{"@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/1363388845879470720.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.5194/nhess-6-1035-2006"}},{"identifier":{"@type":"URI","@value":"https://nhess.copernicus.org/articles/6/1035/2006/nhess-6-1035-2006.pdf"}}],"dc:title":[{"@value":"Meteotsunamis: atmospherically induced destructive ocean waves in the tsunami frequency band"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Abstract. In light of the recent enhanced activity in the study of tsunami waves and their source mechanisms, we consider tsunami-like waves that are induced by atmospheric processes rather than by seismic sources. These waves are mainly associated with atmospheric gravity waves, pressure jumps, frontal passages, squalls and other types of atmospheric disturbances, which normally generate barotropic ocean waves in the open ocean and amplify them near the coast through specific resonance mechanisms (Proudman, Greenspan, shelf, harbour). The main purpose of the present study is to describe this hazardous phenomenon, to show similarities and differences between seismic and meteorological tsunamis and to provide an overview of meteorological tsunamis in the World Ocean. It is shown that tsunamis and meteotsunamis have the same periods, same spatial scales, similar physical properties and affect the coast in a comparably destructive way. Some specific features of meteotsunamis make them akin to landslide-generated tsunamis. The generation efficiency of both phenomena depend on the Froude number (Fr), with resonance taking place when Fr~1.0. Meteotsunamis are much less energetic than seismic tsunamis and that is why they are always local, while seismic tsunamis can have globally destructive effects. Destructive meteotsunamis are always the result of a combination of several resonant factors; the low probability of such a combination is the main reason why major meteotsunamis are infrequent and observed only at some specific locations in the ocean.\n                    </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380017279854195458","@type":"Researcher","foaf:name":[{"@value":"S. Monserrat"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388845879470722","@type":"Researcher","foaf:name":[{"@value":"I. Vilibić"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388845879470720","@type":"Researcher","foaf:name":[{"@value":"A. B. Rabinovich"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"16849981"}],"prism:publicationName":[{"@value":"Natural Hazards and Earth System Sciences"}],"dc:publisher":[{"@value":"Copernicus GmbH"}],"prism:publicationDate":"2006-12-12","prism:volume":"6","prism:number":"6","prism:startingPage":"1035","prism:endingPage":"1051"},"reviewed":"false","dc:rights":["https://creativecommons.org/licenses/by-nc-sa/2.5/"],"url":[{"@id":"https://nhess.copernicus.org/articles/6/1035/2006/nhess-6-1035-2006.pdf"}],"createdAt":"2010-04-29","modifiedAt":"2021-01-29","relatedProduct":[{"@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 Subsequent Tsunami Waves in Japan Excited by Air Pressure Waves Due to the 2022 Tonga Volcanic Eruption"}]},{"@id":"https://cir.nii.ac.jp/crid/1050577818266683264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Ocean gravity waves generated by the meteotsunami at the Japan Trench following the 2022 Tonga volcanic eruption"}]},{"@id":"https://cir.nii.ac.jp/crid/1050585407782335232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Contribution of microtopography off the Ryukyu Islands to coastal sea-level amplification during the 2022 Tonga meteotsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017280668032640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunamis in Lingding Bay, China, caused by the 2022 Tonga volcanic eruption"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282208759808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Periodic sea-level oscillation in Tokyo Bay detected with the Tokyo-Bay seafloor hyper-kilometric submarine deep detector (TS-HKMSDD)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282433121792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ocean-Wave Gradiometry: Visualizing and Extracting Propagation Features of the 15 January 2022 Tsunami Wavefield with Dense Ocean-Bottom Pressure Gauge Arrays"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283690395850624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Field observations of meteotsunami locally called “abiki” in Urauchi Bay, Kami-Koshiki Island, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285706391566080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Abiki oscillations in Sakitsu Bay, west Kyushu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617673187712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Meteorological Tsunami Generation Due to Sea‐Surface Pressure Change: Three‐Dimensional Theory and Synthetics of Ocean‐Bottom Pressure Change"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294647368684160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Meteotsunami observed by the deep-ocean seafloor pressure gauge network off northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306906104282240","@type":"Article","resourceType":"学術雑誌論文(journal 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estimation of the tsunami later phases associated with the 2022 Hunga Tonga volcanic eruption"}]},{"@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/1390012313366440448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"CHARACTERISTICS OF INTENSIFICATION OF METEOROLOGICAL TSUNAMI IN OSAKA BAY CAUSED BY A MICROBAROMETRIC WAVE PROPAGATING NORTHEASTWARD, AND SENSITIVITY ON GRID RESOLUTION FOR NUMERICAL MODELING"},{"@language":"ja","@value":"北東進する微気圧波による大阪湾内の気象津波増幅特性とその評価に格子解像度が及ぼす影響"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680295879040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Spatial Variation of Damage due to Storm Surge and Waves during Typhoon Haiyan in the Philippines"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680296177280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Amplification factors of Abiki oscillations along the western coast of Kyushu Island"},{"@language":"ja","@value":"九州西岸域における副振動の増幅要因に関する一考察"},{"@language":"ja-Kana","@value":"キュウシュウ セイガンイキ ニ オケル フクシンドウ ノ ゾウフク ヨウイン ニ カンスル イチ コウサツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680296428416","@type":"Article","resourceType":"学術雑誌論文(journal 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