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dc.contributor.authorGuida, Vincent G.  Concept link
dc.contributor.authorValentine, Page C.  Concept link
dc.contributor.authorGallea, Leslie B.  Concept link
dc.date.accessioned2013-04-04T15:48:18Z
dc.date.available2013-04-04T15:48:18Z
dc.date.issued2013-02-06
dc.identifier.citationPLoS ONE 8 (2013): e55273en_US
dc.identifier.urihttps://hdl.handle.net/1912/5832
dc.descriptionThis article is distributed under the terms of the Creative Commons Public Domain. The definitive version was published in PLoS ONE 8 (2013): e55273, doi:10.1371/journal.pone.0055273.en_US
dc.description.abstractGeorges Bank is a large, shallow feature separating the Gulf of Maine from the Atlantic Ocean. Previous studies demonstrated a strong tidal-mixing front during the warm season on the northern bank margin between thermally stratified water in the Gulf of Maine and mixed water on the bank. Tides transport warm water off the bank during flood tide and cool gulf water onto the bank during ebb tide. During 10 days in August 2009, we mapped frontal temperatures in five study areas along ~100 km of the bank margin. The seabed “frontal zone”, where temperature changed with frontal movment, experienced semidiurnal temperature maxima and minima. The tidal excursion of the frontal boundary between stratified and mixed water ranged 6 to 10 km. This “frontal boundary zone” was narrower than the frontal zone. Along transects perpendicular to the bank margin, seabed temperature change at individual sites ranged from 7.0°C in the frontal zone to 0.0°C in mixed bank water. At time series in frontal zone stations, changes during tidal cycles ranged from 1.2 to 6.1°C. The greatest rate of change (−2.48°C hr−1) occurred at mid-ebb. Geographic plots of seabed temperature change allowed the mapping of up to 8 subareas in each study area. The magnitude of temperature change in a subarea depended on its location in the frontal zone. Frontal movement had the greatest effect on seabed temperature in the 40 to 80 m depth interval. Subareas experiencing maximum temperature change in the frontal zone were not in the frontal boundary zone, but rather several km gulfward (off-bank) of the frontal boundary zone. These results provide a new ecological framework for examining the effect of tidally-driven temperature variability on the distribution, food resources, and reproductive success of benthic invertebrate and demersal fish species living in tidal front habitats.en_US
dc.description.sponsorshipThis study was supported by salary funds from the regular annual salary budget from Northeast Fisheries Science Center (NEFSC) and United States Geological Survey Woods Hole Coastal and Marine Science Center (USGS WH C&MSC), respectively; ship time funds from the NEFSC annual budget for days-at-sea ship operations; equipment from the NEFSC and USGS WH C&MSC annual equipment budgets.en_US
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen_US
dc.publisherPublic Library of Scienceen_US
dc.relation.urihttps://doi.org/10.1371/journal.pone.0055273
dc.rightsPublic Domain Dedication*
dc.rights.urihttp://creativecommons.org/publicdomain/zero/1.0/*
dc.titleSemidiurnal temperature changes caused by tidal front movements in the warm season in seabed habitats on the Georges Bank northern margin and their ecological implicationsen_US
dc.typeArticleen_US
dc.identifier.doi10.1371/journal.pone.0055273


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