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On October 30, 2026 at 2:11:32 PM MDT,
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Added resource Submergence influences higher shoreline retreat rates in complex low-lying tundra coasts (Tuktoyaktuk Peninsula, NWT, Canada) to Submergence influences higher shoreline retreat rates in complex low-lying tundra coasts
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| 2 | "Creator": "Academic Journal", | 2 | "Creator": "Academic Journal", | ||
| 3 | "author": null, | 3 | "author": null, | ||
| 4 | "author_email": null, | 4 | "author_email": null, | ||
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| 6 | "description": "", | 6 | "description": "", | ||
| 7 | "funding_program": "", | 7 | "funding_program": "", | ||
| 8 | "geographic_range": [ | 8 | "geographic_range": [ | ||
| 9 | "Beaufort Delta" | 9 | "Beaufort Delta" | ||
| 10 | ], | 10 | ], | ||
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| 15 | "license_title": "License Not Specified", | 15 | "license_title": "License Not Specified", | ||
| 16 | "local_relevance": "This study assesses the shoreline dynamics and | 16 | "local_relevance": "This study assesses the shoreline dynamics and | ||
| 17 | its spatiotemporal trends from 1950 to 2020 in the Tuktoyaktuk | 17 | its spatiotemporal trends from 1950 to 2020 in the Tuktoyaktuk | ||
| 18 | Peninsula, analysed in three periods: 1950\u20132020, 1950\u20131985, | 18 | Peninsula, analysed in three periods: 1950\u20132020, 1950\u20131985, | ||
| 19 | and 1985\u20132020", | 19 | and 1985\u20132020", | ||
| 20 | "maintainer": null, | 20 | "maintainer": null, | ||
| 21 | "maintainer_email": null, | 21 | "maintainer_email": null, | ||
| 22 | "metadata_created": "2026-10-30T20:09:55.325035", | 22 | "metadata_created": "2026-10-30T20:09:55.325035", | ||
| n | 23 | "metadata_modified": "2026-10-30T20:09:55.325042", | n | 23 | "metadata_modified": "2026-10-30T20:11:32.059914", |
| 24 | "metatags": "Permafrost thaw,Arctic,Sea Level | 24 | "metatags": "Permafrost thaw,Arctic,Sea Level | ||
| 25 | Rise,Erosion,Biodiversity,Tundra,Thermokarst", | 25 | Rise,Erosion,Biodiversity,Tundra,Thermokarst", | ||
| 26 | "modified_date": "2026-08-18", | 26 | "modified_date": "2026-08-18", | ||
| 27 | "name": | 27 | "name": | ||
| 28 | es-higher-shoreline-retreat-rates-in-complex-low-lying-tundra-coasts", | 28 | es-higher-shoreline-retreat-rates-in-complex-low-lying-tundra-coasts", | ||
| 29 | "notes": "This study highlights the importance of existing coastal | 29 | "notes": "This study highlights the importance of existing coastal | ||
| 30 | morphology in controlling shoreline change evolution in the | 30 | morphology in controlling shoreline change evolution in the | ||
| 31 | Tuktoyaktuk Peninsula.", | 31 | Tuktoyaktuk Peninsula.", | ||
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| 35 | "approval_status": "approved", | 35 | "approval_status": "approved", | ||
| 36 | "created": "2023-11-27T15:29:16.450990", | 36 | "created": "2023-11-27T15:29:16.450990", | ||
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| 42 | "name": "academic-journal", | 42 | "name": "academic-journal", | ||
| 43 | "state": "active", | 43 | "state": "active", | ||
| 44 | "title": "Academic Journal", | 44 | "title": "Academic Journal", | ||
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| 51 | "release_date": "2026-08-18", | 51 | "release_date": "2026-08-18", | ||
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| 67 | "name": "Submergence influences higher shoreline retreat rates | ||||
| 68 | in complex low-lying tundra coasts (Tuktoyaktuk Peninsula, NWT, | ||||
| 69 | Canada)", | ||||
| 70 | "package_id": "863965d4-6a88-4287-af33-6f890e6ad728", | ||||
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| 74 | "state": "active", | ||||
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| 76 | luences-higher-shoreline-retreat-rates-in-complex-low-lying-tund.pdf", | ||||
| 77 | "url_type": "upload" | ||||
| 78 | } | ||||
| 79 | ], | ||||
| 53 | "state": "draft", | 80 | "state": "draft", | ||
| 54 | "summary": "This study highlights the importance of existing coastal | 81 | "summary": "This study highlights the importance of existing coastal | ||
| 55 | morphology in controlling shoreline change evolution in the | 82 | morphology in controlling shoreline change evolution in the | ||
| 56 | Tuktoyaktuk Peninsula. Data analysis shows that submergence is a key | 83 | Tuktoyaktuk Peninsula. Data analysis shows that submergence is a key | ||
| 57 | process driving extreme shoreline retreat hotspots, particularly in | 84 | process driving extreme shoreline retreat hotspots, particularly in | ||
| 58 | low-lying areas. The distinction between erosion and submergence is | 85 | low-lying areas. The distinction between erosion and submergence is | ||
| 59 | key in Arctic coastal studies, as its differing drivers and impacts | 86 | key in Arctic coastal studies, as its differing drivers and impacts | ||
| 60 | must be thoroughly assessed to improve coastal management and climate | 87 | must be thoroughly assessed to improve coastal management and climate | ||
| 61 | and morphodynamic models. Future research should focus on integrating | 88 | and morphodynamic models. Future research should focus on integrating | ||
| 62 | sea-level rise, permafrost thaw, and isostatic subsidence alongside | 89 | sea-level rise, permafrost thaw, and isostatic subsidence alongside | ||
| 63 | erosion in coastal change models. ", | 90 | erosion in coastal change models. ", | ||
| 64 | "tags": [ | 91 | "tags": [ | ||
| 65 | { | 92 | { | ||
| 66 | "display_name": "Arctic", | 93 | "display_name": "Arctic", | ||
| 67 | "id": "25dee16e-a24a-4238-a428-3617178f21cc", | 94 | "id": "25dee16e-a24a-4238-a428-3617178f21cc", | ||
| 68 | "name": "Arctic", | 95 | "name": "Arctic", | ||
| 69 | "state": "active", | 96 | "state": "active", | ||
| 70 | "vocabulary_id": null | 97 | "vocabulary_id": null | ||
| 71 | }, | 98 | }, | ||
| 72 | { | 99 | { | ||
| 73 | "display_name": "Biodiversity", | 100 | "display_name": "Biodiversity", | ||
| 74 | "id": "e6c38500-1f0d-4085-b5ba-7c92726db6b7", | 101 | "id": "e6c38500-1f0d-4085-b5ba-7c92726db6b7", | ||
| 75 | "name": "Biodiversity", | 102 | "name": "Biodiversity", | ||
| 76 | "state": "active", | 103 | "state": "active", | ||
| 77 | "vocabulary_id": null | 104 | "vocabulary_id": null | ||
| 78 | }, | 105 | }, | ||
| 79 | { | 106 | { | ||
| 80 | "display_name": "Erosion", | 107 | "display_name": "Erosion", | ||
| 81 | "id": "95d06e76-8e97-4bf8-9687-ea846516d7db", | 108 | "id": "95d06e76-8e97-4bf8-9687-ea846516d7db", | ||
| 82 | "name": "Erosion", | 109 | "name": "Erosion", | ||
| 83 | "state": "active", | 110 | "state": "active", | ||
| 84 | "vocabulary_id": null | 111 | "vocabulary_id": null | ||
| 85 | }, | 112 | }, | ||
| 86 | { | 113 | { | ||
| 87 | "display_name": "Permafrost thaw", | 114 | "display_name": "Permafrost thaw", | ||
| 88 | "id": "626e7222-e3d2-4539-92b5-b0eae33ed4dd", | 115 | "id": "626e7222-e3d2-4539-92b5-b0eae33ed4dd", | ||
| 89 | "name": "Permafrost thaw", | 116 | "name": "Permafrost thaw", | ||
| 90 | "state": "active", | 117 | "state": "active", | ||
| 91 | "vocabulary_id": null | 118 | "vocabulary_id": null | ||
| 92 | }, | 119 | }, | ||
| 93 | { | 120 | { | ||
| 94 | "display_name": "Sea Level Rise", | 121 | "display_name": "Sea Level Rise", | ||
| 95 | "id": "88ef7eeb-7a8c-483a-9e97-57322d00781a", | 122 | "id": "88ef7eeb-7a8c-483a-9e97-57322d00781a", | ||
| 96 | "name": "Sea Level Rise", | 123 | "name": "Sea Level Rise", | ||
| 97 | "state": "active", | 124 | "state": "active", | ||
| 98 | "vocabulary_id": null | 125 | "vocabulary_id": null | ||
| 99 | }, | 126 | }, | ||
| 100 | { | 127 | { | ||
| 101 | "display_name": "Thermokarst", | 128 | "display_name": "Thermokarst", | ||
| 102 | "id": "b430c74d-efa4-4ece-85ad-384962cba114", | 129 | "id": "b430c74d-efa4-4ece-85ad-384962cba114", | ||
| 103 | "name": "Thermokarst", | 130 | "name": "Thermokarst", | ||
| 104 | "state": "active", | 131 | "state": "active", | ||
| 105 | "vocabulary_id": null | 132 | "vocabulary_id": null | ||
| 106 | }, | 133 | }, | ||
| 107 | { | 134 | { | ||
| 108 | "display_name": "Tundra", | 135 | "display_name": "Tundra", | ||
| 109 | "id": "8bd5a50b-bb3f-4ebd-a7bb-7ddc204957b6", | 136 | "id": "8bd5a50b-bb3f-4ebd-a7bb-7ddc204957b6", | ||
| 110 | "name": "Tundra", | 137 | "name": "Tundra", | ||
| 111 | "state": "active", | 138 | "state": "active", | ||
| 112 | "vocabulary_id": null | 139 | "vocabulary_id": null | ||
| 113 | } | 140 | } | ||
| 114 | ], | 141 | ], | ||
| 115 | "title": "Submergence influences higher shoreline retreat rates in | 142 | "title": "Submergence influences higher shoreline retreat rates in | ||
| 116 | complex low-lying tundra coasts", | 143 | complex low-lying tundra coasts", | ||
| 117 | "type": "dataset", | 144 | "type": "dataset", | ||
| 118 | "url": null, | 145 | "url": null, | ||
| 119 | "version": null | 146 | "version": null | ||
| 120 | } | 147 | } |