of extreme long-term stalling of Harvey near the central coast of Texas and the higher rainfall rate.</p>"}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420282801197241216","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40414403"},{"@type":"NRID","@value":"1000040414403"},{"@type":"NRID","@value":"9000016856853"},{"@type":"NRID","@value":"9000400192842"},{"@type":"NRID","@value":"9000403034410"},{"@type":"NRID","@value":"9000400192756"},{"@type":"NRID","@value":"9000410311726"},{"@type":"NRID","@value":"9000314383771"},{"@type":"NRID","@value":"9000415314926"},{"@type":"NRID","@value":"9000363500616"},{"@type":"NRID","@value":"9000260207004"},{"@type":"NRID","@value":"9000400194080"},{"@type":"NRID","@value":"9000410278154"},{"@type":"NRID","@value":"9000257766538"},{"@type":"NRID","@value":"9000413527839"},{"@type":"NRID","@value":"9000410194118"},{"@type":"NRID","@value":"9000283101703"},{"@type":"NRID","@value":"9000412002571"},{"@type":"NRID","@value":"9000411562918"},{"@type":"NRID","@value":"9000309172272"},{"@type":"NRID","@value":"9000410655224"},{"@type":"NRID","@value":"9000400194720"},{"@type":"NRID","@value":"9000283892839"},{"@type":"NRID","@value":"9000405693386"},{"@type":"NRID","@value":"9000411073850"},{"@type":"NRID","@value":"9000411811578"},{"@type":"NRID","@value":"9000410320058"},{"@type":"NRID","@value":"9000015590727"},{"@type":"NRID","@value":"9000404665257"},{"@type":"NRID","@value":"9000018936562"},{"@type":"NRID","@value":"9000411512026"},{"@type":"NRID","@value":"9000410320051"},{"@type":"NRID","@value":"9000409182563"},{"@type":"NRID","@value":"9000404949750"},{"@type":"NRID","@value":"9000411807094"},{"@type":"NRID","@value":"9000412195234"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/iizuka.satoshi"}],"foaf:name":[{"@language":"en","@value":"Iizuka Satoshi"}],"jpcoar:affiliationName":[{"@language":"en","@value":"National Research Institute for Earth Science and Disaster Resilience (NIED)"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801197246208","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40414990"},{"@type":"NRID","@value":"1000040414990"},{"@type":"NRID","@value":"9000400192845"},{"@type":"NRID","@value":"9000400192412"},{"@type":"NRID","@value":"9000005521390"},{"@type":"NRID","@value":"9000413472429"},{"@type":"NRID","@value":"9000256316777"},{"@type":"NRID","@value":"9000001960396"},{"@type":"NRID","@value":"9000253615577"},{"@type":"NRID","@value":"9000326645037"},{"@type":"NRID","@value":"9000015297647"},{"@type":"NRID","@value":"9000398382578"},{"@type":"NRID","@value":"9000343338736"},{"@type":"NRID","@value":"9000409205813"},{"@type":"NRID","@value":"9000398283769"},{"@type":"NRID","@value":"9000411580097"},{"@type":"NRID","@value":"9000343338841"},{"@type":"NRID","@value":"9000400194576"},{"@type":"NRID","@value":"9000010319672"},{"@type":"NRID","@value":"9000283417781"},{"@type":"NRID","@value":"9000256316561"},{"@type":"NRID","@value":"9000411116853"},{"@type":"NRID","@value":"9000258500437"},{"@type":"NRID","@value":"9000018878730"},{"@type":"NRID","@value":"9000415395268"},{"@type":"NRID","@value":"9000410911114"},{"@type":"NRID","@value":"9000410311733"},{"@type":"NRID","@value":"9000410311725"},{"@type":"NRID","@value":"9000412003053"},{"@type":"NRID","@value":"9000414560815"},{"@type":"NRID","@value":"9000410320052"},{"@type":"NRID","@value":"9000256316807"},{"@type":"NRID","@value":"9000016715794"},{"@type":"NRID","@value":"9000413740742"},{"@type":"NRID","@value":"9000410911166"},{"@type":"NRID","@value":"9000414560819"},{"@type":"NRID","@value":"9000256316445"},{"@type":"NRID","@value":"9000410484408"},{"@type":"NRID","@value":"9000006013125"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/nsakai0505"}],"foaf:name":[{"@language":"en","@value":"Sakai Naoki"}],"jpcoar:affiliationName":[{"@language":"en","@value":"National Research Institute for Earth Science and Disaster Resilience (NIED)"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"18812473"},{"@type":"EISSN","@value":"18838030"},{"@type":"NDL_BIB_ID","@value":"000008195934"},{"@type":"ISSN","@value":"18812473"},{"@type":"LISSN","@value":"18812473"}],"prism:publicationName":[{"@language":"ja","@value":"Journal of Disaster Research"},{"@language":"en","@value":"Journal of Disaster Research"},{"@language":"en","@value":"J. Disaster Res."}],"dc:publisher":[{"@language":"en","@value":"Fuji Technology Press Ltd."},{"@language":"ja","@value":"富士技術出版株式会社"}],"prism:publicationDate":"2020-10-01","prism:volume":"15","prism:number":"6","prism:startingPage":"726","prism:endingPage":"734"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/030656397"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I030656397"},{"@id":"https://www.fujipress.jp/main/wp-content/themes/Fujipress/phyosetsu.php?ppno=DSSTR001500060005"}],"availableAt":"2020-10-01","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Hurricane%20Harvey","dc:title":"Hurricane Harvey"},{"@id":"https://cir.nii.ac.jp/all?q=rainfall","dc:title":"rainfall"},{"@id":"https://cir.nii.ac.jp/all?q=flood","dc:title":"flood"},{"@id":"https://cir.nii.ac.jp/all?q=Texas","dc:title":"Texas"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781895300608","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H01844"},{"@type":"JGN","@value":"JP16H01844"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16H01844/"}],"notation":[{"@language":"ja","@value":"日本周辺の海面水温場が局所的な豪雨・豪雪の予測可能性に与える影響の定量的評価"},{"@language":"en","@value":"A quantitative assessment of the impacts of sea-surface temperature distribution around Japan on the predictability of regional heavy rainfall/snowfall events"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000781895313152","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H01846"},{"@type":"JGN","@value":"JP16H01846"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16H01846/"}],"notation":[{"@language":"ja","@value":"激甚化する台風・爆弾低気圧起源の災害ハザード予測研究"},{"@language":"en","@value":"Studies on redictability of natural hazards induced by powerful typhoons and explosive cyclones"}]},{"@id":"https://cir.nii.ac.jp/crid/1040285300694327936","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"20H00289"},{"@type":"JGN","@value":"JP20H00289"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-20H00289/"}],"notation":[{"@language":"ja","@value":"メガストームに係る災害ハザードの近未来予測研究"},{"@language":"en","@value":"Studies of near-future prediction of natural hazards induced by megastorms"}]},{"@id":"https://cir.nii.ac.jp/crid/1040848250603444864","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"19H05697"},{"@type":"JGN","@value":"JP19H05697"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-19H05697/"}],"notation":[{"@language":"ja","@value":"急速に温暖化する日本周辺海域での大気海洋相互作用と極端気象"},{"@language":"en","@value":"Impacts of rapid SST rise in western boundary currents and marginal seas on extreme weather events"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360574095685984640","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hurricane stalling along the North American coast and implications for rainfall"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569358995072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hurricane Harvey Links to Ocean Heat Content and Climate Change Adaptation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571308164096","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rainfall asymmetries of tropical cyclones prior to, during, and after making landfall in South China and Southeast United States"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519441477760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Associations between the size of hurricane rain fields at landfall and their surrounding environments"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470802912512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tropical Cyclone Motion and Surrounding Flow Relationships: Searching for Beta Gyres in Omega Dropwindsonde Datasets"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368442718080","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A global slowdown of tropical-cyclone translation speed"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370549183616","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tropical cyclone rainfall area controlled by relative sea surface temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843932819328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Influence of environmental moisture on TRMM‐derived tropical cyclone precipitation over land and ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845436527360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Relationships between tropical cyclone attributes and precipitation totals: considerations of scale"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318949215232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"North American Regional Reanalysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320283782272","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Relationships between tropical cyclones and heavy rainfall in the Carolina region of the USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320546471040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The influence of Arctic amplification on mid-latitude summer circulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793573221760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Doppler Profiler and Radar Observations of Boundary Layer Variability during the Landfall of Tropical Storm Gabrielle"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794095426688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Causes of large projected increases in hurricane precipitation rates with global warming"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268753541760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Assessing objective techniques for gauge‐based analyses of global daily precipitation"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:2008065098"},{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R000000004-I030656397"},{"@type":"CROSSREF","@value":"10.20965/jdr.2020.p0726"},{"@type":"CIA","@value":"130007921734"},{"@type":"KAKEN","@value":"PRODUCT-23737385"},{"@type":"KAKEN","@value":"PRODUCT-23504081"}]}