{"@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/1390282681481522816.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2151/jmsj1965.72.5_627"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"3902017"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/3902017"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I3902017"}},{"identifier":{"@type":"URI","@value":"https://dl.ndl.go.jp/pid/10611029"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"10611029"}},{"identifier":{"@type":"NAID","@value":"110001807362"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/digimeta/10611029"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/jmsj1965/72/5/72_5_627/_pdf"}},{"identifier":{"@type":"URI","@value":"http://dl.ndl.go.jp/info:ndljp/pid/10611029"}},{"identifier":{"@type":"NAID","@value":"130007345495"}}],"dc:title":[{"@language":"ja","@value":"熱帯西部太平洋における対流活動の日変化"},{"@language":"en","@value":"Diurnal Variation of Convective Activity over the Tropical Western Pacific"},{"@value":"熱帯西部太平洋における対流活動の日変化〔英文〕"},{"@language":"ja-Kana","@value":"ネッタイ セイブ タイヘイヨウ ニ オケル タイリュウ カツドウ ノ ニチヘン"}],"description":[{"type":"abstract","notation":[{"@language":"en","@value":"Diurnal variations of convective activities in the tropical western Pacific are examined by using 3-hourly geostationary meteorological satellite data acquired over a 9-year period (1980-1989). Large diurnal variations of convection exist over continents, large islands and their adjacent sea regions such as the Indochina Peninsula, the Tibetan Plateau, North Australia and the maritime continent regions. Large diurnal variations are also found over the Bay of Bengal and the South China Sea. Although the diurnal variation is less pronounced over the open oceanic regions east of 150°E than over the maritime continent regions, moderate amplitudes of diurnal variations are observed over the Intertropical Convergence Zone (ITCZ) and the South Pacific Convergence Zone (SPCZ). Features of the diurnal variation vary with the seasons and it is enhanced during seasons in which mean convective activities become strong. Over continents and large islands, the convection attains its maximum intensity in late afternoon to evening, probably due to strong surface heating during daytime. Over sea areas in the vicinity of large islands, the maximum convective activity generally occurs in the morning. It is suggested that the interaction between land-sea circulations and large-scale environmental flows may produce a diurnal cycle in the offshore convection. There exist large amplitudes of diurnal variations over the head of the Bay of Bengal during the Indian summer monsoon season with the maximum amplitude in the afternoon. The diurnal cycle of convection becomes predominant during summer and fall over the South China Sea, with the maximum convective activity near local noontime. The convection over the ITCZ and the SPCZ has a maximum intensity in the morning, in general, but a secondary maximum of convection occurs in the afternoon. The Fourier analysis of the second component (semi-diurnal variation) suggests that there exist semi-diurnal variations of convection over the ITCZ and the SPCZ with maximum peaks around 3-4 LST and 15-16 LST."},{"@language":"ja","@value":"静止気象衛星「ひまわり」による3時間間隔、9年間のT<SUB>BB</SUB>データを用いて、熱帯西部太平洋域の対流活動の日変化の解析を行った。対流活動の大きな日変化がインドシナ半島、チベット高原、北オーストラリア、海洋大陸域等の大陸や大きな島及びその周辺海域に存在する。また、ベンガル湾と南シナ海にも大きな日変化が存在する。一方、海洋大陸域ほど大きくはないが、熱帯収束帯(ITCZ)と南太平洋収束帯(SPCZ)にも日変化が見られる。日変化の特徴は季節によって変化し、対流活動が活発な季節に日変化の振幅も増大する。大陸上及び大きな島の上では、対流活動は午後遅くから夜にかけてピークに達するが、これは日中の地表からの加熱によるものと思われる。一方、大きな島の周辺海域では、対流活動のピークは一般に午前中に現れる。このような周辺海域の対流活動の日変化は、海陸風循環と大規模な一般風との相互作用によって作られているものと思われる。ベンガル湾の北端海域の対流活動は夏のインドモンスーン期に大きな日変化を示し、午後に対流活動のピークが現れる。南シナ海の対流活動の日変化は夏から秋にかけて顕著になり、正午頃ピークになる。ITCZとSPCZの対流活動は一般に午前に最盛期に達するが、午後にもう一度活発になる。フーリエ解析の結果、ITCZやSPCZ上には半日周期の変動が存在し、3-4地方時と15-16地方時に対流活動が最大となることがわかった。"}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1030003658360829446","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"00014762"},{"@type":"NRID","@value":"1000000014762"},{"@type":"NRID","@value":"9000363497453"}],"foaf:name":[{"@language":"ja","@value":"新田 勍"},{"@language":"en","@value":"Nitta Tsuyoshi"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282681481522816","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000363496605"},{"@type":"NRID","@value":"9000392816527"}],"foaf:name":[{"@language":"ja","@value":"関根 創太"},{"@language":"en","@value":"Sekine Sota"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00261165"},{"@type":"LISSN","@value":"00261165"},{"@type":"EISSN","@value":"21869057"},{"@type":"NDL_BIB_ID","@value":"000000004812"},{"@type":"ISSN","@value":"00261165"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/00261165"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/00261165"},{"@type":"NCID","@value":"AN00317933"}],"prism:publicationName":[{"@language":"ja","@value":"気象集誌. 第2輯"},{"@value":"気象集誌. 第2輯"},{"@language":"en","@value":"Journal of the Meteorological Society of Japan. Ser. II"},{"@language":"ja","@value":"気象集誌"},{"@language":"ja","@value":"氣象集誌. 第2輯"},{"@language":"en","@value":"Journal of the Meteorological Society of Japan"},{"@language":"en","@value":"JMSJ"}],"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":"1994","prism:volume":"72","prism:number":"5","prism:startingPage":"627","prism:endingPage":"641"},"reviewed":"false","url":[{"@id":"http://id.ndl.go.jp/bib/3902017"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I3902017"},{"@id":"https://dl.ndl.go.jp/pid/10611029"},{"@id":"http://id.ndl.go.jp/digimeta/10611029"},{"@id":"https://www.jstage.jst.go.jp/article/jmsj1965/72/5/72_5_627/_pdf"},{"@id":"http://dl.ndl.go.jp/info:ndljp/pid/10611029"}],"availableAt":"1994","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011142932313728","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Diurnal Variation of Deep Cumulus Convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285711536194688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of Long- and Short-Term Atmospheric Water Cycles on the Water Balance over the Maritime Continent"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617911878144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tropical cloudiness and rainfall related to pressure and tidal variations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643726297728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Toward More Integrated Utilizations of Geostationary Satellite Data for Disaster Management and Risk Mitigation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567186513468288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Statistical Analysis of the Life Cycle of Isolated Tropical Cold Cloud Systems Using MTSAT-1R and TRMM Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580229780148992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Diurnal variations of different types of cloud over the Baiu–Meiyu frontal zone using retrieved cloud properties: Implication for the rainfall process"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654735525376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Relationship between the direction of diurnal rainfall migration and the ambient wind over the Southern Sumatra Island"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848665119431168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Diurnal variation of short-period (20–120 min) gravity waves in the equatorial Mesosphere and Lower Thermosphere and its relation to deep tropical convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570105201152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Cloud-Coverage Characteristics during Phase III of GATE as Derived from Satellite and Ship Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861294965348096","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Diurnal variation of monsoon rainfall In central India"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865815669426560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seasonal sea breeze variation analysis based on multi‐year near‐surface observations in Jakarta, Indonesia"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045122989824","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Winter Monsoon Convection in the Vicinity of North Borneo. 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Atmosphere)"},{"@value":"The dependence of numerically simulated convective storms in vertical wind shear and buoyancy"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206503590656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"西太平洋および東南アジア地域における深い積雲対流活動の解析"},{"@language":"en","@value":"Analysis of the Deep Convective Activity Over the Western Pacific and Southeast Asia"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206503728512","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"静止気象衛星観測に基づく東アジア・西太平洋における暖候期の雲量の日変化"},{"@language":"en","@value":"Diurnal Variability of Cloudiness over East Asia and the Western Pacific Ocean as Revealed by GMS during the Warm Season"},{"@language":"ja-Kana","@value":"Diurnal Variability of Cloudiness over"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206503973504","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Diurnal March of Rainfall Simulated in a T106 AGCM and Dependence on Cumulus Schemes"},{"@value":"Diurnal March of Rainfall Simulated in a T106 AGCM and Dependence on Cumulus Schemes(<Special Issue>The International Workshop on High-Resolution and Cloud Modeling, 2006)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206504398720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"衛星観測の雲量から推算した熱帯域西太平洋の月平均雨量"},{"@language":"en","@value":"Estimation of Monthly Rainfall from Satellite-Observed Cloud Amount in the Tropical Western Pacific"},{"@value":"衛星観測の雲量から推算した熱帯域西太平洋の月平均雨量〔英文〕"},{"@language":"ja-Kana","@value":"エイセイ カンソク ノ ウンリョウ カラ スイサンシタ ネッタイイキ ニシ タ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206504771328","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"北半球夏季西太平洋上における大規模対流活動の急激な季節変化"},{"@language":"en","@value":"Abrupt Seasonal Change of Large-Scale Convective Activity over the Western Pacific in the Northern Summer"},{"@value":"北半球夏季西太平洋上における大規模対流活動の急激な季節変化〔英文〕"},{"@language":"ja-Kana","@value":"キタハンキュウ カキ ニシ タイヘイヨウジョウ ニ オケル ダイキボ タイリュ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206504780672","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"アジア大陸と西部北太平洋における夏のモンスーン"},{"@language":"en","@value":"Summer Monsoon over the Asian Continent and Western North Pacific"},{"@value":"アジア大陸と西部北太平洋における夏のモンスーン〔英文〕"},{"@language":"ja-Kana","@value":"アジア タイリク ト セイブ キタ タイヘイヨウ ニ オケル ナツ ノ モンス"},{"@value":"Summer monsoon over the Asian continent and the western North Pacific."}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206504790016","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"熱帯太平洋・インド洋における降水量の十年スケール変動"},{"@language":"en","@value":"Interdecadal Variations of Precipitation over the Tropical Pacific and Indian Oceans"},{"@value":"熱帯太平洋・インド洋における降水量の10年スケール変動〔英文〕"},{"@language":"ja-Kana","@value":"ネッタイ タイヘイヨウ インドヨウ ニ オケル コウスイリョウ ノ 10ネン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206505361152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Diurnal Convection Peaks over the Eastern Indian Ocean off Sumatra during Different MJO Phases"},{"@value":"Notes and correspondence: Diurnal convection peaks over the eastern Indian Ocean off Sumatra during different MJO phases"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206505366784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Convective Systems Developed along the Coastline of Sumatera Island, Indonesia, Observed with an X-band Doppler Radar during the HARIMAU2006 Campaign"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206505609216","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Diurnal Cycle of Cloud System Migration over Sumatera Island"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679415752832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Characteristics of Precipitation Distribution over the Irrawaddy and the Mekong Watersheds Using Tropical Rainfall Measuring Misson (TRMM) Data"},{"@language":"ja","@value":"熱帯降雨観測衛星データを用いたイラワジ川，メコン川流域における降水量分布の特性"},{"@language":"ja-Kana","@value":"ネッタイ コウウ カンソク エイセイ データ オ モチイタ イラワジガワ メコンガワ リュウイキ ニ オケル 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