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dc.contributor.author馬場, 康之ja
dc.contributor.author水谷, 英朗ja
dc.contributor.author久保, 輝広ja
dc.contributor.author内山, 雄介ja
dc.contributor.author森, 信人ja
dc.contributor.author渡部, 靖憲ja
dc.contributor.author山田, 朋人ja
dc.contributor.author猿渡, 亜由未ja
dc.contributor.author大塚, 淳一ja
dc.contributor.author二宮, 順一ja
dc.contributor.alternativeBABA, Yasuyukien
dc.contributor.alternativeMIZUTANI, Hideakien
dc.contributor.alternativeKUBO, Teruhiroen
dc.contributor.alternativeUCHIYAMA, Yusukeen
dc.contributor.alternativeMORI, Nobuhitoen
dc.contributor.alternativeWATANABE, Yasunorien
dc.contributor.alternativeYAMADA, Tomohitoen
dc.contributor.alternativeSARUWATARI, Ayumien
dc.contributor.alternativeOTSUKA, Junichien
dc.contributor.alternativeNINOMIYA, Junichien
dc.date.accessioned2016-11-15T01:15:44Z-
dc.date.available2016-11-15T01:15:44Z-
dc.date.issued2016-06-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/217281-
dc.description.abstractThis paper shows some results of a field observation carried out in the summer of 2015. The vertical profiles of currents and water temperature have been measured as well as wave and wind conditions, and salinity observations have been carried out at the observation tower of Shirahama Oceanographic Observatory. In the summer in 2015, no typhoon approached around the observation site, and the high wave and strong wind conditions have not been captured during the observation. Several short-term rainfalls due to front and low pressure occurred, and it is reported that local areas in Shirahama town and neighboring towns suffered some damages with windblasts from late August to early September. It is found in the observation results of water temperature that the temporal variations of water temperature have a period of 3 to 6 days in the deeper layers like 20m deep and 30m deep. The cyclical fluctuation of water temperature at 30m deep has opposite phase to the fluctuation of salinity. This result means that low temperature and high salinity water approaches to the observation site periodically and that some influences of the water mass of the open sea exist.en
dc.format.mimetypeapplication/pdf-
dc.language.isojpn-
dc.publisher京都大学防災研究所ja
dc.publisher.alternativeDisaster Prevention Research Institute, Kyoto Universityen
dc.subject現地観測ja
dc.subject台風ja
dc.subject海水温および塩分濃度の変動ja
dc.subjectField observationen
dc.subjectTyphoonen
dc.subjectVariations of water temperature and salinityen
dc.subject.ndc519.9-
dc.title田辺中島高潮観測塔における2015年夏季観測結果ja
dc.title.alternativeField Measurements at Tanabe-Nakashima Observation Tower in the Summer of 2015en
dc.typedepartmental bulletin paper-
dc.type.niitypeDepartmental Bulletin Paper-
dc.identifier.ncidAN00027784-
dc.identifier.jtitle京都大学防災研究所年報. Bja
dc.identifier.volume59-
dc.identifier.issueB-
dc.identifier.spage431-
dc.identifier.epage437-
dc.textversionpublisher-
dc.sortkey41-
dc.relation.urlhttp://www.dpri.kyoto-u.ac.jp/nenpo/nenpo.html-
dcterms.accessRightsopen access-
dc.identifier.pissn0386-412X-
dc.identifier.jtitle-alternativeDisaster Prevention Research Institute Annuals. Ben
出現コレクション:Vol.59 B

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