Changes
On August 30, 2025, 8:14:55 AM UTC,
-
Added resource 64PE529-14CTD01.cnv to Depth, potential T, practical S, density data 64PE529
| f | 1 | { | f | 1 | { |
| 2 | "author": "Furu Mienis (Royal Netherlands Institute for Sea | 2 | "author": "Furu Mienis (Royal Netherlands Institute for Sea | ||
| 3 | Research)", | 3 | Research)", | ||
| 4 | "author_email": "furu.mienis@nioz.nl", | 4 | "author_email": "furu.mienis@nioz.nl", | ||
| 5 | "code": "7b.b.1j", | 5 | "code": "7b.b.1j", | ||
| 6 | "contributor": "Royal Netherlands Institute for Sea Research | 6 | "contributor": "Royal Netherlands Institute for Sea Research | ||
| 7 | (NIOZ)", | 7 | (NIOZ)", | ||
| 8 | "creator_user_id": "e0aae3b1-c805-4be7-819b-8ae1f478dca4", | 8 | "creator_user_id": "e0aae3b1-c805-4be7-819b-8ae1f478dca4", | ||
| 9 | "creators": | 9 | "creators": | ||
| 10 | "Furu\",\"lastname\":\"Mienis\",\"orcid\":null,\"affiliation\":\"Royal | 10 | "Furu\",\"lastname\":\"Mienis\",\"orcid\":null,\"affiliation\":\"Royal | ||
| 11 | Netherlands Institute for Sea | 11 | Netherlands Institute for Sea | ||
| 12 | e,\"contactemailaddress\":\"furu.mienis@nioz.nl\",\"formatted\":\"Furu | 12 | e,\"contactemailaddress\":\"furu.mienis@nioz.nl\",\"formatted\":\"Furu | ||
| 13 | Mienis - Royal Netherlands Institute for Sea Research - ORCID: - | 13 | Mienis - Royal Netherlands Institute for Sea Research - ORCID: - | ||
| 14 | Corresponding Author - | 14 | Corresponding Author - | ||
| 15 | a\",\"lastname\":\"Bertoncelj\",\"orcid\":null,\"affiliation\":\"Royal | 15 | a\",\"lastname\":\"Bertoncelj\",\"orcid\":null,\"affiliation\":\"Royal | ||
| 16 | Netherlands Institute for Sea | 16 | Netherlands Institute for Sea | ||
| 17 | ondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Vesna | 17 | ondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Vesna | ||
| 18 | Bertoncelj - Royal Netherlands Institute for Sea Research - ORCID: | 18 | Bertoncelj - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 19 | \"}]", | 19 | \"}]", | ||
| 20 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.1j", | 20 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.1j", | ||
| 21 | "deposit_date": "2025-08-30", | 21 | "deposit_date": "2025-08-30", | ||
| 22 | "depositor": "Furu Mienis (furu.mienis@nioz.nl)", | 22 | "depositor": "Furu Mienis (furu.mienis@nioz.nl)", | ||
| 23 | "distribution_date": "2025-08-30", | 23 | "distribution_date": "2025-08-30", | ||
| 24 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 24 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 25 | Institute for Sea Research)", | 25 | Institute for Sea Research)", | ||
| 26 | "doi_date_published": "2025-08-30T10:13:52.170364", | 26 | "doi_date_published": "2025-08-30T10:13:52.170364", | ||
| 27 | "funding_references": | 27 | "funding_references": | ||
| 28 | er\":\"NWOCA.2019.003\",\"awardtitle\":\"Sealink\",\"formatted\":\"NWO | 28 | er\":\"NWOCA.2019.003\",\"awardtitle\":\"Sealink\",\"formatted\":\"NWO | ||
| 29 | - NWOCA.2019.003 - Sealink\"}]", | 29 | - NWOCA.2019.003 - Sealink\"}]", | ||
| 30 | "groups": [], | 30 | "groups": [], | ||
| 31 | "id": "cfd0527b-ae45-42e1-a648-67a3902ebea5", | 31 | "id": "cfd0527b-ae45-42e1-a648-67a3902ebea5", | ||
| 32 | "isopen": false, | 32 | "isopen": false, | ||
| 33 | "license_title": null, | 33 | "license_title": null, | ||
| 34 | "maintainer": "Furu", | 34 | "maintainer": "Furu", | ||
| 35 | "maintainer_email": "furu.mienis@nioz.nl", | 35 | "maintainer_email": "furu.mienis@nioz.nl", | ||
| 36 | "metadata_created": "2025-08-30T08:14:24.484818", | 36 | "metadata_created": "2025-08-30T08:14:24.484818", | ||
| n | 37 | "metadata_modified": "2025-08-30T08:14:55.236215", | n | 37 | "metadata_modified": "2025-08-30T08:14:55.625113", |
| 38 | "name": "depth", | 38 | "name": "depth", | ||
| 39 | "notes": "Shallow-water coral reef ecosystems are positioned at the | 39 | "notes": "Shallow-water coral reef ecosystems are positioned at the | ||
| 40 | critical interface between terrestrial and marine environments, where | 40 | critical interface between terrestrial and marine environments, where | ||
| 41 | ocean circulation patterns control the delivery and distribution of | 41 | ocean circulation patterns control the delivery and distribution of | ||
| 42 | nutrients and land-derived substances. This study examines | 42 | nutrients and land-derived substances. This study examines | ||
| 43 | three-dimensional circulation patterns around Cura\u00e7ao, a southern | 43 | three-dimensional circulation patterns around Cura\u00e7ao, a southern | ||
| 44 | Caribbean reef island, using Lagrangian particle tracking analysis | 44 | Caribbean reef island, using Lagrangian particle tracking analysis | ||
| 45 | with the hydrodynamic model SCARIBOS over the period 2020-2024. We | 45 | with the hydrodynamic model SCARIBOS over the period 2020-2024. We | ||
| 46 | analyze two distinct surface flow regimes previously identified around | 46 | analyze two distinct surface flow regimes previously identified around | ||
| 47 | the island: NW-flow periods dominated by the Caribbean Surface | 47 | the island: NW-flow periods dominated by the Caribbean Surface | ||
| 48 | Current, and EDDY-flow periods characterized by cyclonic eddies or | 48 | Current, and EDDY-flow periods characterized by cyclonic eddies or | ||
| 49 | low-energy conditions. These regimes create contrasting patterns in | 49 | low-energy conditions. These regimes create contrasting patterns in | ||
| 50 | horizontal surface circulation and vertical exchange, with significant | 50 | horizontal surface circulation and vertical exchange, with significant | ||
| 51 | differences in flow direction at the surface layer and enhanced | 51 | differences in flow direction at the surface layer and enhanced | ||
| 52 | upwelling during EDDY-flow conditions. However, analysis of | 52 | upwelling during EDDY-flow conditions. However, analysis of | ||
| 53 | offshore-to-nearshore connectivity using conditional pathways reveals | 53 | offshore-to-nearshore connectivity using conditional pathways reveals | ||
| 54 | that these large-scale surface regimes have no apparent influence on | 54 | that these large-scale surface regimes have no apparent influence on | ||
| 55 | the delivery of deeper waters to nearshore coral reef areas. Spatial | 55 | the delivery of deeper waters to nearshore coral reef areas. Spatial | ||
| 56 | analysis reveals that volumetric transport decreases from east to west | 56 | analysis reveals that volumetric transport decreases from east to west | ||
| 57 | along the southern coastline. The West Point segment exhibits the | 57 | along the southern coastline. The West Point segment exhibits the | ||
| 58 | lowest horizontal transport but the highest vertical exchange, | 58 | lowest horizontal transport but the highest vertical exchange, | ||
| 59 | receiving 48% of its volume transport from subsurface layers, | 59 | receiving 48% of its volume transport from subsurface layers, | ||
| 60 | contrasting with other segments where surface volume transport | 60 | contrasting with other segments where surface volume transport | ||
| 61 | dominates (75-87%). These findings demonstrate that three-dimensional | 61 | dominates (75-87%). These findings demonstrate that three-dimensional | ||
| 62 | circulation patterns create spatially variable conditions for water | 62 | circulation patterns create spatially variable conditions for water | ||
| 63 | renewal, nutrient delivery, and thermal regulation, improving our | 63 | renewal, nutrient delivery, and thermal regulation, improving our | ||
| 64 | understanding of coral reef ecosystem dynamics and supporting reef | 64 | understanding of coral reef ecosystem dynamics and supporting reef | ||
| 65 | management strategies.", | 65 | management strategies.", | ||
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| 67 | "num_tags": 5, | 67 | "num_tags": 5, | ||
| 68 | "organization": { | 68 | "organization": { | ||
| 69 | "approval_status": "approved", | 69 | "approval_status": "approved", | ||
| 70 | "created": "2024-10-22T06:06:56.074257", | 70 | "created": "2024-10-22T06:06:56.074257", | ||
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| 75 | "is_organization": true, | 75 | "is_organization": true, | ||
| 76 | "name": "nioz", | 76 | "name": "nioz", | ||
| 77 | "state": "active", | 77 | "state": "active", | ||
| 78 | "title": "Royal Netherlands Institute for Sea Research", | 78 | "title": "Royal Netherlands Institute for Sea Research", | ||
| 79 | "type": "organization" | 79 | "type": "organization" | ||
| 80 | }, | 80 | }, | ||
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| 221 | "subject": "Earth and Environmental Sciences", | 243 | "subject": "Earth and Environmental Sciences", | ||
| 222 | "tags": [ | 244 | "tags": [ | ||
| 223 | { | 245 | { | ||
| 224 | "display_name": "ctd data", | 246 | "display_name": "ctd data", | ||
| 225 | "id": "49fd7983-2c98-4610-a00f-3e643dcebd46", | 247 | "id": "49fd7983-2c98-4610-a00f-3e643dcebd46", | ||
| 226 | "name": "ctd data", | 248 | "name": "ctd data", | ||
| 227 | "state": "active", | 249 | "state": "active", | ||
| 228 | "vocabulary_id": null | 250 | "vocabulary_id": null | ||
| 229 | }, | 251 | }, | ||
| 230 | { | 252 | { | ||
| 231 | "display_name": "density", | 253 | "display_name": "density", | ||
| 232 | "id": "a53df545-b54d-4e31-8673-3949c3ac036d", | 254 | "id": "a53df545-b54d-4e31-8673-3949c3ac036d", | ||
| 233 | "name": "density", | 255 | "name": "density", | ||
| 234 | "state": "active", | 256 | "state": "active", | ||
| 235 | "vocabulary_id": null | 257 | "vocabulary_id": null | ||
| 236 | }, | 258 | }, | ||
| 237 | { | 259 | { | ||
| 238 | "display_name": "depth", | 260 | "display_name": "depth", | ||
| 239 | "id": "3d04a30a-3ff8-4cfc-ae86-45b5c80899b5", | 261 | "id": "3d04a30a-3ff8-4cfc-ae86-45b5c80899b5", | ||
| 240 | "name": "depth", | 262 | "name": "depth", | ||
| 241 | "state": "active", | 263 | "state": "active", | ||
| 242 | "vocabulary_id": null | 264 | "vocabulary_id": null | ||
| 243 | }, | 265 | }, | ||
| 244 | { | 266 | { | ||
| 245 | "display_name": "salinity", | 267 | "display_name": "salinity", | ||
| 246 | "id": "1e285d08-e3be-4bdb-8ea4-8c7301ce7253", | 268 | "id": "1e285d08-e3be-4bdb-8ea4-8c7301ce7253", | ||
| 247 | "name": "salinity", | 269 | "name": "salinity", | ||
| 248 | "state": "active", | 270 | "state": "active", | ||
| 249 | "vocabulary_id": null | 271 | "vocabulary_id": null | ||
| 250 | }, | 272 | }, | ||
| 251 | { | 273 | { | ||
| 252 | "display_name": "temperature", | 274 | "display_name": "temperature", | ||
| 253 | "id": "9ba5054b-963b-4a54-bcaa-cf1f6c3cf801", | 275 | "id": "9ba5054b-963b-4a54-bcaa-cf1f6c3cf801", | ||
| 254 | "name": "temperature", | 276 | "name": "temperature", | ||
| 255 | "state": "active", | 277 | "state": "active", | ||
| 256 | "vocabulary_id": null | 278 | "vocabulary_id": null | ||
| 257 | } | 279 | } | ||
| 258 | ], | 280 | ], | ||
| 259 | "title": "Depth, potential T, practical S, density data 64PE529", | 281 | "title": "Depth, potential T, practical S, density data 64PE529", | ||
| 260 | "type": "dataset", | 282 | "type": "dataset", | ||
| 261 | "url": "https://doi.org/10.25850/nioz/7b.b.1j", | 283 | "url": "https://doi.org/10.25850/nioz/7b.b.1j", | ||
| 262 | "version": "1" | 284 | "version": "1" | ||
| 263 | } | 285 | } |