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| 03888cam 2200553zi 4500 |
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001 | 9.923547 |
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003 | CaOODSP |
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005 | 20230614153517 |
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006 | m o d f |
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007 | cr mn||||||||| |
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008 | 230606t20232023nscab ob f000 0 eng d |
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020 | |a9780660490243 |
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040 | |aCaOODSP|beng|erda|cCaOODSP |
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041 | 0 |aeng|beng|bfre |
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043 | |an-cn---|an-us-ak|aln-----|ar------|apn----- |
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045 | |ax5y2 |
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086 | 1 |aFs97-18/355E-PDF |
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100 | 1 |aMcKee, Erin, |eauthor. |
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245 | 10|aEvaluation of bottom temperature from GLORYS12 and EN4 for North American continental shelf waters : |bfrom the North Atlantic, to the Arctic, to the North Pacific Oceans / |cby Erin Mckee, Zeliang Wang, and Brendan DeTracey. |
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264 | 1|aDartmouth, N.S., Canada : |bOcean and Ecosystem Sciences Division, Maritimes Region, Fisheries and Oceans Canada, Bedford Institute of Oceanography, |c2023. |
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264 | 4|c©2023 |
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300 | |a1 online resource (vii, 34 pages) : |bcolour illustrations, colour maps. |
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336 | |atext|btxt|2rdacontent |
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337 | |acomputer|bc|2rdamedia |
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338 | |aonline resource|bcr|2rdacarrier |
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490 | 1 |aCanadian technical report of hydrography and ocean sciences, |x1488-5417 ; |v355 |
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504 | |aIncludes bibliographical references (pages 32-34). |
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520 | 3 |a"Bottom temperature data is an important determinant for the distribution of many marine species. A scarcity of bottom temperature observations in Canadian shelf waters often leads to the use of ocean models and products as alternative sources of data. However, the performance of these products through validation with collected observations is not frequently conducted. We validated the ocean products EN4 and GLORYS12 using available bottom temperature observational data as a baseline comparison. Model bias, correlation, standard deviations, and trends were evaluated for eight regions of the Canadian/North American shelves: the Scotian Shelf, Gulf of St. Lawrence, Newfoundland Shelf, Labrador Shelf, Chukchi Sea, Bering Sea, Alaska Shelf, and the British Columbia Shelf. GLORSY12 out-performed the EN4 product in all regions assessed with the exception of the Gulf of St. Lawrence. Our analyses suggest that regionally averaged bottom temperature of the GLORYS12 could better represent the observed regional mean than the comparison for individual stations"--Abstract, page vi. |
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546 | |aIncludes abstracts in English and French. |
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650 | 0|aOcean bottom temperature|zScotian Shelf. |
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650 | 0|aOcean bottom temperature|zSaint Lawrence, Gulf of. |
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650 | 0|aOcean bottom temperature|zNewfoundland and Labrador|zAtlantic Coast. |
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650 | 0|aOcean bottom temperature|zChukchi Sea. |
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650 | 0|aOcean bottom temperature|zAlaska|zBering Sea Coast. |
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650 | 0|aOcean bottom temperature|zAlaska|zPacific Coast. |
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650 | 0|aOcean bottom temperature|zBritish Columbia|zPacific Coast. |
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650 | 0|aTime-series analysis. |
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650 | 6|aFonds marins|xTempérature|zNéo-écossaise, Plateforme. |
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650 | 6|aFonds marins|xTempérature|zSaint-Laurent, Golfe du. |
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650 | 6|aFonds marins|xTempérature|zTerre-Neuve-et-Labrador|zAtlantique, Côte de l'. |
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650 | 6|aFonds marins|xTempérature|zTchouktches, Mer des. |
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650 | 6|aFonds marins|xTempérature|zAlaska|zBéring, Côte de la mer de. |
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650 | 6|aFonds marins|xTempérature|zAlaska|zPacifique, Côte du. |
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650 | 6|aFonds marins|xTempérature|zColombie-Britannique|zPacifique, Côte du. |
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650 | 6|aSérie chronologique. |
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710 | 1 |aCanada. |bDepartment of Fisheries and Oceans, |eissuing body. |
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710 | 2 |aBedford Institute of Oceanography, |eissuing body. |
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830 | #0|aCanadian technical report of hydrography and ocean sciences ;|v355.|w(CaOODSP)9.504781 |
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856 | 40|qPDF|s2.13 MB|uhttps://publications.gc.ca/collections/collection_2023/mpo-dfo/Fs97-18-355-eng.pdf |
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