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| "author": null, | | "author": null, |
| "author_email": null, | | "author_email": null, |
| "code": "7b.b.zf", | | "code": "7b.b.zf", |
| "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", |
| "creator_user_id": "7971cdd7-a042-49be-b21c-5b1b6dc17378", | | "creator_user_id": "7971cdd7-a042-49be-b21c-5b1b6dc17378", |
| "creators": | | "creators": |
| \":\"Fried\",\"orcid\":\"0000-0001-5457-1026\",\"affiliation\":\"Royal | | \":\"Fried\",\"orcid\":\"0000-0001-5457-1026\",\"affiliation\":\"Royal |
| Netherlands Institute for Sea | | Netherlands Institute for Sea |
| ondingauthor\":true,\"contactemailaddress\":\"nora.fried@nioz.nl\"}]", | | ondingauthor\":true,\"contactemailaddress\":\"nora.fried@nioz.nl\"}]", |
| n | "dataset_persistent_id": "DOI:10.33591/nioz/7b.b.zf", | n | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.zf", |
| "deposit_date": "2023-09-11", | | "deposit_date": "2023-09-11", |
| "depositor": "Nora Fried", | | "depositor": "Nora Fried", |
| "distribution_date": "2023-09-11", | | "distribution_date": "2023-09-11", |
| "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": "2023-11-14", | | "doi_date_published": "2023-11-14", |
| "groups": [], | | "groups": [], |
| "id": "a523df17-914d-4d33-b012-64554169c11c", | | "id": "a523df17-914d-4d33-b012-64554169c11c", |
| "isopen": false, | | "isopen": false, |
| "license_title": null, | | "license_title": null, |
| "maintainer": null, | | "maintainer": null, |
| "maintainer_email": null, | | "maintainer_email": null, |
| "metadata_created": "2024-10-22T11:54:38.383220", | | "metadata_created": "2024-10-22T11:54:38.383220", |
| n | "metadata_modified": "2024-10-22T11:54:40.187040", | n | "metadata_modified": "2024-10-22T17:30:35.349351", |
| "name": "7bbzf", | | "name": "7bbzf", |
| "notes": "The dataset contains particle tracks along the OSNAP East | | "notes": "The dataset contains particle tracks along the OSNAP East |
| line in the Irminger Sea (from Cape Farewell to the top of the | | line in the Irminger Sea (from Cape Farewell to the top of the |
| Reykjanes Ridge) using OceanParcels within the ocean-only model POP. | | Reykjanes Ridge) using OceanParcels within the ocean-only model POP. |
| We release particles every day for one year and track them backwards | | We release particles every day for one year and track them backwards |
| in time for five years to identify pathways and sources of the | | in time for five years to identify pathways and sources of the |
| Irminger Current. In the vertical particles are released every 50 | | Irminger Current. In the vertical particles are released every 50 |
| meters from the surface to 2000 meters depth. In the horizontal the | | meters from the surface to 2000 meters depth. In the horizontal the |
| spacing is approximately 6km. The data were saved in netcdf formats | | spacing is approximately 6km. The data were saved in netcdf formats |
| n | and are published here as matfiles (*parcles_backward*.mat). netCDF | n | and are published here as matfiles. netCDF files can be accessed upon |
| files can be accessed upon request. Python code on the particle | | request. Python code on the particle tracking is published as well.", |
| tracking is published as well.\n\nFor the study we performed the | | |
| following processing:\nAfter tracking for one year, we perform a | | |
| quality control procedure on the particle tracks to check for | | |
| particles that display unrealistic behavior, in particular particles | | |
| that unexpectedly stop moving which might be related to the tracking | | |
| software. When that occurs, we exclude the remainder of the track. | | |
| \nWe only include particle tracks longer than 50 days. As our goal is | | |
| to identify the potential different sources of the two Irminger | | |
| Current cores we need to make sure that tracks are sufficiently long | | |
| to travel from the Iceland Basin to the release location. Preliminary | | |
| analyses showed more than 90% of the particles coming from the Iceland | | |
| Basin cross the Reykjanes Ridge and reach the release location within | | |
| less than 50 days. \nThose files are saved as *cleaned_files.mat.", | | |
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| "num_tags": 5, | | "num_tags": 5, |
| "organization": { | | "organization": { |
| "approval_status": "approved", | | "approval_status": "approved", |
| "created": "2024-10-22T06:06:56.074257", | | "created": "2024-10-22T06:06:56.074257", |
| "description": "", | | "description": "", |
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| "is_organization": true, | | "is_organization": true, |
| "name": "nioz", | | "name": "nioz", |
| "state": "active", | | "state": "active", |
| "title": "Royal Netherlands Institute for Sea Research", | | "title": "Royal Netherlands Institute for Sea Research", |
| "type": "organization" | | "type": "organization" |
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| "subject": "Earth and Environmental Sciences", | | "subject": "Earth and Environmental Sciences", |
| "tags": [ | | "tags": [ |
| { | | { |
| "display_name": "Irminger Current", | | "display_name": "Irminger Current", |
| "id": "47a1e0c5-8e84-4890-b07d-1f1e19468e75", | | "id": "47a1e0c5-8e84-4890-b07d-1f1e19468e75", |
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| "state": "active", | | "state": "active", |
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| "title": "Lagrangian Particle tracks in the Irminger Current using | | "title": "Lagrangian Particle tracks in the Irminger Current using |
| OceanParcels within the ocean model POP", | | OceanParcels within the ocean model POP", |
| "type": "dataset", | | "type": "dataset", |
| t | "url": "https://dataportal.nioz.nl/doi/10.33591/nioz/7b.b.zf", | t | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.zf", |
| "version": "2" | | "version": "1" |
| } | | } |