2017
DOI: 10.1016/j.pocean.2015.03.008
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Possible link between interannual variation of neon flying squid (Ommastrephes bartramii) abundance in the North Pacific and the climate phase shift in 1998/1999

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Cited by 25 publications
(10 citation statements)
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“…We developed the MOVE‐3D model by adding several 3D ocean environmental parameters to the MOVE‐2D model. Firstly, we added MLD as an additional parameter since a previous study pointed out that MLD is one of the environmental factors that influence the neon flying squid habitats (Alabia et al., ), and it is assumed to affect the squid habitat via the nutrient‐rich water supply from lower layers of the ocean (Igarashi et al., ; Nishikawa et al., ). The MLD was estimated using vertical profiles of temperature and salinity derived from MOVE‐WNP.…”
Section: Resultsmentioning
confidence: 99%
“…We developed the MOVE‐3D model by adding several 3D ocean environmental parameters to the MOVE‐2D model. Firstly, we added MLD as an additional parameter since a previous study pointed out that MLD is one of the environmental factors that influence the neon flying squid habitats (Alabia et al., ), and it is assumed to affect the squid habitat via the nutrient‐rich water supply from lower layers of the ocean (Igarashi et al., ; Nishikawa et al., ). The MLD was estimated using vertical profiles of temperature and salinity derived from MOVE‐WNP.…”
Section: Resultsmentioning
confidence: 99%
“…Moreover, in the North Pacific, O . bartramii population is comprised of two seasonal spawning cohorts (winter-spring and autumn) with life histories extremely dependent on the variability of spatial and temporal features of the oceanographic environment [ 17 , 18 , 19 , 20 ]. For instance, the squids’ annual roundtrip north-south migration for feeding and spawning is linked with the northern warm-water branches and the warm-core rings of the Kuroshio Current [ 21 , 22 ].…”
Section: Introductionmentioning
confidence: 99%
“…Previous studies have described the spatial and temporal patterns of potential habitat of neon flying squid in response to dominant modes of high-frequency climate variability such as the El Niño Southern Oscillation (ENSO) [6,46,47]. Moreover, the impacts of the basin-wide regime shifts based on PDO patterns on relative abundances of autumn [7,8] and winter [35] cohorts of neon flying squid in the northwestern Pacific have been previously explored. Our analyses, however, focused on temporal habitat and environmental gradients in summer foraging zones of the autumn cohort (central Pacific; 160 • W-160 • E) under the contemporary PDO phase transitions, hence, affording insights into its distributional response to shifting climate and setting this work apart from previous studies.…”
Section: Discussionmentioning
confidence: 99%
“…bartramii population in the North Pacific Ocean encompasses two seasonal cohorts: winter-spring and autumn spawning groups [5]. Their spatial and temporal distributions are linked with the basin-wide oceanic circulation and their life history stages are highly responsive to the variability in ambient oceanographic regimes and concomitant changes in epipelagic environment [6][7][8]. Furthermore, both squid cohorts undergo extensive seasonal and meridional migrations between their spawning (subtropical region; 20-30 • N) and foraging sites (Kuroshio-Oyashio transition and subarctic frontal zones; 30-50 • N), within their brief 1-year life-span ( Figure 1A) [5,9,10].…”
Section: Introductionmentioning
confidence: 99%