{"@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/1390282681483863808.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2151/jmsj1965.78.4_461"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/jmsj1965/78/4/78_4_461/_pdf"}},{"identifier":{"@type":"NAID","@value":"130007347303"}}],"dc:title":[{"@language":"ja","@value":"インドシナ半島の降水日変化"},{"@language":"en","@value":"Diurnal variation of precipitation over the Indo-China Peninsula"},{"@value":"Diurnal variation of precipitation over the Indo‐China Peninsula: two‐dimensional numerical simulation"}],"dcterms:alternative":[{"@language":"ja","@value":"2次元数値実験"},{"@language":"en","@value":"Two-dimensional numerical simulation"}],"description":[{"type":"abstract","notation":[{"@language":"en","@value":"The diurnal variation of precipitation over the Indo-China Peninsula is investigated using a two-dimensional, nonhydrostatic, and cloud-resolving numerical model. The model is initialized by the climatological monthly mean vertical profiles of zonal flow, temperature and humidity at the center of the Indo-China Peninsula in June.<br>The model successfully simulates the diurnal variation of precipitation. The simulated diurnal variation is as follows: convection is activated at the lee-side foot of two mountainous regions located at the west and middle of Thailand in the evening of each day; activated clouds then are organized into squall lines that travel eastward during the night at about 5-10m s<sup>-1</sup>. These squall lines weaken around midnight.<br>It is concluded that the solar-synchronized life cycle of the squall lines and their eastward movement cause the nighttime maximum of the precipitation over the inland area of the Indo-China Peninsula. High resolution analysis of a convective activity index calculated from the GMS IR data over the Peninsula supports this conclusion."},{"@language":"ja","@value":"2次元非静水圧雲解像モデルを用い、インドシナ半島の降水日変化について調べた。モデルの初期値は、インドシナ半島のほぼ中央である東経102.5度北緯17.5度における6月気候値の風速・気温・湿度の鉛直分布から作成した。<br>モデルは観測されている日変化の特徴をうまく再現することができた。モデルによる日変化は、1)タイ西部と中央部に位置する山地の風下側山麓において対流雲が夕方に励起され、2)それらがスコールラインに組織化されて夜間に東へ移動して行く、という現象の繰り返しで起こっている。このスコールラインの移動速度は5-10ms<sup>-1</sup>であった。また、風下山麓での対流励起機構やスコールラインの構造について検討し、中緯度での観測や数値実験との比較も行った。<br>これらの計算結果に基づき、太陽同期したスコールラインの発生と東への移動がインドシナ半島内陸部の降水日変化の夜の極大をもたらしている、と結論した。高分解能の対流活動指数を用いた対流雲活動の日変化の空間分布も解析し、数値実験を支持する結果を得た。"}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1030003658634122629","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"20273435"},{"@type":"NRID","@value":"1000020273435"},{"@type":"NRID","@value":"9000363405154"},{"@type":"NRID","@value":"9000363407253"},{"@type":"NRID","@value":"9000024147423"},{"@type":"NRID","@value":"9000018860739"},{"@type":"NRID","@value":"9000392819677"},{"@type":"NRID","@value":"9000007402404"},{"@type":"NRID","@value":"9000363406384"},{"@type":"NRID","@value":"9000283228375"},{"@type":"NRID","@value":"9000257978915"},{"@type":"NRID","@value":"9000363488235"},{"@type":"NRID","@value":"9000363405192"},{"@type":"NRID","@value":"9000363405362"},{"@type":"NRID","@value":"9000363404161"},{"@type":"NRID","@value":"9000363404239"},{"@type":"NRID","@value":"9000363406073"},{"@type":"NRID","@value":"9000363406667"},{"@type":"NRID","@value":"9000363406945"},{"@type":"NRID","@value":"9000363406468"},{"@type":"NRID","@value":"9000024139458"},{"@type":"NRID","@value":"9000283784018"},{"@type":"NRID","@value":"9000392818035"},{"@type":"NRID","@value":"9000363485353"},{"@type":"NRID","@value":"9000363410931"},{"@type":"NRID","@value":"9000363405342"},{"@type":"NRID","@value":"9000363481298"},{"@type":"NRID","@value":"9000392814599"},{"@type":"NRID","@value":"9000254885086"},{"@type":"NRID","@value":"9000363405214"},{"@type":"NRID","@value":"9000363407300"},{"@type":"NRID","@value":"9000363407034"},{"@type":"NRID","@value":"9000392818039"},{"@type":"NRID","@value":"9000363408611"},{"@type":"NRID","@value":"9000363407306"},{"@type":"NRID","@value":"9000365518824"},{"@type":"NRID","@value":"9000392819088"},{"@type":"NRID","@value":"9000363496470"},{"@type":"NRID","@value":"9000363410550"},{"@type":"NRID","@value":"9000363480064"},{"@type":"NRID","@value":"9000392820072"},{"@type":"NRID","@value":"9000392819702"},{"@type":"NRID","@value":"9000254865076"},{"@type":"NRID","@value":"9000363481522"},{"@type":"NRID","@value":"9000363404933"},{"@type":"NRID","@value":"9000347102247"},{"@type":"NRID","@value":"9000392812967"},{"@type":"NRID","@value":"9000283236768"},{"@type":"NRID","@value":"9000007401910"},{"@type":"NRID","@value":"9000363407773"},{"@type":"NRID","@value":"9000363406551"},{"@type":"NRID","@value":"9000392817252"},{"@type":"NRID","@value":"9000265258143"},{"@type":"NRID","@value":"9000363501294"},{"@type":"NRID","@value":"9000363480013"},{"@type":"NRID","@value":"9000363405583"},{"@type":"NRID","@value":"9000363405617"},{"@type":"NRID","@value":"9000392816834"},{"@type":"NRID","@value":"9000363407649"},{"@type":"NRID","@value":"9000363407663"},{"@type":"NRID","@value":"9000258521878"},{"@type":"NRID","@value":"9000363410828"},{"@type":"NRID","@value":"9000363405058"},{"@type":"NRID","@value":"9000363407767"},{"@type":"NRID","@value":"9000365518859"},{"@type":"NRID","@value":"9000392815683"},{"@type":"NRID","@value":"9000363401309"},{"@type":"NRID","@value":"9000363404687"},{"@type":"NRID","@value":"9000363402948"},{"@type":"NRID","@value":"9000363485458"},{"@type":"NRID","@value":"9000363487869"},{"@type":"NRID","@value":"9000363485268"},{"@type":"NRID","@value":"9000363499214"},{"@type":"NRID","@value":"9000363401637"},{"@type":"NRID","@value":"9000363482057"},{"@type":"NRID","@value":"9000363484552"},{"@type":"NRID","@value":"9000363404487"},{"@type":"NRID","@value":"9000363404838"},{"@type":"NRID","@value":"9000363489730"},{"@type":"NRID","@value":"9000364841010"},{"@type":"NRID","@value":"9000363401091"},{"@type":"NRID","@value":"9000363485462"},{"@type":"NRID","@value":"9000363404568"},{"@type":"NRID","@value":"9000363487399"},{"@type":"NRID","@value":"9000363401446"},{"@type":"NRID","@value":"9000363497340"},{"@type":"NRID","@value":"9000363483280"},{"@type":"NRID","@value":"9000363402877"},{"@type":"NRID","@value":"9000363403211"},{"@type":"NRID","@value":"9000363492882"},{"@type":"NRID","@value":"9000363499029"},{"@type":"NRID","@value":"9000363401729"},{"@type":"NRID","@value":"9000363490050"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0046926"}],"foaf:name":[{"@language":"ja","@value":"里村 雄彦"},{"@language":"en","@value":"Satomura Takehiko"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Division of Earth and Planetary Science, Graduate School of Science, Kyoto University"},{"@language":"ja","@value":"京都大学大学院理学研究科"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00261165"},{"@type":"LISSN","@value":"00261165"},{"@type":"EISSN","@value":"21869057"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/00261165"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/00261165"}],"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":"2000","prism:volume":"78","prism:number":"4","prism:startingPage":"461","prism:endingPage":"475"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"https://www.jstage.jst.go.jp/article/jmsj1965/78/4/78_4_461/_pdf"}],"availableAt":"2000","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011145618240128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mesoscale and Convective–Scale Downdrafts as Distinct Components of Squall-Line Structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145958362880","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the use of a coordinate transformation for the solution of the Navier-Stokes equations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617917296128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Diurnal Variations in Tropical Oceanic Cumulus Convection during TOGA COARE"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620038908544","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Generation of a Mesoscale Convective System from Mountain Convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181944823296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Cloud episode propagation over the Indonesian Maritime Continent from 10years of infrared brightness temperature observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092884785408","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Relationship between Large-Scale Convective Rainfall and Cold Cloud over the Western Hemisphere during 1982-84"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092894011264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Diurnal Variations in Precipitation and Thunderstorm Frequency over the Conterminous United States"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574093586600960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Diurnal Variability of Precipitation across the Central Rockies and Adjacent Great Plains"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848655105760128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Land‐lake breezes at low latitudes: The case of Tonle Sap Lake in Cambodia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567869935232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An Examination of the Diurnal Cycle in Oceanic Tropical Rainfall Using Satellite and In Situ Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569495649152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Simulation of Three-Dimensional Convective Storm Dynamics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593759055104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Diurnal Characteristics of Summer Precipitation Over Luzon Island, Philippines"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044794046208","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mechanisms of Cell Regeneration, Development, and Propagation within a Two-Dimensional Multicell Storm"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993753190784","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Comparison of Two Methods for the Retrieval of Thermodynamic and Microphysical Variables from Doppler Radar Measurements: Application to the Case of a Tropical Squall Line"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994598870528","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the Relationship between Satellite-Observed Cloud Cover and Precipitation"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699996095036800","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Tropical Squall Line Observed during the COPT 81 Experiment in West Africa. 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Season"},{"@language":"ja-Kana","@value":"Diurnal Variability of Cloudiness over"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206503973504","@type":"Article","relationType":["isReferencedBy"],"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/1390001206504902656","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Internal Structures of Migratory Cloud Systems with Diurnal Cycle over Sumatera Island during CPEA-I Campaign"},{"@value":"Internal structures of migratory cloud systems with diurnal cycle over Sumatera Island during CPEA-1 campaign"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206505609216","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Diurnal Cycle of Cloud System Migration over Sumatera Island"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206505726720","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Nighttime Precipitation Induced by a Synoptic-scale Convergence in the Central Tibetan Plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679415752832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"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 コウスイリョウ ブンプ ノ トクセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680199553920","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Numerical Simulation on the Diurnal Variation of Precipitation over Northeastern Bangladesh: A Case Study of an Active Period 14-21 June 1995"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680199610240","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Impact of Trans-equatorial Monsoon Flow on the Formation of Repeated Torrential Rains over Java Island"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680199949184","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seasonal and Diurnal Variations in Rainfall Characteristics over the Tropical Asian Monsoon Region Using TRMM-PR 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