{"@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/1390282680265476992.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.3178/hrl.5.11"}},{"identifier":{"@type":"NAID","@value":"130000415070"}}],"dc:title":[{"@language":"en","@value":"Monthly maximum number of consecutive dry days in Japan and its reproducibility by a 5-km-mesh cloud-system resolving regional climate model"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"The geographical distribution of the Monthly maximum number of Consecutive Dry Days (MCDD) over Japan during June–October in 2002–2006 is investigated from observed raingauge data. In June and July, areas with low MCDD (< 6 days) are analyzed associated with the climatological location of the Baiu front. In August, low MCDD [high MCDD (> 10 days)] is found in inland areas [coastal areas of the Seto Inland Sea, southern Kanto, and parts of Hokkaido]. In September and October, low MCDD [high MCDD] is found on the Japan Sea side of Honshu [in Kyushu and coastal areas of the Seto Inland Sea].<br> The reproducibility of the MCDD by a 5-km-mesh cloud-system resolving regional climate model (NHM-5km) is statistically examined in numerical experiments with regional objective analysis data of the Japan Meteorological Agency. NHM-5km performs well in reproducing the features of the local geographical distribution and seasonal march of MCDD, although MCDD is slightly overestimated. The MCDD values averaged for 11 sub-regions of Japan are compared with observations, revealing a good agreement (correlation coefficient, 0.755; root mean square error, 1.49; mean error, 1.10). Moreover, annual variations in MCDD averaged over Japan are well reproduced by the model.<br>"}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420001326232041088","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40713954"},{"@type":"NRID","@value":"1000040713954"},{"@type":"ORCID","@value":"0000-0003-3839-3826"},{"@type":"NRID","@value":"9000001341720"},{"@type":"NRID","@value":"9000020296335"},{"@type":"NRID","@value":"9000283593635"},{"@type":"NRID","@value":"9000257827581"},{"@type":"NRID","@value":"9000415323859"},{"@type":"NRID","@value":"9000257768330"},{"@type":"NRID","@value":"9000021862011"},{"@type":"NRID","@value":"9000020230447"},{"@type":"NRID","@value":"9000018916419"},{"@type":"NRID","@value":"9000402246598"},{"@type":"NRID","@value":"9000257768313"},{"@type":"NRID","@value":"9000257768247"},{"@type":"NRID","@value":"9000370744987"},{"@type":"NRID","@value":"9000018916424"},{"@type":"NRID","@value":"9000370254208"},{"@type":"NRID","@value":"9000020194446"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/masuo"}],"foaf:name":[{"@language":"en","@value":"Nakano Masuo"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Japan Agency for Marine-Earth Science and Technology"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282680265476993","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000021862015"}],"foaf:name":[{"@language":"en","@value":"Kanada Sachie"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Japan Agency for Marine-Earth Science and Technology"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282680265476864","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000021862020"}],"foaf:name":[{"@language":"en","@value":"Kato Teruyuki"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Japan Meteorological Agency"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282680265476992","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000021862026"}],"foaf:name":[{"@language":"en","@value":"Kurihara Kazuo"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research Institute"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"18823416"},{"@type":"LISSN","@value":"18823416"}],"prism:publicationName":[{"@language":"en","@value":"Hydrological Research Letters"},{"@language":"en","@value":"Hydrological Research Letters"}],"dc:publisher":[{"@language":"en","@value":"Japan Society of Hydrology and Water Resources (JSHWR) / Japanese Association of Groundwater Hydrology (JAGH) / Japanese Association of Hydrological Sciences (JAHS) / Japanese Society of Physical Hydrology (JSPH)"},{"@language":"ja","@value":"水文・水資源学会／日本地下水学会／日本水文科学会／陸水物理研究会"}],"prism:publicationDate":"2011","prism:volume":"5","prism:startingPage":"11","prism:endingPage":"15"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","availableAt":"2011","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360292620945975552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seasonal and secular variations of sunshine duration and natural seasons in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621137009024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A One-Dimensional Entraining/Detraining Plume Model and Its Application in Convective Parameterization"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470477092352","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Observed coherent changes in climatic extremes during the second half of the twentieth century"}]},{"@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/1390001205223103104","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Reproducibility of Maximum Daily Precipitation Amount over Japan by a High-resolution Non-hydrostatic Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205289671168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Projection of changes in future weather extremes using super-high-resolution global and regional atmospheric models in the KAKUSHIN Program: Results of preliminary experiments"},{"@value":"Projection of changes in future weather extremes using super-high-resolution global and regional atmospheric models in the KAKUSHIN program"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205290977792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Statistical analysis of simulated direct and indirect precipitation associated with typhoons around Japan using a cloud-system resolving model"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206503268352","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Dynamical Downscaling for Climate Projection with High-Resolution MRI AGCM-RCM"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206504122752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"孤立した対流雲の力学的•微物理学的変化の数値モデリング"},{"@language":"en","@value":"Numerical Modeling of Dynamical and Microphysical Evolution of an Isolated Convective Cloud"},{"@value":"Numerical modeling of dynamical and microphysical evolution of an isolated convective cloud—The 19 July 1981 CCOPE cloud"},{"@value":"Numerical modeling of dynamical and microphysical evolution of an isolated convective cloud: the 19 July 1981 CCOPE cloud"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680198885632","@type":"Article","resourceType":"学術雑誌論文(journal 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