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| "author": null, | | "author": null, |
| "author_email": null, | | "author_email": null, |
| "code": "7b.b.lb", | | "code": "7b.b.lb", |
| "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", |
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| "creators": "[{\"firstname\":\"Hans\",\"lastname\":\"van | | "creators": "[{\"firstname\":\"Hans\",\"lastname\":\"van |
| Haren\",\"affiliation\":\"Royal Netherlands Institute for Sea | | Haren\",\"affiliation\":\"Royal Netherlands Institute for Sea |
| stname\":\"Corina\",\"lastname\":\"Brussaard\",\"affiliation\":\"Royal | | stname\":\"Corina\",\"lastname\":\"Brussaard\",\"affiliation\":\"Royal |
| Netherlands Institute for Sea | | Netherlands Institute for Sea |
| Research\",\"orcid\":\"0000-0002-6320-9229 | | Research\",\"orcid\":\"0000-0002-6320-9229 |
| firstname\":\"Loes\",\"lastname\":\"Gerringa\",\"affiliation\":\"Royal | | firstname\":\"Loes\",\"lastname\":\"Gerringa\",\"affiliation\":\"Royal |
| Netherlands Institute for Sea | | Netherlands Institute for Sea |
| espondingauthor\":false},{\"firstname\":\"Mathijs\",\"lastname\":\"van | | espondingauthor\":false},{\"firstname\":\"Mathijs\",\"lastname\":\"van |
| Manen\",\"affiliation\":\"Royal Netherlands Institute for Sea | | Manen\",\"affiliation\":\"Royal Netherlands Institute for Sea |
| iladdress\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Rob | | iladdress\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Rob |
| \",\"lastname\":\"Middag\",\"affiliation\":\"Royal Netherlands | | \",\"lastname\":\"Middag\",\"affiliation\":\"Royal Netherlands |
| Institute for Sea Research\",\"orcid\":\"0000-0002-3326-530X | | Institute for Sea Research\",\"orcid\":\"0000-0002-3326-530X |
| laddress\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Ruud | | laddress\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Ruud |
| \",\"lastname\":\"Groenewegen\",\"affiliation\":\"Royal Netherlands | | \",\"lastname\":\"Groenewegen\",\"affiliation\":\"Royal Netherlands |
| Institute for Sea | | Institute for Sea |
| :\"\",\"contactemailaddress\":\"\",\"iscorrespondingauthor\":false}]", | | :\"\",\"contactemailaddress\":\"\",\"iscorrespondingauthor\":false}]", |
| n | "dataset_persistent_id": "DOI:10.33591/nioz/7b.b.lb", | n | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.lb", |
| "dates": | | "dates": |
| -08-17T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"\"}]", | | -08-17T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"\"}]", |
| "deposit_date": "2021-01-14", | | "deposit_date": "2021-01-14", |
| "depositor": "loes gerringa", | | "depositor": "loes gerringa", |
| "distribution_date": "2021-01-14", | | "distribution_date": "2021-01-14", |
| "distributor": "Research Data Management(NIOZ Royal Netherlands | | "distributor": "Research Data Management(NIOZ Royal Netherlands |
| Institute for Sea Research)", | | Institute for Sea Research)", |
| "doi_date_published": "2021-01-15", | | "doi_date_published": "2021-01-15", |
| "funding_references": "[{\"name\":\"NWO\",\"awardnumber\":\"basic | | "funding_references": "[{\"name\":\"NWO\",\"awardnumber\":\"basic |
| funding\",\"awardtitle\":\"\"}]", | | funding\",\"awardtitle\":\"\"}]", |
| "geographic_coverage": "[{\"place\":\"NE Altlantic | | "geographic_coverage": "[{\"place\":\"NE Altlantic |
| \"longitude_1\":62.8,\"latitude_2\":-21.7545,\"longitude_2\":29.75}]", | | \"longitude_1\":62.8,\"latitude_2\":-21.7545,\"longitude_2\":29.75}]", |
| "groups": [], | | "groups": [], |
| "id": "c41bb32e-93e4-42bf-b5e1-e6ae78a1f82e", | | "id": "c41bb32e-93e4-42bf-b5e1-e6ae78a1f82e", |
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| "license_title": null, | | "license_title": null, |
| "maintainer": null, | | "maintainer": null, |
| "maintainer_email": null, | | "maintainer_email": null, |
| "metadata_created": "2024-10-22T09:45:11.516183", | | "metadata_created": "2024-10-22T09:45:11.516183", |
| n | "metadata_modified": "2024-10-22T09:45:12.826029", | n | "metadata_modified": "2024-10-22T16:41:23.595016", |
| "name": "7bblb", | | "name": "7bblb", |
| "notes": "In this data file nutrient, DFe and raw CTD data are | | "notes": "In this data file nutrient, DFe and raw CTD data are |
| n | available used for the paper \n\"Diapycnal mixing across the photic | n | available used for the paper \nDiapycnal mixing across the photic zone |
| zone of the NE-Atlantic\".\nVariable physical conditions such as | | of the NE-Atlantic.\nVariable physical conditions such as vertical |
| vertical turbulent exchange, internal wave and mesoscale eddy action, | | turbulent exchange, internal wave and mesoscale eddy action, affect |
| affect the availability of light and nutrients for phytoplankton | | the availability of light and nutrients for phytoplankton (unicellular |
| (unicellular algae) growth. It is hypothesized that changes in ocean | | algae) growth. It is hypothesized that changes in ocean temperature |
| temperature may affect ocean vertical density stratification, which | | may affect ocean vertical density stratification, which may hamper |
| may hamper vertical exchange. In order to quantify variations in | | vertical exchange. In order to quantify variations in physical |
| physical conditions in the Northeast Atlantic Ocean, we sampled a | | conditions in the Northeast Atlantic Ocean, we sampled a latitudinal |
| latitudinal transect along 17 degrees 5minutes W between 30 and 63 | | transect along 17\u00b15\u00b0W between 30 and 63\u00b0N in summer. A |
| degrees N in summer. A shipborne Conductivity-Temperature-Depth | | shipborne Conductivity-Temperature-Depth CTD-instrumented package was |
| CTD-instrumented package was used with a custom-made modification of | | used with a custom-made modification of the pump-inlet to minimize |
| the pump-inlet to minimize detrimental effects of ship motions on its | | detrimental effects of ship motions on its data. Thorpe-scale analysis |
| data. Thorpe-scale analysis was used to establish turbulence values | | was used to establish turbulence values for the upper 500 m from 3 to |
| for the upper 500 m from 3 to 6 profiles obtained in a short CTD-yoyo, | | 6 profiles obtained in a short CTD-yoyo, 3 to 5 h after local sunrise. |
| 3 to 5 h after local sunrise. From south to north, average temperature | | From south to north, average temperature decreased together with |
| decreased together with stratification while turbulence values weakly | | stratification while turbulence values weakly increased or remained |
| increased or remained constant. Vertical turbulent nutrient fluxes did | | constant. Vertical turbulent nutrient fluxes did not vary |
| not vary significantly with stratification and latitude. This apparent | | significantly with stratification and latitude. This apparent lack of |
| lack of correspondence between turbulent mixing and temperature is | | correspondence between turbulent mixing and temperature is likely due |
| likely due to internal waves breaking (increased stratification can | | to internal waves breaking (increased stratification can support more |
| support more internal waves), acting as a potential feed-back | | internal waves), acting as a potential feed-back mechanism. As this |
| mechanism. As this feed-back mechanism mediates potential physical | | feed-back mechanism mediates potential physical environment changes in |
| environment changes in temperature, global surface ocean warming may | | temperature, global surface ocean warming may not affect the vertical |
| not affect the vertical nutrient fluxes to a large degree. We urge | | nutrient fluxes to a large degree. We urge modelers to test this |
| modelers to test this deduction as it could imply that the future | | deduction as it could imply that the future summer phytoplankton |
| summer phytoplankton productivity in stratified oligotrophic waters | | productivity in stratified oligotrophic waters would experience little |
| would experience little alterations in nutrient input from deeper | | alterations in nutrient input from deeper waters.\n", |
| waters.", | | |
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| "organization": { | | "organization": { |
| "approval_status": "approved", | | "approval_status": "approved", |
| "created": "2024-10-22T06:06:56.074257", | | "created": "2024-10-22T06:06:56.074257", |
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| "name": "nioz", | | "name": "nioz", |
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| "production_date": "2021-01-15", | | "production_date": "2021-01-15", |
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| "subject": "Earth and Environmental Sciences", | | "subject": "Earth and Environmental Sciences", |
| "tags": [ | | "tags": [ |
| { | | { |
| "display_name": "NE Atlantic Ocean", | | "display_name": "NE Atlantic Ocean", |
| "id": "3a8c2eac-3b78-4a54-8aae-1f7045b03aff", | | "id": "3a8c2eac-3b78-4a54-8aae-1f7045b03aff", |
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| "display_name": "stratification", | | "display_name": "stratification", |
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| "display_name": "vertical exchange", | | "display_name": "vertical exchange", |
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| ], | | ], |
| "title": "Diapycnal nutrient mixing", | | "title": "Diapycnal nutrient mixing", |
| "type": "dataset", | | "type": "dataset", |
| t | "url": "https://dataportal.nioz.nl/doi/10.33591/nioz/7b.b.lb", | t | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.lb", |
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