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  "code": "7b.b.lb",
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  "code": "7b.b.lb",
            
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  "contributor": "NIOZ Royal Netherlands Institute for Sea Research",
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  "contributor": "NIOZ Royal Netherlands Institute for Sea Research",
            
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stname\":\"Corina\",\"lastname\":\"Brussaard\",\"affiliation\":\"Royal 
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stname\":\"Corina\",\"lastname\":\"Brussaard\",\"affiliation\":\"Royal 
            
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Netherlands Institute for Sea 
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Netherlands Institute for Sea 
            
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Research\",\"orcid\":\"0000-0002-6320-9229 
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Research\",\"orcid\":\"0000-0002-6320-9229 
            
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firstname\":\"Loes\",\"lastname\":\"Gerringa\",\"affiliation\":\"Royal 
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firstname\":\"Loes\",\"lastname\":\"Gerringa\",\"affiliation\":\"Royal 
            
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Netherlands Institute for Sea 
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Netherlands Institute for Sea 
            
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espondingauthor\":false},{\"firstname\":\"Mathijs\",\"lastname\":\"van 
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Manen\",\"affiliation\":\"Royal Netherlands Institute for Sea 
            
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iladdress\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Rob 
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iladdress\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Rob 
            
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Institute for Sea Research\",\"orcid\":\"0000-0002-3326-530X 
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Institute for Sea Research\",\"orcid\":\"0000-0002-3326-530X 
            
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laddress\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Ruud 
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laddress\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Ruud 
            
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\",\"lastname\":\"Groenewegen\",\"affiliation\":\"Royal Netherlands 
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\",\"lastname\":\"Groenewegen\",\"affiliation\":\"Royal Netherlands 
            
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Institute for Sea 
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Institute for Sea 
            
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  "dates": 
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  "dates": 
            
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-08-17T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"\"}]",
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  "deposit_date": "2021-01-14",
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  "deposit_date": "2021-01-14",
            
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  "depositor": "loes gerringa",
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  "depositor": "loes gerringa",
            
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  "distribution_date": "2021-01-14",
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  "distribution_date": "2021-01-14",
            
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  "distributor": "Research Data Management(NIOZ Royal Netherlands 
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  "distributor": "Research Data Management(NIOZ Royal Netherlands 
            
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Institute for Sea Research)",
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Institute for Sea Research)",
            
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  "doi_date_published": "2021-01-15",
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  "doi_date_published": "2021-01-15",
            
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  "funding_references": "[{\"name\":\"NWO\",\"awardnumber\":\"basic 
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funding\",\"awardtitle\":\"\"}]",
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funding\",\"awardtitle\":\"\"}]",
            
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  "geographic_coverage": "[{\"place\":\"NE Altlantic 
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  "geographic_coverage": "[{\"place\":\"NE Altlantic 
            
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\"longitude_1\":62.8,\"latitude_2\":-21.7545,\"longitude_2\":29.75}]",
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\"longitude_1\":62.8,\"latitude_2\":-21.7545,\"longitude_2\":29.75}]",
            
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  "metadata_created": "2024-10-22T09:45:11.516183",
            
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  "metadata_modified": "2024-10-22T16:41:27.369171",
            
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  "name": "7bblb",
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  "name": "7bblb",
            
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  "notes": "In this data file nutrient, DFe and raw CTD data are 
45
  "notes": "In this data file nutrient, DFe and raw CTD data are 
            
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available used for the paper \nDiapycnal mixing across the photic zone 
46
available used for the paper \nDiapycnal mixing across the photic zone 
            
47
of the NE-Atlantic.\nVariable physical conditions such as vertical 
47
of the NE-Atlantic.\nVariable physical conditions such as vertical 
            
48
turbulent exchange, internal wave and mesoscale eddy action, affect 
48
turbulent exchange, internal wave and mesoscale eddy action, affect 
            
49
the availability of light and nutrients for phytoplankton (unicellular 
49
the availability of light and nutrients for phytoplankton (unicellular 
            
50
algae) growth. It is hypothesized that changes in ocean temperature 
50
algae) growth. It is hypothesized that changes in ocean temperature 
            
51
may affect ocean vertical density stratification, which may hamper 
51
may affect ocean vertical density stratification, which may hamper 
            
52
vertical exchange. In order to quantify variations in physical 
52
vertical exchange. In order to quantify variations in physical 
            
53
conditions in the Northeast Atlantic Ocean, we sampled a latitudinal 
53
conditions in the Northeast Atlantic Ocean, we sampled a latitudinal 
            
54
transect along 17\u00b15\u00b0W between 30 and 63\u00b0N in summer. A 
54
transect along 17\u00b15\u00b0W between 30 and 63\u00b0N in summer. A 
            
55
shipborne Conductivity-Temperature-Depth CTD-instrumented package was 
55
shipborne Conductivity-Temperature-Depth CTD-instrumented package was 
            
56
used with a custom-made modification of the pump-inlet to minimize 
56
used with a custom-made modification of the pump-inlet to minimize 
            
57
detrimental effects of ship motions on its data. Thorpe-scale analysis 
57
detrimental effects of ship motions on its data. Thorpe-scale analysis 
            
58
was used to establish turbulence values for the upper 500 m from 3 to 
58
was used to establish turbulence values for the upper 500 m from 3 to 
            
59
6 profiles obtained in a short CTD-yoyo, 3 to 5 h after local sunrise. 
59
6 profiles obtained in a short CTD-yoyo, 3 to 5 h after local sunrise. 
            
60
From south to north, average temperature decreased together with 
60
From south to north, average temperature decreased together with 
            
61
stratification while turbulence values weakly increased or remained 
61
stratification while turbulence values weakly increased or remained 
            
62
constant. Vertical turbulent nutrient fluxes did not vary 
62
constant. Vertical turbulent nutrient fluxes did not vary 
            
63
significantly with stratification and latitude. This apparent lack of 
63
significantly with stratification and latitude. This apparent lack of 
            
64
correspondence between turbulent mixing and temperature is likely due 
64
correspondence between turbulent mixing and temperature is likely due 
            
65
to internal waves breaking (increased stratification can support more 
65
to internal waves breaking (increased stratification can support more 
            
66
internal waves), acting as a potential feed-back mechanism. As this 
66
internal waves), acting as a potential feed-back mechanism. As this 
            
67
feed-back mechanism mediates potential physical environment changes in 
67
feed-back mechanism mediates potential physical environment changes in 
            
68
temperature, global surface ocean warming may not affect the vertical 
68
temperature, global surface ocean warming may not affect the vertical 
            
69
nutrient fluxes to a large degree. We urge modelers to test this 
69
nutrient fluxes to a large degree. We urge modelers to test this 
            
70
deduction as it could imply that the future summer phytoplankton 
70
deduction as it could imply that the future summer phytoplankton 
            
71
productivity in stratified oligotrophic waters would experience little 
71
productivity in stratified oligotrophic waters would experience little 
            
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alterations in nutrient input from deeper waters.\n",
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alterations in nutrient input from deeper waters.\n",
            
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    {
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      "display_name": "dissolved Fe",
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      "display_name": "dissolved Fe",
            
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      "id": "270ed0d5-67db-4795-b144-92ef05c08076",
            
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      "name": "dissolved Fe",
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      "name": "dissolved Fe",
            
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      "state": "active",
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      "state": "active",
            
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      "vocabulary_id": null
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      "vocabulary_id": null
            
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    },
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    },
            
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    {
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    {
            
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      "display_name": "nutrients",
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      "display_name": "nutrients",
            
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      "id": "28bdb9b3-fb1d-4304-b1f2-cef16d09f4e9",
            
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      "name": "nutrients",
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      "name": "nutrients",
            
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      "state": "active",
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      "state": "active",
            
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      "vocabulary_id": null
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      "vocabulary_id": null
            
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    },
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    },
            
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    {
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    {
            
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      "display_name": "stratification",
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      "display_name": "stratification",
            
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      "id": "a0a1d5d7-2881-4bfb-96b5-89a9e8476a9f",
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      "id": "a0a1d5d7-2881-4bfb-96b5-89a9e8476a9f",
            
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      "name": "stratification",
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      "name": "stratification",
            
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      "state": "active",
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      "state": "active",
            
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      "vocabulary_id": null
            
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    },
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    },
            
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    {
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    {
            
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      "display_name": "vertical exchange",
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      "display_name": "vertical exchange",
            
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      "id": "43ad5f03-4227-4762-9739-83654e2048b1",
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      "id": "43ad5f03-4227-4762-9739-83654e2048b1",
            
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      "name": "vertical exchange",
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      "name": "vertical exchange",
            
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      "state": "active",
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      "state": "active",
            
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      "vocabulary_id": null
            
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    }
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    }
            
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  ],
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  ],
            
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  "title": "Diapycnal nutrient mixing",
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  "title": "Diapycnal nutrient mixing",
            
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  "type": "dataset",
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  "type": "dataset",
            
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  "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.lb",
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  "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.lb",
            
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  "version": "1"
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  "version": "1"
            
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}
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}