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    "Beaufort Delta"
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    "Beaufort Delta"
            
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  "license_title": "License Not Specified",
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  "license_title": "License Not Specified",
            
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  "local_relevance": "This study assesses the shoreline dynamics and 
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  "local_relevance": "This study assesses the shoreline dynamics and 
            
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its spatiotemporal trends from 1950 to 2020 in the Tuktoyaktuk 
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its spatiotemporal trends from 1950 to 2020 in the Tuktoyaktuk 
            
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Peninsula, analysed in three periods: 1950\u20132020, 1950\u20131985, 
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Peninsula, analysed in three periods: 1950\u20132020, 1950\u20131985, 
            
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and 1985\u20132020",
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and 1985\u20132020",
            
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  "metatags": "Permafrost thaw,Arctic,Sea Level 
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  "metatags": "Permafrost thaw,Arctic,Sea Level 
            
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Rise,Erosion,Biodiversity,Tundra,Thermokarst",
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Rise,Erosion,Biodiversity,Tundra,Thermokarst",
            
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  "modified_date": "2026-08-18",
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  "modified_date": "2026-08-18",
            
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  "name": 
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  "name": 
            
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es-higher-shoreline-retreat-rates-in-complex-low-lying-tundra-coasts",
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es-higher-shoreline-retreat-rates-in-complex-low-lying-tundra-coasts",
            
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  "notes": "This study highlights the importance of existing coastal 
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  "notes": "This study highlights the importance of existing coastal 
            
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morphology in controlling shoreline change evolution in the 
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morphology in controlling shoreline change evolution in the 
            
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Tuktoyaktuk Peninsula.",
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Tuktoyaktuk Peninsula, NWT.",
            
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    "title": "Academic Journal",
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    "title": "Academic Journal",
            
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      "name": "Submergence influences higher shoreline retreat rates 
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      "name": "Submergence influences higher shoreline retreat rates 
            
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in complex low-lying tundra coasts (Tuktoyaktuk Peninsula, NWT, 
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in complex low-lying tundra coasts (Tuktoyaktuk Peninsula, NWT, 
            
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Canada)",
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Canada)",
            
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      "url": 
            
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luences-higher-shoreline-retreat-rates-in-complex-low-lying-tund.pdf",
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luences-higher-shoreline-retreat-rates-in-complex-low-lying-tund.pdf",
            
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  ],
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  ],
            
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  "state": "active",
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  "state": "active",
            
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  "summary": "This study highlights the importance of existing coastal 
100
  "summary": "This study highlights the importance of existing coastal 
            
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morphology in controlling shoreline change evolution in the 
101
morphology in controlling shoreline change evolution in the 
            
83
Tuktoyaktuk Peninsula. Data analysis shows that submergence is a key 
102
Tuktoyaktuk Peninsula. Data analysis shows that submergence is a key 
            
84
process driving extreme shoreline retreat hotspots, particularly in 
103
process driving extreme shoreline retreat hotspots, particularly in 
            
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low-lying areas. The distinction between erosion and submergence is 
104
low-lying areas. The distinction between erosion and submergence is 
            
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key in Arctic coastal studies, as its differing drivers and impacts 
105
key in Arctic coastal studies, as its differing drivers and impacts 
            
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must be thoroughly assessed to improve coastal management and climate 
106
must be thoroughly assessed to improve coastal management and climate 
            
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and morphodynamic models. Future research should focus on integrating 
107
and morphodynamic models. Future research should focus on integrating 
            
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sea-level rise, permafrost thaw, and isostatic subsidence alongside 
108
sea-level rise, permafrost thaw, and isostatic subsidence alongside 
            
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erosion in coastal change models. ",
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erosion in coastal change models. ",
            
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  "tags": [
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  "tags": [
            
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    {
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    {
            
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      "display_name": "Arctic",
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      "display_name": "Arctic",
            
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      "id": "25dee16e-a24a-4238-a428-3617178f21cc",
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      "id": "25dee16e-a24a-4238-a428-3617178f21cc",
            
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      "name": "Arctic",
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      "name": "Arctic",
            
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      "state": "active",
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    {
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      "display_name": "Erosion",
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      "display_name": "Erosion",
            
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      "id": "95d06e76-8e97-4bf8-9687-ea846516d7db",
            
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      "name": "Erosion",
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      "name": "Erosion",
            
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    {
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    {
            
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      "display_name": "Permafrost thaw",
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      "display_name": "Permafrost thaw",
            
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      "id": "626e7222-e3d2-4539-92b5-b0eae33ed4dd",
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      "id": "626e7222-e3d2-4539-92b5-b0eae33ed4dd",
            
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      "name": "Permafrost thaw",
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      "name": "Permafrost thaw",
            
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      "state": "active",
            
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    {
            
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      "display_name": "Sea Level Rise",
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      "display_name": "Sea Level Rise",
            
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      "id": "88ef7eeb-7a8c-483a-9e97-57322d00781a",
            
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      "name": "Sea Level Rise",
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      "name": "Sea Level Rise",
            
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      "state": "active",
            
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    {
            
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      "display_name": "Thermokarst",
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      "display_name": "Thermokarst",
            
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      "id": "b430c74d-efa4-4ece-85ad-384962cba114",
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      "id": "b430c74d-efa4-4ece-85ad-384962cba114",
            
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      "name": "Thermokarst",
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      "name": "Thermokarst",
            
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      "state": "active",
            
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      "display_name": "Tundra",
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      "display_name": "Tundra",
            
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      "id": "8bd5a50b-bb3f-4ebd-a7bb-7ddc204957b6",
            
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      "name": "Tundra",
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      "name": "Tundra",
            
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    }
            
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  ],
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  ],
            
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  "title": "Submergence Influences Higher Shoreline Retreat Rates in 
161
  "title": "Submergence Influences Higher Shoreline Retreat Rates in 
            
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Complex low-lying Tundra Coasts",
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Complex low-lying Tundra Coasts",
            
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}