{"@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/1360004229806915584.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2016jd026116"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016JD026116"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016JD026116"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Contrasting Features of Monsoon Precipitation Around the Meghalaya Plateau Under Westerly and Easterly Regimes"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Precipitation features around the Meghalaya Plateau, northeast India, during summer are investigated using a 17 year (1998–2014) high‐spatial‐resolution Tropical Rainfall Measuring Mission precipitation radar data set. Precipitation around the plateau fell into two distinct regimes based on the low‐level wind direction that fluctuates on intraseasonal time scales over Bangladesh, windward of the plateau: a westerly regime (WR) and an easterly regime (ER). Under the WR, strong low‐level onshore southwesterlies across Bangladesh encounter the plateau, and localized strong low‐level southerlies running parallel to the Arakan Mountains (i.e., the barrier jet) also blow toward the plateau, concentrating convective unstable air onto its southern slopes. The low‐level wind fields and large‐scale upper level divergent fields promote frequent and intense orographic rainfall along the southern slopes due to forced uplift, generating high precipitation. In contrast, under the ER, strong southeasterlies that blow along the Gangetic Plain without encountering the plateau and subsidence inhibit upward motion around the plateau, resulting in low precipitation. Diurnal variations in precipitation significantly affect the daily precipitation around the plateau under both regimes. High rainfall frequency persists over the southern slopes between 2100 and 1200 LT of the next day under the WR, whereas modest rainfall frequency occurs between 0000 and 0600 LT under the ER, with a daytime minimum and nocturnal maximum in both regimes. The atmospheric boundary layer processes over Bangladesh regulate the wind speed and vertical structure of the low‐level wind toward the plateau, with deceleration during daytime and acceleration at night (i.e., nocturnal jet) that result in the nocturnal rainfall maximum.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420845751164004864","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"60402559"},{"@type":"NRID","@value":"1000060402559"},{"@type":"NRID","@value":"9000363499847"},{"@type":"NRID","@value":"9000363486197"},{"@type":"NRID","@value":"9000363504104"},{"@type":"NRID","@value":"9000398135214"},{"@type":"NRID","@value":"9000257827553"},{"@type":"NRID","@value":"9000370253476"},{"@type":"NRID","@value":"9000257767694"},{"@type":"NRID","@value":"9000283593278"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0133100"}],"foaf:name":[{"@value":"Hatsuki Fujinami"}],"jpcoar:affiliationName":[{"@value":"Institute for Space‐Earth Environmental Research Nagoya University  Nagoya Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420564276170793600","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"10512270"},{"@type":"NRID","@value":"1000010512270"},{"@type":"NRID","@value":"9000403044928"},{"@type":"NRID","@value":"9000363489961"},{"@type":"NRID","@value":"9000283593785"},{"@type":"NRID","@value":"9000248205958"},{"@type":"NRID","@value":"9000365497883"},{"@type":"NRID","@value":"9000413536716"},{"@type":"NRID","@value":"9000308732196"},{"@type":"NRID","@value":"9000283593424"},{"@type":"NRID","@value":"9000270894664"},{"@type":"NRID","@value":"9000391552546"},{"@type":"NRID","@value":"9000283621214"},{"@type":"NRID","@value":"9000283419154"},{"@type":"NRID","@value":"9000270894642"},{"@type":"NRID","@value":"9000410493974"},{"@type":"NRID","@value":"9000275837959"},{"@type":"NRID","@value":"9000243844096"},{"@type":"NRID","@value":"9000378104696"},{"@type":"NRID","@value":"9000406310681"},{"@type":"NRID","@value":"9000363481804"},{"@type":"NRID","@value":"9000365043224"},{"@type":"NRID","@value":"9000363481461"},{"@type":"NRID","@value":"9000363493778"},{"@type":"NRID","@value":"9000263041455"},{"@type":"NRID","@value":"9000270894835"},{"@type":"NRID","@value":"9000362802342"},{"@type":"NRID","@value":"9000365497940"},{"@type":"NRID","@value":"9000402607655"},{"@type":"NRID","@value":"9000296664320"},{"@type":"NRID","@value":"9000311062245"},{"@type":"NRID","@value":"9000402246595"},{"@type":"NRID","@value":"9000257827940"},{"@type":"NRID","@value":"9000365043626"},{"@type":"NRID","@value":"9000404630298"},{"@type":"NRID","@value":"9000290819238"},{"@type":"NRID","@value":"9000392043761"},{"@type":"NRID","@value":"9000341532784"},{"@type":"NRID","@value":"9000333924097"},{"@type":"NRID","@value":"9000403151049"},{"@type":"NRID","@value":"9000365043324"},{"@type":"NRID","@value":"9000380122989"},{"@type":"NRID","@value":"9000380123006"},{"@type":"NRID","@value":"9000257767690"},{"@type":"NRID","@value":"9000332695288"},{"@type":"NRID","@value":"9000241967196"},{"@type":"NRID","@value":"9000402937647"},{"@type":"NRID","@value":"9000412526302"},{"@type":"NRID","@value":"9000283593264"},{"@type":"NRID","@value":"9000283593731"},{"@type":"NRID","@value":"9000241177661"},{"@type":"NRID","@value":"9000398388366"},{"@type":"NRID","@value":"9000399252238"},{"@type":"NRID","@value":"9000363489953"},{"@type":"NRID","@value":"9000363490246"},{"@type":"NRID","@value":"9000363488433"},{"@type":"NRID","@value":"9000363504061"},{"@type":"NRID","@value":"9000363492245"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/tmnr193sato"}],"foaf:name":[{"@value":"Tomonori Sato"}],"jpcoar:affiliationName":[{"@value":"Faculty of Environmental Earth Science Hokkaido University  Sapporo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420845751140749312","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"50422803"},{"@type":"NRID","@value":"1000050422803"},{"@type":"NRID","@value":"9000016707938"}],"foaf:name":[{"@value":"Hironari Kanamori"}],"jpcoar:affiliationName":[{"@value":"Institute for Space‐Earth Environmental Research Nagoya University  Nagoya Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229806915717","@type":"Researcher","foaf:name":[{"@value":"Fumie Murata"}],"jpcoar:affiliationName":[{"@value":"Faculty of Science and Technology Kochi University  Kochi Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"2169897X"},{"@type":"EISSN","@value":"21698996"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Atmospheres"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2017-09-21","prism:volume":"122","prism:number":"18","prism:startingPage":"9591","prism:endingPage":"9610"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016JD026116"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016JD026116"}],"createdAt":"2017-08-29","modifiedAt":"2023-09-10","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781833377920","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H05464"},{"@type":"JGN","@value":"JP15H05464"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15H05464/"}],"notation":[{"@language":"ja","@value":"日本およびアジア地域における過去の地域気候変動のアトリビューション"},{"@language":"en","@value":"Attribution of the past regional climate change around Japan and East Asia"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257256993792","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26220202"},{"@type":"JGN","@value":"JP26220202"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26220202/"}],"notation":[{"@language":"ja","@value":"過去120年間におけるアジアモンスーン変動の解明"},{"@language":"en","@value":"Asian monsoon variability during the past 120 years"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257274582912","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26400465"},{"@type":"JGN","@value":"JP26400465"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26400465/"}],"notation":[{"@language":"ja","@value":"メガラヤ・バングラデシュ・ミャンマー地域に豪雨をもたらす渦状低気圧の実態解明"},{"@language":"en","@value":"A study on vortex-type low pressure systems around the Meghalaya, Bangladesh and Myanmar region"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050587981430747776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Effects of the South Asian Monsoon Intraseasonal Modes on Genesis of Low Pressure Systems over Bangladesh"}]},{"@id":"https://cir.nii.ac.jp/crid/1050869456410090880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mechanism of Orographic Precipitation around the Meghalaya Plateau Associated with Intraseasonal Oscillation and the Diurnal Cycle"},{"@value":"Mechanism of Orographic Precipitation around the Meghalaya Plateau Associated with Intraseasonal Oscillation and Diurnal Cycle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216709789568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal variation of rainfall over the central Himalayan region revealed by TRMM Precipitation Radar"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005514860703104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mesoscale precipitation systems and their role in the rapid development of a monsoon depression over the Bay of Bengal"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142938625792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Diurnal rainfall pattern observed by Tropical Rainfall Measuring Mission Precipitation Radar (TRMM‐PR) around the Indochina peninsula"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143940938496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Nocturnal jet and its effects on early morning rainfall peak over northeastern Bangladesh during the summer monsoon season"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144472245760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global Distribution and Characteristics of Diurnally Varying Low-Level Jets"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144793773440","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Diurnal variation in summer monsoon precipitation during active and break periods over central India and southern Himalayan foothills"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146205644288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Surface flux and atmospheric boundary layer observations from the LAPS project over the middle stream of the Huaihe River basin in China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013173111529472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Time evolution of monsoon low-level jet observed over an Indian tropical station during the peak monsoon period from high-resolution Doppler wind lidar measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617911043328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The ERA‐Interim reanalysis: configuration and performance of the data assimilation system"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617915336576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Convectively coupled equatorial waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621167950336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Very high resolution precipitation climatologies from the Tropical Rainfall Measuring Mission precipitation radar"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643749111552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Cloud-Resolving-Model Simulations of Nocturnal Precipitation over the Himalayan Slopes and Foothills"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643755648896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of Convection Representation and Model Resolution on Diurnal Precipitation Cycle Over the Indian Monsoon Region: Toward a Convection‐Permitting Regional Climate Simulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298754807874560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Nocturnal Southerly Moist Surge Parallel to the Coastline Over the Western Bay of Bengal"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302865716298112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Climatological characteristics of nocturnal eastward‐propagating diurnal precipitation peak over South India during summer monsoon: Role of monsoon low‐level circulation and gravity waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165256564096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Dynamics of distinct intraseasonal oscillation in summer monsoon rainfall over the Meghalaya–Bangladesh–western Myanmar region: covariability between the tropics and mid-latitudes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565168765464704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seasonal and Intraseasonal Modulation of Tropical Cyclogenesis Environment over the Bay of Bengal during the Extended Summer Monsoon"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179901011584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Decreasing number of propagating mesoscale convective systems in Bangladesh and surrounding area during 1998–2015"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092461265152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Characteristics of Orographic Rain Drop-Size Distribution at Cherrapunji, Northeast India"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092887121536","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Spatial and diurnal variation of precipitation systems over Asia observed by the TRMM Precipitation Radar"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118725245696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Twice‐Daily Monsoon Precipitation Maxima in the Himalayas Driven by Land Surface Effects"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118726246272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Influence of Terrestrial Precipitation on the Variability of Extreme Sea Levels along the Coast of Bangladesh"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848661490222848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Characteristics of Low Pressure Systems Associated with Intraseasonal Oscillation of Rainfall over Bangladesh during Boreal Summer"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567860544256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rain-Profiling Algorithm for the TRMM Precipitation Radar"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569724617088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Topography, relief, and TRMM‐derived rainfall variations along the Himalaya"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570978132096","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Active / break cycles: diagnosis of the intraseasonal variability of the Asian Summer Monsoon"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043646064384","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Relationship between atmospheric conditions at Dhaka, Bangladesh, and rainfall at Cherrapunjee, India"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045345631744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Status of the Tropical Rainfall Measuring Mission (TRMM) after Two Years in Orbit"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520501402624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Some Effects of Finite Sample Size and Persistence on Meteorological Statistics. Part I: Autocorrelations"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520637131648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Tropical Rainfall Measuring Mission (TRMM) Sensor Package"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520848046592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Barrier Winds Along the Sierra Nevada Mountains"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418521297490176","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The composite structure of the monsoon depression"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993672049664","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Characteristic intraseasonal oscillation of rainfall and its effect on interannual variability over Bangladesh during boreal summer"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994689470848","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Onset and Interannual Variability of the Asian Summer Monsoon in Relation to Land–Sea Thermal Contrast"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995765447168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The 10 to 20-day westward propagating mode and “Breaks in the Monsoons”"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469439116416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Probing orographic controls in the Himalayas during the monsoon using satellite imagery"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944109668992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the Structure and Dynamics of Indian Monsoon Depressions"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945073482112","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Very high resolution rainfall patterns measured by TRMM precipitation radar: seasonal and diurnal cycles"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262946112211712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Characteristics of Precipitating Convective Systems in the South Asian Monsoon"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544418639698432","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Conceptual View on Inertial Oscillations and Nocturnal Low-Level Jets"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419330699648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Orographic effects on precipitating clouds"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420810884224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"APHRODITE: Constructing a Long-Term Daily Gridded Precipitation Dataset for Asia Based on a Dense Network of Rain Gauges"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894837986432","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Clustering of synoptic activity by Indian summer monsoon intraseasonal oscillations"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369117845504","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The 10–20-Day Mode of the 1979 Indian Monsoon: Its Relation with the Time Variation of Monsoon Rainfall"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370632261888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Boundary Layer Wind Maxima and Their Significance for the Growth of Nocturnal Inversions"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107371386194304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Composite Structure of Monsoon Low Pressure Systems and Its Relation to Indian Rainfall"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845788054144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A global climatology of monsoon low‐pressure systems"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319763603584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Regional, Seasonal, and Diurnal Variations of Extreme Convection in the South Asian Region"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320716668672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Barrier Jets during TAMEX"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670321097378048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Finescale Diurnal Rainfall Statistics Refined from Eight Years of TRMM PR Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795621338880","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rainfall on the Meghalaya plateau in northeastern India—one of the rainiest places in the world"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268177308416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A climatological‐dynamical analysis associated with precipitation around the southern part of the Himalayas"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206505233024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"北半球夏季モンスーン時における雲量変動の解析"},{"@language":"en","@value":"Cloudiness Fluctuations Associated with the Northern Hemisphere Summer Monsoon"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206505974656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"ベンガル湾及び南シナ海上の夏季モンスーンの早期開始におけるチベット高原の温度上昇の役割"},{"@language":"en","@value":"Role of Warming over the Tibetan Plateau in Early Onset of the Summer Monsoon over the Bay of Bengal and the South China Sea"},{"@language":"ja-Kana","@value":"Role of Warming over the Tibetan Platea"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680198065024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A 44-Year Daily Gridded Precipitation Dataset for Asia Based on a Dense Network of Rain Gauges"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680199338752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Characteristics of Diurnal Variations in Convection and Precipitation over the Southern Tibetan Plateau during Summer"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680199553920","@type":"Article","relationType":["references"],"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/1390282681478253696","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Seasonal and Intraseasonal Variability of Diurnal Cloud Activity over the Tibetan Plateau."},{"@language":"ja-Kana","@value":"Seasonal and Intraseasonal Variability of Diurnal Cloud Activity over the Tibetan Plateau"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681479347200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Diurnal Variations of Convective Activity and Rainfall in Tropical Asia."},{"@value":"Diurnal variations of connective activity and rainfall in tropical Asia"},{"@value":"The diurnal variations of convective activity and rainfall in tropical Asia"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681482291200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Formation of Tropical Cyclones in the Northern Indian Ocean Associated with Two Types of Tropical Intraseasonal Oscillation Modes"},{"@value":"Formation of Nargis (2008) and tropical cyclones in the northern Indian Ocean associated with with tropical intraseasonal oscillation"}]},{"@id":"https://cir.nii.ac.jp/crid/1390851275429701248","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Progress from TRMM to GPM"},{"@language":"ja","@value":"熱帯降雨観測衛星（TRMM）から全球降水観測計画（GPM）への進歩"},{"@value":"Progress from TRMM to GPM : Special Edition on Global Precipitation Measurement (GPM) : 5th Anniversary"}]},{"@id":"https://cir.nii.ac.jp/crid/1574231874781179392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Intraseasonal oscillations and interannual variability of the Indian summer monsoon"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367065767168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seasonal variation in isotopic composition and the origin of precipitation over Bangladesh"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2016jd026116"},{"@type":"KAKEN","@value":"PRODUCT-21782093"},{"@type":"KAKEN","@value":"PRODUCT-21657906"},{"@type":"KAKEN","@value":"PRODUCT-21875822"},{"@type":"OPENAIRE","@value":"doi_dedup___::3a11720b876fc92b7f5e0c431a7595f5"},{"@type":"CROSSREF","@value":"10.1002/qj.3672_references_DOI_Lur01o0csk8niJnR2RxrwSv9FF5"},{"@type":"CROSSREF","@value":"10.2151/jmsj.2021-035_references_DOI_Lur01o0csk8niJnR2RxrwSv9FF5"},{"@type":"CROSSREF","@value":"10.1175/jhm-d-21-0103.1_references_DOI_Lur01o0csk8niJnR2RxrwSv9FF5"},{"@type":"CROSSREF","@value":"10.1029/2019jd032150_references_DOI_Lur01o0csk8niJnR2RxrwSv9FF5"},{"@type":"CROSSREF","@value":"10.1029/2022gl100174_references_DOI_Lur01o0csk8niJnR2RxrwSv9FF5"},{"@type":"CROSSREF","@value":"10.1002/met.2106_references_DOI_Lur01o0csk8niJnR2RxrwSv9FF5"},{"@type":"CROSSREF","@value":"10.1002/asl.879_references_DOI_Lur01o0csk8niJnR2RxrwSv9FF5"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0231-4_references_DOI_Lur01o0csk8niJnR2RxrwSv9FF5"},{"@type":"CROSSREF","@value":"10.3390/atmos11080777_references_DOI_Lur01o0csk8niJnR2RxrwSv9FF5"},{"@type":"CROSSREF","@value":"10.1029/2020jd034255_references_DOI_Lur01o0csk8niJnR2RxrwSv9FF5"},{"@type":"CROSSREF","@value":"10.3390/w13202915_references_DOI_Lur01o0csk8niJnR2RxrwSv9FF5"}]}