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| 02553nam 2200349za 4500 |
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001 | 9.801189 |
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003 | CaOODSP |
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005 | 20221107134741 |
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007 | cr ||||||||||| |
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008 | 150605s2015 bccd ob f000 0 eng d |
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020 | |a978-0-660-02512-4|z978-0-660-02511-7 |
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040 | |aCaOODSP|beng |
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041 | |aeng|bfre |
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043 | |an-cn--- |
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086 | 1 |aFs97-18/308E-PDF|zFs97-18/308E |
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100 | 1 |aJohannessen, S. C. |q(Sophia C.), |d1972- |
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245 | 10|aSeasonality and physical control of water properties and sinking and suspended particles in Douglas Channel, British Columbia |h[electronic resource] / |cS.C. Johannessen, C.A. Wright, and D.J. Spear. |
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246 | 33|aSaisonnalité et contrôle physique des propriétés de l'eau et des particules en suspension ou qui sombrent dans le chenal |
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260 | |aSidney, BC : |bFisheries and Oceans Canada, |c2015. |
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300 | |aiv, 26 p. : |bgraphs |
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490 | 1 |aCanadian technical report of hydrography and ocean sciences, |x1488-5417 ; |v308 |
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504 | |aIncludes bibliographical references (p. 12-13). |
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520 | |aWater properties and particles in Douglas Channel were characterized during four cruises (July 2013, April, July and October 2014), and with moored sensors and sediment traps (July 2013-June 2014.) An outflowing surface layer 10-30 m thick, driven by Kitimat and Kemano River discharge, overlay a mid-depth layer that exchanged with Hecate Strait. Deep-water renewal in June increased the concentration of oxygen by 1 mL/L to 3.5 mL/L. The surface layer was turbid (beam attenuation coefficient ≤6 m-1). The sinking particle flux at 50 m was 438 g m-2yr-1,and the organic carbon flux 37 gC m-2yr-1. Fluxes of particles and organic carbon peaked in late May, during the river freshet. The concentration of organic carbon in the sinking particles was highest in August and September (12-13%), except for a single peak in mid-November (22%). |
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530 | |aIssued also in printed form. |
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546 | |aText in English, abstract in English and French. |
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692 | 07|2gccst|aHydrography |
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700 | 1 |aWright, Cynthia. |
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700 | 1 |aSpear, D. J. |
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710 | 1 |aCanada. |bDepartment of Fisheries and Oceans. |
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776 | 0#|tSeasonality and physical control of water properties and sinking and suspended particles in Douglas Channel, British Columbia / |w(CaOODSP)9.801188 |
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830 | #0|aCanadian technical report of hydrography and ocean sciences,|x1488-5417 ; |v308.|w(CaOODSP)9.504781 |
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856 | 40|qPDF|s2.84 MB|uhttps://publications.gc.ca/collections/collection_2016/mpo-dfo/Fs97-18-308-eng.pdf |
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