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| "code": "7b.b.7c", | | "code": "7b.b.7c", |
| "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", |
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| ":\"Mienis\",\"orcid\":\"0000-0002-7370-0652\",\"affiliation\":\"Royal | | ":\"Mienis\",\"orcid\":\"0000-0002-7370-0652\",\"affiliation\":\"Royal |
| Netherlands Institute for Sea | | Netherlands Institute for Sea |
| ndingauthor\":true,\"contactemailaddress\":\"furu.mienis@nioz.nl\"}]", | | ndingauthor\":true,\"contactemailaddress\":\"furu.mienis@nioz.nl\"}]", |
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| "deposit_date": "2022-03-24", | | "deposit_date": "2022-03-24", |
| "depositor": "Furu Mienis", | | "depositor": "Furu Mienis", |
| "distribution_date": "2022-03-24", | | "distribution_date": "2022-03-24", |
| "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": "2022-05-16", | | "doi_date_published": "2022-05-16", |
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| "name": "7bb7c", | | "name": "7bb7c", |
| "notes": "This dataset covers ADCP data collected in Whittard Canyon | | "notes": "This dataset covers ADCP data collected in Whittard Canyon |
| at 2200 m water depth. THe 75 kHz ADCP was upward looking and deployed | | at 2200 m water depth. THe 75 kHz ADCP was upward looking and deployed |
| in Whittard to monitor daily to seasonal changes in current speed and | | in Whittard to monitor daily to seasonal changes in current speed and |
| n | acoustic backscatter.", | n | acoustic backscatter.\n\nChallenging the highstand-dormant paradigm |
| | | for land-detached submarine canyons (Heijnen et al.):\nAbstract: |
| | | Sediment, nutrients, organic carbon and pollutants are funnelled down |
| | | submarine canyons from continental shelves by sediment-laden flows |
| | | called turbidity currents, which dominate particulate transfer to the |
| | | deep sea. Post-glacial sea-level rise disconnected more than three |
| | | quarters of the >9000 submarine canyons worldwide from their former |
| | | river or long-shore drift sediment inputs. Existing models therefore |
| | | assume that land-detached submarine canyons are dormant in the |
| | | present-day; however, monitoring has focused on land-attached canyons |
| | | and this paradigm remains untested. Here we present the most detailed |
| | | field measurements yet of turbidity currents within a land-detached |
| | | submarine canyon, documenting a remarkably similar frequency (6 yr-1) |
| | | and speed (up to 5-8 ms-1) to those in large land-attached submarine |
| | | canyons. Major triggers such as storms or earthquakes are not |
| | | required; instead, seasonal variations in cross-shelf sediment |
| | | transport explain temporal-clustering of flows, and why the storm |
| | | season is surprisingly absent of turbidity currents. As >1000 other |
| | | canyons have a similar configuration, we propose that contemporary |
| | | deep-sea particulate transport via such land- detached canyons may |
| | | have been dramatically under-estimated.", |
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| "subject": "Earth and Environmental Sciences", | | "subject": "Earth and Environmental Sciences", |
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| { | | { |
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| "id": "54d2124d-9aef-4811-b3b5-eaf7dc2927dc", | | "id": "54d2124d-9aef-4811-b3b5-eaf7dc2927dc", |
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| "state": "active", | | "state": "active", |
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| "title": "ADCP data Whittard Canyon 64PE453-53", | | "title": "ADCP data Whittard Canyon 64PE453-53", |
| "type": "dataset", | | "type": "dataset", |
| "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.7c", | | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.7c", |
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