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dc.contributor.authorRobinson, E
dc.contributor.authorHosegood, P
dc.contributor.authorBolton, A
dc.date.accessioned2023-09-27T10:46:45Z
dc.date.available2023-09-27T10:46:45Z
dc.date.issued2023-10-04
dc.identifier.issn1873-4472
dc.identifier.issn1873-4472
dc.identifier.other103129
dc.identifier.urihttps://pearl.plymouth.ac.uk/handle/10026.1/21344
dc.description.abstract

Physical oceanographic observations were made with subsurface, taut-line moorings at Egmont Island, a tropical atoll within the Chagos Archipelago in the central Indian Ocean, to elucidate the dynamics of near-bed cold-water intrusions implicated in driving local aggregations of reef manta rays (Mobula alfredi). Manta have been previously shown to aggregate within ‘Manta Alley’, a lipped gully at 65 m depth along the north coast, at times when the surface to bottom temperature difference was highest. We here identify the dynamical processes driving these temperature differences and shaping the foraging landscape at Egmont, and equivalent small-scale atolls, improving our understanding of manta behavior at hotspots where they are most vulnerable to exploitation.

The thermal regime within Manta Alley is shown to be governed at several spatiotemporal scales. The extreme 2019 Indian Ocean Dipole event drove a depression of the 26 °C isotherm to a depth of 115 m precluding the observation of cooling within the alley. As the thermocline shoaled with the change in phase of the IOD, near bed cold water flushing was seen with tidal periodicity within the gully. The internal tide is accompanied by high frequency internal waves with periods of O (5 min) which are shown to promote mixing through shear instability, evidenced by subcritical Richardson numbers, with surface-seabed temperature differences ∼4 °C observed throughout a tidal period.

Our results highlight a level of heterogeneity in oceanographic dynamics at sub-atoll spatial scales within an environment in which these processes are rarely resolved. Whilst the physical mechanisms through which these dynamics drive foraging within the resident manta population remain unclear, the generation of turbulence by high frequency internal wave events as shown here may influence zooplankton distributions, improving feeding efficiency at discrete locations within atolls. Our results thus highlight the need to account for fine scale changes in oceanographic conditions when attempting to explain habitat utilization by mobile species.

dc.format.extent103129-103129
dc.languageen
dc.publisherElsevier
dc.subjectInternal waves
dc.subjectPhysical oceanography
dc.subjectBiodiversity
dc.subjectLocal movements
dc.subjectIndian Ocean Dipole
dc.subjectChagos archipelago
dc.titleDynamical oceanographic processes impact on reef manta ray behaviour: Extreme Indian Ocean Dipole influence on local internal wave dynamics at a remote tropical atoll
dc.typejournal-article
dc.typeReview
plymouth.volume218
plymouth.publication-statusPublished
plymouth.journalProgress in Oceanography
dc.identifier.doi10.1016/j.pocean.2023.103129
plymouth.organisational-group|Plymouth
plymouth.organisational-group|Plymouth|Research Groups
plymouth.organisational-group|Plymouth|PRIMaRE Publications
plymouth.organisational-group|Plymouth|Faculty of Science and Engineering
plymouth.organisational-group|Plymouth|Faculty of Science and Engineering|School of Biological and Marine Sciences
plymouth.organisational-group|Plymouth|Research Groups|Marine Institute
plymouth.organisational-group|Plymouth|REF 2021 Researchers by UoA
plymouth.organisational-group|Plymouth|Users by role
plymouth.organisational-group|Plymouth|Users by role|Academics
plymouth.organisational-group|Plymouth|REF 2021 Researchers by UoA|UoA07 Earth Systems and Environmental Sciences
plymouth.organisational-group|Plymouth|Users by role|Researchers in ResearchFish submission
dcterms.dateAccepted2023-09-26
dc.date.updated2023-09-27T10:46:44Z
dc.rights.embargodate2023-10-21
dc.identifier.eissn1873-4472
dc.rights.embargoperiodforever
rioxxterms.versionofrecord10.1016/j.pocean.2023.103129


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