Changes
On October 22, 2024, 6:09:11 PM UTC,
-
Added resource 64PE529060_000000_osite_fhv21.nc to VMADCP data for validation of SCARIBOS model
| f | 1 | { | f | 1 | { |
| 2 | "author": null, | 2 | "author": null, | ||
| 3 | "author_email": null, | 3 | "author_email": null, | ||
| 4 | "code": "7b.b.xh", | 4 | "code": "7b.b.xh", | ||
| 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | ||
| 6 | "creator_user_id": "3c315d64-040e-4a62-b8a9-6e24c44cbbda", | 6 | "creator_user_id": "3c315d64-040e-4a62-b8a9-6e24c44cbbda", | ||
| 7 | "creators": | 7 | "creators": | ||
| 8 | a\",\"lastname\":\"Bertoncelj\",\"orcid\":null,\"affiliation\":\"Royal | 8 | a\",\"lastname\":\"Bertoncelj\",\"orcid\":null,\"affiliation\":\"Royal | ||
| 9 | Netherlands Institute for Sea | 9 | Netherlands Institute for Sea | ||
| 10 | ntactemailaddress\":\"vesna.bertoncelj@nioz.nl\",\"formatted\":\"Vesna | 10 | ntactemailaddress\":\"vesna.bertoncelj@nioz.nl\",\"formatted\":\"Vesna | ||
| 11 | Bertoncelj - Royal Netherlands Institute for Sea Research - ORCID: - | 11 | Bertoncelj - Royal Netherlands Institute for Sea Research - ORCID: - | ||
| 12 | Corresponding Author - vesna.bertoncelj@nioz.nl\"}]", | 12 | Corresponding Author - vesna.bertoncelj@nioz.nl\"}]", | ||
| 13 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.xh", | 13 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.xh", | ||
| 14 | "dates": "[{\"datefrom\":\"2024-01-04 | 14 | "dates": "[{\"datefrom\":\"2024-01-04 | ||
| 15 | 00:00:00.000\",\"dateto\":\"2024-01-20 | 15 | 00:00:00.000\",\"dateto\":\"2024-01-20 | ||
| 16 | \":\"collected\",\"information\":\"64PE529\",\"formatted\":\"collected | 16 | \":\"collected\",\"information\":\"64PE529\",\"formatted\":\"collected | ||
| 17 | from: 04/01/2024 to: 20/01/2024 64PE529\"}]", | 17 | from: 04/01/2024 to: 20/01/2024 64PE529\"}]", | ||
| 18 | "deposit_date": "2024-10-18", | 18 | "deposit_date": "2024-10-18", | ||
| 19 | "depositor": "Furu Mienis", | 19 | "depositor": "Furu Mienis", | ||
| 20 | "distribution_date": "2024-10-18", | 20 | "distribution_date": "2024-10-18", | ||
| 21 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 21 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 22 | Institute for Sea Research)", | 22 | Institute for Sea Research)", | ||
| 23 | "doi_date_published": "2024-10-18", | 23 | "doi_date_published": "2024-10-18", | ||
| 24 | "funding_references": | 24 | "funding_references": | ||
| 25 | er\":\"NWOCA.2019.003\",\"awardtitle\":\"SEALINK\",\"formatted\":\"NWO | 25 | er\":\"NWOCA.2019.003\",\"awardtitle\":\"SEALINK\",\"formatted\":\"NWO | ||
| 26 | - NWOCA.2019.003 - SEALINK\"}]", | 26 | - NWOCA.2019.003 - SEALINK\"}]", | ||
| 27 | "groups": [], | 27 | "groups": [], | ||
| 28 | "id": "27896c10-e60b-4fec-817e-a1a36b109385", | 28 | "id": "27896c10-e60b-4fec-817e-a1a36b109385", | ||
| 29 | "isopen": false, | 29 | "isopen": false, | ||
| 30 | "license_title": null, | 30 | "license_title": null, | ||
| 31 | "maintainer": null, | 31 | "maintainer": null, | ||
| 32 | "maintainer_email": null, | 32 | "maintainer_email": null, | ||
| 33 | "metadata_created": "2024-10-22T18:09:05.477501", | 33 | "metadata_created": "2024-10-22T18:09:05.477501", | ||
| n | 34 | "metadata_modified": "2024-10-22T18:09:10.429758", | n | 34 | "metadata_modified": "2024-10-22T18:09:11.249560", |
| 35 | "name": "7bbxh", | 35 | "name": "7bbxh", | ||
| 36 | "notes": "Bertoncelj et al. Ocean Sciences\n\nFlow patterns, | 36 | "notes": "Bertoncelj et al. Ocean Sciences\n\nFlow patterns, | ||
| 37 | hotspots and connectivity of land-derived substances at the sea | 37 | hotspots and connectivity of land-derived substances at the sea | ||
| 38 | surface of Cura\u00e7ao in the Southern Caribbean\n\nThe South | 38 | surface of Cura\u00e7ao in the Southern Caribbean\n\nThe South | ||
| 39 | Caribbean Island of Cura\u00e7ao is abundant in coral reef | 39 | Caribbean Island of Cura\u00e7ao is abundant in coral reef | ||
| 40 | communities, but they are declining. Land-derived nutrients and | 40 | communities, but they are declining. Land-derived nutrients and | ||
| 41 | pollutants are a potential contributing factor to this decline, as | 41 | pollutants are a potential contributing factor to this decline, as | ||
| 42 | these substances after entering the ocean, can be transported towards | 42 | these substances after entering the ocean, can be transported towards | ||
| 43 | reef sites by ocean currents. To study the movement of the substances | 43 | reef sites by ocean currents. To study the movement of the substances | ||
| 44 | and their potential impact on coral reefs, we developed SCARIBOS, a | 44 | and their potential impact on coral reefs, we developed SCARIBOS, a | ||
| 45 | fine-resolution hydrodynamic model of the South CARIBbean Ocean | 45 | fine-resolution hydrodynamic model of the South CARIBbean Ocean | ||
| 46 | System, with a 1/100\u00b0 resolution. SCARIBOS covers the period from | 46 | System, with a 1/100\u00b0 resolution. SCARIBOS covers the period from | ||
| 47 | April 2020 to March 2024 (excluding spin-up time) to analyse flow | 47 | April 2020 to March 2024 (excluding spin-up time) to analyse flow | ||
| 48 | patterns within that period around the close proximity of | 48 | patterns within that period around the close proximity of | ||
| 49 | Cura\u00e7ao. Furthermore, SCARIBOS is used as hydrodynamic input for | 49 | Cura\u00e7ao. Furthermore, SCARIBOS is used as hydrodynamic input for | ||
| 50 | Lagrangian particle tracking analysis with the Parcels framework, | 50 | Lagrangian particle tracking analysis with the Parcels framework, | ||
| 51 | where we assess the distribution of positively buoyant substances and | 51 | where we assess the distribution of positively buoyant substances and | ||
| 52 | explore connectivity within Cura\u00e7ao\u2019s coastlines as well as | 52 | explore connectivity within Cura\u00e7ao\u2019s coastlines as well as | ||
| 53 | with nearby regions of Aruba, Bonaire, the Venezuelan islands, and a | 53 | with nearby regions of Aruba, Bonaire, the Venezuelan islands, and a | ||
| 54 | portion of the Venezuelan mainland. Results reveal two dominant | 54 | portion of the Venezuelan mainland. Results reveal two dominant | ||
| 55 | processes: the northwest-directed Caribbean Current and weaker | 55 | processes: the northwest-directed Caribbean Current and weaker | ||
| 56 | cyclonic eddies moving in the opposite direction. These flow patterns | 56 | cyclonic eddies moving in the opposite direction. These flow patterns | ||
| 57 | influence hotspot locations of higher substance concentrations | 57 | influence hotspot locations of higher substance concentrations | ||
| 58 | observed during eddy events. Our analysis also highlights increased | 58 | observed during eddy events. Our analysis also highlights increased | ||
| 59 | particle accumulation of land-derived substances in the northwest of | 59 | particle accumulation of land-derived substances in the northwest of | ||
| 60 | Cura\u00e7ao, corresponding to the prevailing currents. While the | 60 | Cura\u00e7ao, corresponding to the prevailing currents. While the | ||
| 61 | focus is on land-derived nutrients and pollutants, this methodology | 61 | focus is on land-derived nutrients and pollutants, this methodology | ||
| 62 | can be extended to study other particle types such as plastic debris | 62 | can be extended to study other particle types such as plastic debris | ||
| 63 | and coral larvae, providing valuable insights for marine conservation | 63 | and coral larvae, providing valuable insights for marine conservation | ||
| 64 | efforts and environmental management.", | 64 | efforts and environmental management.", | ||
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| 66 | "num_tags": 2, | 66 | "num_tags": 2, | ||
| 67 | "organization": { | 67 | "organization": { | ||
| 68 | "approval_status": "approved", | 68 | "approval_status": "approved", | ||
| 69 | "created": "2024-10-22T06:06:56.074257", | 69 | "created": "2024-10-22T06:06:56.074257", | ||
| 70 | "description": "", | 70 | "description": "", | ||
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| 72 | "image_url": | 72 | "image_url": | ||
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| 75 | "name": "nioz", | 75 | "name": "nioz", | ||
| 76 | "state": "active", | 76 | "state": "active", | ||
| 77 | "title": "Royal Netherlands Institute for Sea Research", | 77 | "title": "Royal Netherlands Institute for Sea Research", | ||
| 78 | "type": "organization" | 78 | "type": "organization" | ||
| 79 | }, | 79 | }, | ||
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| 82 | "production_date": "2024-10-18", | 82 | "production_date": "2024-10-18", | ||
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| 175 | "state": "active", | 197 | "state": "active", | ||
| 176 | "subject": "Earth and Environmental Sciences", | 198 | "subject": "Earth and Environmental Sciences", | ||
| 177 | "tags": [ | 199 | "tags": [ | ||
| 178 | { | 200 | { | ||
| 179 | "display_name": "VMADCP", | 201 | "display_name": "VMADCP", | ||
| 180 | "id": "8ec40947-4093-4f6c-bf83-2e88479998a1", | 202 | "id": "8ec40947-4093-4f6c-bf83-2e88479998a1", | ||
| 181 | "name": "VMADCP", | 203 | "name": "VMADCP", | ||
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| 183 | "vocabulary_id": null | 205 | "vocabulary_id": null | ||
| 184 | }, | 206 | }, | ||
| 185 | { | 207 | { | ||
| 186 | "display_name": "validation", | 208 | "display_name": "validation", | ||
| 187 | "id": "d21ffdbb-b03e-48d8-abe7-efad917c3df1", | 209 | "id": "d21ffdbb-b03e-48d8-abe7-efad917c3df1", | ||
| 188 | "name": "validation", | 210 | "name": "validation", | ||
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| 190 | "vocabulary_id": null | 212 | "vocabulary_id": null | ||
| 191 | } | 213 | } | ||
| 192 | ], | 214 | ], | ||
| 193 | "title": "VMADCP data for validation of SCARIBOS model", | 215 | "title": "VMADCP data for validation of SCARIBOS model", | ||
| 194 | "type": "dataset", | 216 | "type": "dataset", | ||
| 195 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.xh", | 217 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.xh", | ||
| 196 | "version": "1" | 218 | "version": "1" | ||
| 197 | } | 219 | } |