DELIVERABLE D2.1 - Ifremer

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Figure 10a. Temperature and Salinity at 1000m in the North Atlantic from the 27 th January 2010 Analysisin the Mercator operational oceanography system 1/12° Atlantic and Mediterranean Model (lowerresolution models 1/4° and 2° are also available covering a global domain, including the Nordic Seasand Arctic) www.mercator-ocean.fr.Figure 10b. Temperature at 700m in theNordic Seas and NE Atlantic from the 1stMarch analysis of the TOPAZ systemhttp://topaz.nersc.no/Barents Portal – a recent initiative has developed a joint Norwegian-Russianenvironmental data portal for the Barents Sea called BarentsPortal(www.barentsportal.com) as a support to environmental status reporting. This portaltakes an integrated approach including abiotic (hydrography, chemistry etc) andbiotic (seabird, fisheries etc) monitoring that allows a full ecosystem assessment to bemade. In particular for hydrography they include 7 standard sections that have beensampled for many decades (Figure 11).18
Figure 11. Barents Sea Standard Sections all of which collect T and S data, some of which also monitornutrients and plankton. A is fixed station Ingøy(1936-1944, 1968-present), B is Fugløya-Bear Island (since1977, 6 times per year), C is North Cape-Bear Island (since 1929, varying frequency), D is Vardø-North(since 1977, 4 times per year), E is Kola (since 1900, varying frequency), F is Sem Island-North(since1977, intermittently), G is Kanin section (since 1936, varying frequency) and H is Bear Island-East (since1936, varying frequency). www.barentsportal.com.Global datasets- There are a number of initiatives by the international sciencecommunity that aim to bring together as much of the hydrographic data collected aspossible, quality control them and make them available as a coherent dataset. Theprincipal of these are the World Ocean Database and its associated World OceanAtlas produced by the US National Oceanographic Data Center(www.nodc.noaa.gov/OC5/indprod.htm). The latest updates of these were made in2009 and are referred to as WOD09 and WOA09 (Boyer at al 2009) where the WOAshows the average and statistics of data within the database for chosen parametersand locations.A further step on are attempts to analyze these sparse data to form gridded fields. In2007, Ingleby and Huddleston described the methodology used to produce qualitycontrolled subsurface temperature and salinity data that is used to produce the EN3dataset (http://hadobs.metoffice.com/en3/). This dataset includes the monthlyobserved ocean temperature and salinity profiles taken by standard hydrographyand by floats since 1950 with an assessment of data quality and also the objectiveanalyses of all these data.19
Page 1 and 2: DEEPFISHMANManagement And Monitorin
Page 3 and 4: 1. Salient characteristics of the d
Page 5 and 6: DEEPFISHMAN case study fleet that p
Page 7 and 8: Figure 2. NE Atlantic - Deep (> 200
Page 9 and 10: Fracture zone, between the Greenlan
Page 11 and 12: Figure 4 Location of carbonate moun
Page 13 and 14: and the frequency of observation wh
Page 15 and 16: countries to make in-situ and satel
Page 17: Figure 9. One of the mooring arrays
Page 21 and 22: temperature and salinity, which are
Page 23 and 24: Figure 14. WOCE section A24S (the s
Page 25 and 26: Figure 15. WOCE section A24N (the n
Page 27 and 28: Figure 17. Modified from Stramma et
Page 29 and 30: that of the atmosphere on time scal
Page 31 and 32: Figure 21. Time-series from the Ice
Page 33 and 34: Figure 22. Height in cm of the prin
Page 35 and 36: Dickson et al (1996) found evidence
Page 37 and 38: global ocean leads to niche and res
Page 39 and 40: The combination of physical charact
Page 41 and 42: most dominant source of primary pro
Page 43 and 44: a framework for describing function
Page 45 and 46: Table 1. Classification scheme modi
Page 47 and 48: The primary production at hydrother
Page 49 and 50: ocean colonisation. Calcium carbona
Page 51 and 52: Figure 27. The distribution of cold
Page 53 and 54: The biological diversity of coral g
Page 55 and 56: The fauna associated with the spong
Page 57 and 58: The most species-rich environments
Page 59 and 60: 2.8.1. Ecosystem structureEcosystem
Page 61 and 62: In general, an indicator can be def
Page 63 and 64: Table 3. List of indicators from th
Page 65 and 66: affects the longevity of a given sp
Page 67 and 68: significant interactions between hu
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Define Appropriate SpatialManagemen
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flow of energy from primary produce
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disease is usually superficial and
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Atlantic). In none of these cases w
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complete lifecycles of deep-water d
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of other hosts, including Nototheni
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parasite within the tissues. It is
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Order Family Genus Number deepwater
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classifiers are combined by majorit
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information on stock status and fis
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Development. This resolution also c
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of populations, communities and hab
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over the increase of shark catches
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On the basis of specified criteria
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• the plans should also aim at di
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the industry to identify technical
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A requirement to land all fish will
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interactions and applying an integr
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equested Scientific, Technical and
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(4) all elements of the marine food
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e.g. control and safety at sea. In
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several stocks from recovering in s
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• disturbance to sea bed communit
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smooth oreo, 150t for other oreos,
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emit of the CCAMLR. Here, we focus
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on the high seas with the discovery
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stocks deeper than 600 m. There is
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target, the MEY (Maximum Economic Y
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Rebuilding strategies are developed
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stock biomass is below that limit i
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fishers to pay the charge requested
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ecent surveys have combined acousti
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Table 8. Main features of the manag
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Figure 40. Continental margin off B
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southeastern and southern coasts (2
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Table 9. Spatial distribution of de
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5.2.5. Fisheries-independent survey
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Annual catches increased from 13 t
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gillnets on large K-strategists (wr
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Table 12. Management elements of th
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Figure 41. Map of CCAMLR convention
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The essential problem with using su
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(c) prevention of changes or minimi
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(certified 2004, recertified with n
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VMS data are only available from 20
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target aggregations associated with
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All fishing activities for fisherie
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advises the Commission as to whethe
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Deep-water coral reefs are local se
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400 and 800 m (Cartes and Sardà, 1
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Red shrimp resources have shown som
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The official landings of the Italia
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The trawl fishery in the Greek Ioni
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In Turkish waters, although GFCM (2
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Italycomputerized yet and depends o
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Pagellus bogaraveo:Moderately explo
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opinion from some scientists from t
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5.6. North Atlantic (NAFO, NEAFC an
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speed above 8 knots to ensure that
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e introduced in Regulation 1359/200
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From a monitoring standpoint, the N
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(C/B) indices indicate show a decre
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set up for spatial protection measu
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measures designed to achieve of mai
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compiles an annual report on single
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6. Views of stakeholders in NE Atla
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Table 18. SWOT (Strengths, Weakness
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(a)(b)Nothing should changen = 42Ot
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The technical measures thought to b
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(a)StakeholdersNGOsCompetition othe
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of methods allowing structured and
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7. References (provisional)Blindhei
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De Forges BR, Koslow JA, Poore GCB
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Bakay,Y.I., 1988. Application of re
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Costa, V., Lourenco, H. M., Figueir
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Klimpel,S., Palm,H.W., Busch,M.W.,
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Pascoe,P.L., 1987. Monogenean paras
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Anderson, O.F. 2008. A summary of b
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Wayte S. 2004. Stock assessment of
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Perez, J.A.A., R. Wahrlich, P.R. Pe
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———. 2009. Report of the work
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Cartes, J.E. and Sardà, F., 1993.
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Moranta J., Palmer M., Massuti E.,
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Tursi, A., Matarrese, A., D' Onghia
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