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  "author": "Furu Mienis (Royal Netherlands Institute for Sea 
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  "author": "Furu Mienis (Royal Netherlands Institute for Sea 
            
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Research)",
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Research)",
            
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  "author_email": "furu.mienis@nioz.nl",
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  "author_email": "furu.mienis@nioz.nl",
            
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  "code": "7b.b.1j",
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  "code": "7b.b.1j",
            
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  "contributor": "Royal Netherlands Institute for Sea Research 
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  "contributor": "Royal Netherlands Institute for Sea Research 
            
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(NIOZ)",
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(NIOZ)",
            
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"Furu\",\"lastname\":\"Mienis\",\"orcid\":null,\"affiliation\":\"Royal 
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"Furu\",\"lastname\":\"Mienis\",\"orcid\":null,\"affiliation\":\"Royal 
            
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Netherlands Institute for Sea 
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Netherlands Institute for Sea 
            
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e,\"contactemailaddress\":\"furu.mienis@nioz.nl\",\"formatted\":\"Furu 
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e,\"contactemailaddress\":\"furu.mienis@nioz.nl\",\"formatted\":\"Furu 
            
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Mienis - Royal Netherlands Institute for Sea Research - ORCID:  - 
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Mienis - Royal Netherlands Institute for Sea Research - ORCID:  - 
            
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Corresponding Author - 
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Corresponding Author - 
            
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a\",\"lastname\":\"Bertoncelj\",\"orcid\":null,\"affiliation\":\"Royal 
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a\",\"lastname\":\"Bertoncelj\",\"orcid\":null,\"affiliation\":\"Royal 
            
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Netherlands Institute for Sea 
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Netherlands Institute for Sea 
            
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ondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Vesna 
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ondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Vesna 
            
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Bertoncelj - Royal Netherlands Institute for Sea Research - ORCID: 
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Bertoncelj - Royal Netherlands Institute for Sea Research - ORCID: 
            
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  "deposit_date": "2025-08-30",
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  "deposit_date": "2025-08-30",
            
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  "depositor": "Furu Mienis (furu.mienis@nioz.nl)",
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  "depositor": "Furu Mienis (furu.mienis@nioz.nl)",
            
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  "distribution_date": "2025-08-30",
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  "distribution_date": "2025-08-30",
            
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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": "2025-08-30T10:13:52.170364",
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  "doi_date_published": "2025-08-30T10:13:52.170364",
            
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  "funding_references": 
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  "funding_references": 
            
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er\":\"NWOCA.2019.003\",\"awardtitle\":\"Sealink\",\"formatted\":\"NWO 
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er\":\"NWOCA.2019.003\",\"awardtitle\":\"Sealink\",\"formatted\":\"NWO 
            
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- NWOCA.2019.003 - Sealink\"}]",
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- NWOCA.2019.003 - Sealink\"}]",
            
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  "name": "depth",
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  "name": "depth",
            
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  "notes": "Shallow-water coral reef ecosystems are positioned at the 
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  "notes": "Shallow-water coral reef ecosystems are positioned at the 
            
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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 
            
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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 
            
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low-energy conditions. These regimes create contrasting patterns in 
49
low-energy conditions. These regimes create contrasting patterns in 
            
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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 
            
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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, 
            
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receiving 48% of its volume transport from subsurface layers, 
59
receiving 48% of its volume transport from subsurface layers, 
            
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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 
            
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management strategies.",
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    {
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      "display_name": "depth",
            
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      "id": "3d04a30a-3ff8-4cfc-ae86-45b5c80899b5",
            
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      "name": "depth",
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      "name": "depth",
            
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    },
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    {
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      "display_name": "salinity",
            
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      "id": "1e285d08-e3be-4bdb-8ea4-8c7301ce7253",
            
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      "name": "salinity",
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      "name": "salinity",
            
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      "state": "active",
            
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    },
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    {
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    {
            
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      "display_name": "temperature",
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      "display_name": "temperature",
            
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  ],
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  ],
            
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  "title": "Depth, potential T, practical S, density data 64PE529",
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  "title": "Depth, potential T, practical S, density data 64PE529",
            
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  "type": "dataset",
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  "type": "dataset",
            
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  "url": "https://doi.org/10.25850/nioz/7b.b.1j",
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  "url": "https://doi.org/10.25850/nioz/7b.b.1j",
            
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  "version": "1"
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  "version": "1"
            
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}
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}