{"@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/1390282681540360960.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1007/bf02110288"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/BF02110288.pdf"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/article/10.1007/BF02110288/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/BF02110288"}},{"identifier":{"@type":"NAID","@value":"130004053478"}}],"dc:title":[{"@language":"en","@value":"Origin of the Abiki phenomenon (a kind of seiche) in Nagasaki bay."},{"@language":"ja","@value":"長崎湾におけるあびき現象 (湾内の大規模なセィシュ) の発生機構"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"Large oscillations of water level in Nagasaki Bay are called <I>Abiki</I> and are most frequently observed in winter. The largest <I>Abiki</I> recorded in the past 20 years at the tide station at Nagasaki occurred on March 31, 1979. Simultaneously, a distinct atmospheric pressure disturbance of solitary type with an amplitude of about 3 mb was recorded at several neighbouring stations in Kyûshû, which indicated the pressure disturbance probably travelled eastward with an average speed of about 110kmh<SUP>-1</SUP><BR>The quantitative relation between this pressure disturbance and notable seiches observed in Nagasaki Bay is examined by means of numerical simulation, and it is confirmed that the exceptionally large range of oscillations in the bay, which reached 278 cm at the tide station, was indeed produced by this travelling pressure disturbance.<BR>The leading part of shallow water waves induced by the atmospheric pressure disturbance was amplified up to about 10cm in amplitude, over the broad continental shelf region off China, because of near resonant coupling to the pressure disturbance. After leaving this continental shelf region, the amplified water wave converged into the shelf region (Gotô Nada) surrounded by the north-western coast of Kyûshû and the Gotô. Islands and excited eigenoscillations on the shelf. A train of waves thus: formed with a period of about 35 min entered Nagasaki Bay and was resonantly amplified at periods of 36 min and 23 min which are the eigen periods of the bay. Besides resonance, the combined effects of shoaling and reflection inside Nagasaki Bay also enhanced the amplification."},{"@value":"長崎湾内で通例は冬期にしばしば見られるあびきが, 1979年3月31日に長崎海洋気象台観測史上最大の規模で発生した.これを例として, 数値シミュレーションを行ない, その発生機構について, 定量的な考察を試みた.その結果, 湾内の顕著な振動 (長崎験潮所で最大潮位差278cmを記録) は, 東シナ海を, ほぼ東向きに, 約110kmh<SUP>-1</SUP>の速度で進行した振幅約3mbの気圧波によっておこされたとすれば説明できることがわかった。<BR>また, その発生の過程については,<BR>1) 東シナ海大陸棚上での気圧波との共鳴的カップリングによる海洋長波の振幅10cmに及ぶ増幅3) 長崎湾内での浅水増幅および反射干渉による増幅;3) 長崎湾の固有振動系と, 五島灘領域の振動系との干渉による共鳴増幅効果など, 数段階の増幅作用が絡んでおり, これらによって生成された約35分周期の一連の波によって, 同湾の固有周期に相当する36分および23分周期で共鳴的に増幅されたことが, 定量的に結論づけられた。"}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410282681540360960","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000254986955"}],"foaf:name":[{"@language":"en","@value":"KAJIURA Kinjiro"},{"@language":"ja","@value":"梶浦 欣二郎"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Earthquake Research Institute, University of Tokyo"},{"@language":"ja","@value":"東京大学地震研究所津波・高潮部門"}]},{"@id":"https://cir.nii.ac.jp/crid/1420564276189102464","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"80192714"},{"@type":"NRID","@value":"1000080192714"},{"@type":"NRID","@value":"9000001423531"},{"@type":"NRID","@value":"9000316203821"},{"@type":"NRID","@value":"9000406305787"},{"@type":"NRID","@value":"9000406305886"},{"@type":"NRID","@value":"9000008357345"},{"@type":"NRID","@value":"9000016909925"},{"@type":"NRID","@value":"9000406306154"},{"@type":"NRID","@value":"9000001237681"},{"@type":"NRID","@value":"9000016877978"},{"@type":"NRID","@value":"9000254986954"},{"@type":"NRID","@value":"9000398961875"},{"@type":"NRID","@value":"9000405646396"},{"@type":"NRID","@value":"9000000240502"},{"@type":"NRID","@value":"9000410649568"},{"@type":"NRID","@value":"9000398993052"},{"@type":"NRID","@value":"9000254432573"},{"@type":"NRID","@value":"9000405646291"},{"@type":"NRID","@value":"9000406305699"},{"@type":"NRID","@value":"9000256137532"},{"@type":"NRID","@value":"9000415133579"},{"@type":"NRID","@value":"9000363396769"},{"@type":"NRID","@value":"9000363396975"},{"@type":"NRID","@value":"9000363397332"},{"@type":"NRID","@value":"9000363393749"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0167128"}],"foaf:name":[{"@language":"en","@value":"HIBIYA Toshiyuki"},{"@language":"ja","@value":"日比谷 紀之"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Earthquake Research Institute, University of Tokyo"},{"@language":"ja","@value":"東京大学地震研究所津波・高潮部門"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00298131"},{"@type":"EISSN","@value":"21863113"},{"@type":"EISSN","@value":"1573868X"}],"prism:publicationName":[{"@language":"en","@value":"Journal of the Oceanographical Society of Japan"},{"@language":"ja","@value":"日本海洋学会誌"},{"@language":"en","@value":"Journal of the Oceanographical Society of Japan"},{"@language":"ja","@value":"日本海洋学会誌"}],"dc:publisher":[{"@language":"en","@value":"The Oceanographic Society of Japan"},{"@language":"ja","@value":"日本海洋学会"}],"prism:publicationDate":"1982","prism:volume":"38","prism:number":"3","prism:startingPage":"172","prism:endingPage":"182"},"reviewed":"false","url":[{"@id":"http://link.springer.com/content/pdf/10.1007/BF02110288.pdf"},{"@id":"http://link.springer.com/article/10.1007/BF02110288/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1007/BF02110288"}],"availableAt":"1982","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050296343289995520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tsunami Triggered by the Lamb Wave From the 2022 Tonga Volcanic Eruption and Transition in the Offshore Japan Region"}]},{"@id":"https://cir.nii.ac.jp/crid/1050297892124522496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Multi-scale Simulation of 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トクセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205319424896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Characteristics of Propagation of Slight Atmospheric Pressure Changes by F-K Analysis"},{"@value":"波数スペクトル解析による微気圧変動の水平及び鉛直伝搬特性"},{"@language":"ja-Kana","@value":"ハスウ スペクトル カイセキ ニ ヨル ビキアツ ヘンドウ ノ スイヘイ オヨビ エンチョク デンパン トクセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205319490432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Differences of Sea Areas where Seiches Occur by Differences of Propagation Characteristics of Slight Atmospheric Pressure Changes."},{"@language":"ja","@value":"微気圧変動の伝播特性の違いによる副振動の発生海域の違い"},{"@language":"ja-Kana","@value":"ビキアツ ヘンドウ ノ デンパ トクセイ ノ チガイ ニ ヨル フクシンドウ ノ ハッセイ カイイキ ノ チガイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205319645184","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"冬季東シナ海上における気象津波発生に関する船上観測"},{"@language":"en","@value":"METEOROLOGICAL OBSERVATION ON GENESIS OF THE METEOTSUNAMI IN THE EAST CHINA SEA"},{"@language":"ja-Kana","@value":"トウキ ヒガシシナ カイジョウ ニ オケル キショウ ツナミ ハッセイ ニ カンスル フネ ジョウ カンソク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205319649664","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"東シナ海上における気圧波の伝搬経路と九州西岸で生じる水位変動の関係"},{"@language":"en","@value":"RELATIONSHIP BETWEEN PROPAGATION PATHS OF ATMOSPHERIC PRESSURE WAVE OVER THE EAST CHINA SEA AND SEA LEVEL FLUCTUATION OFF THE WEST COAST OF KYUSHU."},{"@language":"ja-Kana","@value":"ヒガシシナ カイジョウ ニ オケル キアツハ ノ デンパン ケイロ ト キュウシュウ セイガン デ ショウジル スイイ ヘンドウ ノ カンケイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205320203904","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Meteorological conditions inducing meteotsunami at Kamikoshiki Island in February 2009"},{"@language":"ja","@value":"2009年2月に上甑島で潮位副振動を発生させた気象場に関する解析"},{"@language":"ja-Kana","@value":"2009ネン 2ガツ ニ カミコシキジマ デ チョウイ フクシンドウ オ ハッセイ サセタ キショウジョウ ニ カンスル カイセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205320508800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"ニューラルネットワークモデルを用いた九州西岸域のあびき予測に関する基礎的研究"},{"@language":"en","@value":"BASIC STUDY ON REAL-TIME PREDICTION OF ABIKI AROUND WEST KYUSHU COAST BY USING NEURAL NETWORK MODEL"},{"@language":"ja-Kana","@value":"ニューラルネットワークモデル オ モチイタ キュウシュウ セイガンイキ ノ アビキ ヨソク ニ カンスル キソテキ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205320691968","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A Numerical Study on Long-Wave Generation and Propagation due to Atmospheric-Pressure Variation"},{"@language":"ja","@value":"気圧変動に伴う長周期波の発生・伝播過程の数値解析"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205320695424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Field Observation of Secondary Undulation \"Abiki\" in Urauchi Bay, Kami-Koshiki Island"},{"@language":"ja","@value":"上甑島浦内湾における「あびき」の現地観測"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205321818624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"冬季から春季にかけて東シナ海上を伝播する気象津波の発生源に関する解析"},{"@language":"en","@value":"Origins of Atmospheric Disturbance Resulted in Meteotsunamis propagated over the East China Sea in Winter and Spring Season"},{"@language":"ja-Kana","@value":"トウキ カラ シュンキ ニ カケテ ヒガシシナ カイジョウ オ デンパ スル キショウ ツナミ ノ ハッセイ ゲン ニ カンスル カイセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205352665216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"九州周辺海域におけるあびきの伝播，増幅に及ぼす微気圧変動および潮汐変動の影響について"},{"@language":"en","@value":"THE EFFECT OF SMALL FLUCTUATION OF ATOMOSPHERIC PRESSURE AND TIDE TO DEVELOPMENT OF SEICHE AROUND KYUSHU COASTAL AREA"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205352666752","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"鹿児島湾において夏季に発生する副振動の特徴"},{"@language":"en","@value":"SECONDARY UNDULATION OCCURRED IN KAGOSHIMA BAY DURING THE SUMMER SEASON"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205353848192","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"SECONDARY UNDULATION FORECAST IN THE WESTERN REGION OF KYUSHU USING SEA LEVEL DATA AT MESHIMA ISLAND"},{"@language":"ja","@value":"女島の水位データを用いた九州西岸域における副振動の発生予報に関する検討"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205353869952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"CONTROLLING EFFECTS ON SECONDARY UNDULATIONS BY PLACING BREAKWAERS IN A NARROW BRANCHED BAY"},{"@language":"ja","@value":"分岐した細長い湾における副振動対策としての防波堤設置の効果について"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205354015488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"PIV ANALYSIS OF ATMOSPHERIC PRESSURE DISTURBANCE OVER THE EAST CHINA SEA IN RELATION TO OCCURRENCE 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