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  1. National Taiwan Ocean University Research Hub
  2. 海洋科學與資源學院
  3. 環境生物與漁業科學學系
Please use this identifier to cite or link to this item: http://scholars.ntou.edu.tw/handle/123456789/22197
DC FieldValueLanguage
dc.contributor.authorWu, Yan-Lunen_US
dc.contributor.authorLan, Kuo-Weien_US
dc.contributor.authorEvans, Karenen_US
dc.contributor.authorChang, Yi-Jayen_US
dc.contributor.authorChan, Jui-Wenen_US
dc.date.accessioned2022-09-20T02:25:46Z-
dc.date.available2022-09-20T02:25:46Z-
dc.date.issued2022-08-12-
dc.identifier.issn2045-2322-
dc.identifier.urihttp://scholars.ntou.edu.tw/handle/123456789/22197-
dc.description.abstractSpatial variations in tuna population and abundance are strongly linked to large-scale climate fluctuations, such as the Pacific decadal oscillation (PDO) and Atlantic multidecadal oscillation (AMO). However, the mechanisms underlying the association of climate indices with yellowfin tuna (YFT) abundance and habitat preference remain unclear. We analysed long-term longline fishery data for YFT and oceanic climate variability index data for 1971-2018. The standardized catch per unit effort (CPUE) of Indo-Pacific Ocean YFT was higher during negative AMO and positive PDO phases. In tropical Pacific Ocean, the trend of YFT habitat preference exhibited seesaw patterns because of the distinct environmental factors influenced by the PDO phase. The PDO changed the environmental parameters throughout the tropical Indian Ocean such that the habitat preference of YFT remained consistent throughout. However, the variations in habitat suitability did not correspond to the distribution or standardized CPUE of YFT throughout the Pacific Ocean during AMO events. Moreover, the changes in habitat suitability had a positive periodicity of 8-16 years with AMO in the Indian Ocean, but revealed opposite trends with the distribution or standardized CPUE of YFT. Our results provide sufficient information to distinguish the variations between PDO phase changing and YFT standardized CPUE/ habitat preference. Furthermore, the AMO phase shift period 60-100 years longer than that of the PDO (20-30 years), and models employing time series of fishery and environmental data must be extended the time period of our study to make the AMO match the fishery data more complete.en_US
dc.language.isoen_USen_US
dc.publisherNATURE PORTFOLIOen_US
dc.relation.ispartofSCI REP-UKen_US
dc.subjectTHUNNUS-ALBACARESen_US
dc.subjectHABITAT SUITABILITYen_US
dc.subjectOCEANen_US
dc.subjectOSCILLATIONen_US
dc.subjectTEMPERATUREen_US
dc.subjectDYNAMICSen_US
dc.subjectWESTERNen_US
dc.subjectMARINEen_US
dc.subjectPREFERENCESen_US
dc.subjectBEHAVIORen_US
dc.titleEffects of decadal climate variability on spatiotemporal distribution of Indo-Pacific yellowfin tuna populationen_US
dc.typejournal articleen_US
dc.identifier.doi10.1038/s41598-022-17882-w-
dc.identifier.isiWOS:000840132800069-
dc.relation.journalvolume12en_US
dc.relation.journalissue1en_US
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
item.cerifentitytypePublications-
item.languageiso639-1en_US-
item.fulltextno fulltext-
item.grantfulltextnone-
item.openairetypejournal article-
crisitem.author.deptCollege of Ocean Science and Resource-
crisitem.author.deptDepartment of Environmental Biology and Fisheries Science-
crisitem.author.deptNational Taiwan Ocean University,NTOU-
crisitem.author.orcid0000-0002-2637-2932-
crisitem.author.parentorgNational Taiwan Ocean University,NTOU-
crisitem.author.parentorgCollege of Ocean Science and Resource-
Appears in Collections:14 LIFE BELOW WATER
15 LIFE ON LAND
環境生物與漁業科學學系
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