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    Fishing and the oceanography of a stratied shelfsea

     Jonathan Sharples a,⇑, Jim R. Ellis b, Glenn Nolan c, Beth E. Scott d

    ABSTRACT

    Fishing essel position data !rom the "essel #onitoring S$stem %"#S& 'ere (sed toinestigate )shingactiit$ in the Celtic Sea, a seasonall$*strati!$ing, temperate region on the shel! o! north'est E(rope. The spatial pattern o! )shing sho'ed that three main areas are targeted+ %& the Celtic-eep %an areao! deeper 'ater 'ith )ne sediments&, %& the shel! edge, and %/& an area coering seerallarge seabedban0s in the central Celtic Sea. -ata !rom each o! these regions 'ere anal$sed toe1amine the contrastingseasonalit$ o! )shing actiit$, and to highlight 'here the spring*neap tidal c$cle appears

    to be importantto )shing. The oceanographic characteristics o! the Celtic Sea 'ere considered alongsidethe distrib(tionand timing o! )shing, ill(strating li0el$ contrasts in the (nderl$ing enironmental drierso! the di2erent)shed regions. 3n the central Celtic Sea, )shing mainl$ occ(rred d(ring the strati)edperiod bet'een Apriland A(g(st. Based on eidence proided in other papers o! this Special 3ss(e, 'e s(ggestthat the )shingin this area is s(pported b$ %& a broad increase in primar$ prod(ction ca(sed b$ lee*'aes generated b$seabed ban0s aro(nd spring tides driing large s(pplies o! n(trients into the photic 4one,and %& greater

    concentrations o! 4ooplan0ton 'ithin the region in5(enced b$ the seabed ban0s andeleated primar$prod(ction. 3n contrast, 'hile the shel! edge is a site o! eleated s(r!ace chloroph$ll,preio(s 'or0has s(ggested that the periodic mi1ing generated b$ an internal tide at the shel! edgealters the si4e6str(ct(re o! the ph$toplan0ton comm(nit$ 'hich )sh larae !rom the spa'ning stoc0salong the shel! edge are able to e1ploit. The )sher$ !or Nephrops noregic(s in the Celtic -eep 'as theonl$ one to sho'a signi)cant spring*neap c$cle, possibl$ lin0ed to Nephrops !oraging o(tside theirb(rro's less d(ringspring tides. #ore tentatiel$, the )sher$ !or Nephrops correlated most strongl$ 'ith a

    localised shi!tin the tidal c(rrent polarisation, s(ggesting that the m(dd$ seabed re7(ired b$ Nephropsis controlledb$ rotational constraints on the e1tent o! the bottom bo(ndar$ la$er.

    89/ The A(thors. :(blished b$ Elseier ;td. All rights resered.

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