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On 27 mai 2026 à 16:24:56 HER,
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| 2 | "Creator": "Academic Journal", | 2 | "Creator": "Academic Journal", | ||
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| 4 | "author_email": null, | 4 | "author_email": null, | ||
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| 6 | "description": "This research highlights how climate driven | 6 | "description": "This research highlights how climate driven | ||
| 7 | permafrost and thaw slumping is affecting the streams in the Peel | 7 | permafrost and thaw slumping is affecting the streams in the Peel | ||
| 8 | Plateau, NWT. ", | 8 | Plateau, NWT. ", | ||
| 9 | "funding_program": "", | 9 | "funding_program": "", | ||
| 10 | "geographic_range": [ | 10 | "geographic_range": [ | ||
| 11 | "NWT" | 11 | "NWT" | ||
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| 21 | "metadata_created": "2026-05-27T22:24:31.174644", | 21 | "metadata_created": "2026-05-27T22:24:31.174644", | ||
| n | 22 | "metadata_modified": "2026-05-27T22:24:56.676830", | n | 22 | "metadata_modified": "2026-05-27T22:24:56.830957", |
| 23 | "metatags": "Permafrost thaw,Thermokarst,Carbon Cycle,Peel | 23 | "metatags": "Permafrost thaw,Thermokarst,Carbon Cycle,Peel | ||
| 24 | Plateau,Hydrology,Thaw Slumps", | 24 | Plateau,Hydrology,Thaw Slumps", | ||
| 25 | "modified_date": "2020-10-27", | 25 | "modified_date": "2020-10-27", | ||
| 26 | "name": | 26 | "name": | ||
| 27 | -organic-carbon-mobilization-from-thaw-slumps-on-the-peel-plateau-nt", | 27 | -organic-carbon-mobilization-from-thaw-slumps-on-the-peel-plateau-nt", | ||
| 28 | "notes": "This research highlights how climate driven permafrost and | 28 | "notes": "This research highlights how climate driven permafrost and | ||
| 29 | thaw slumping is affecting the streams in the Peel Plateau, NWT. ", | 29 | thaw slumping is affecting the streams in the Peel Plateau, NWT. ", | ||
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| 33 | "approval_status": "approved", | 33 | "approval_status": "approved", | ||
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| 42 | "title": "Academic Journal", | 42 | "title": "Academic Journal", | ||
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| 49 | "release_date": "2020-10-27", | 49 | "release_date": "2020-10-27", | ||
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| 65 | "name": "Particulate dominance of organic carbon mobilization | 65 | "name": "Particulate dominance of organic carbon mobilization | ||
| 66 | from thaw slumps on the Peel Plateau, NT: Quantification and | 66 | from thaw slumps on the Peel Plateau, NT: Quantification and | ||
| 67 | implications for stream systems and permafrost carbon release", | 67 | implications for stream systems and permafrost carbon release", | ||
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| t | 78 | "state": "draft", | t | 78 | "state": "active", |
| 79 | "summary": "This study highlights the pressing need for better | 79 | "summary": "This study highlights the pressing need for better | ||
| 80 | knowledge of sedimentary cascades, mobilization, and storage | 80 | knowledge of sedimentary cascades, mobilization, and storage | ||
| 81 | reservoirs in slump-affected streams, and baseline assessments of the | 81 | reservoirs in slump-affected streams, and baseline assessments of the | ||
| 82 | biodegradability of POC and cycling of particulate nutrients within a | 82 | biodegradability of POC and cycling of particulate nutrients within a | ||
| 83 | sedimentary cascade framework. Explicit incorporation of POC dynamics | 83 | sedimentary cascade framework. Explicit incorporation of POC dynamics | ||
| 84 | into our understanding of land-water carbon mobilization in the face | 84 | into our understanding of land-water carbon mobilization in the face | ||
| 85 | of permafrost thaw is critical for understanding implications of | 85 | of permafrost thaw is critical for understanding implications of | ||
| 86 | thermokarst for regional carbon cycling and fluvial ecosystems.", | 86 | thermokarst for regional carbon cycling and fluvial ecosystems.", | ||
| 87 | "tags": [ | 87 | "tags": [ | ||
| 88 | { | 88 | { | ||
| 89 | "display_name": "Carbon Cycle", | 89 | "display_name": "Carbon Cycle", | ||
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| 101 | }, | 101 | }, | ||
| 102 | { | 102 | { | ||
| 103 | "display_name": "Peel Plateau", | 103 | "display_name": "Peel Plateau", | ||
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| 108 | }, | 108 | }, | ||
| 109 | { | 109 | { | ||
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| 111 | "id": "626e7222-e3d2-4539-92b5-b0eae33ed4dd", | 111 | "id": "626e7222-e3d2-4539-92b5-b0eae33ed4dd", | ||
| 112 | "name": "Permafrost thaw", | 112 | "name": "Permafrost thaw", | ||
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| 114 | "vocabulary_id": null | 114 | "vocabulary_id": null | ||
| 115 | }, | 115 | }, | ||
| 116 | { | 116 | { | ||
| 117 | "display_name": "Thaw Slumps", | 117 | "display_name": "Thaw Slumps", | ||
| 118 | "id": "8df558b1-dbdb-4daf-9519-661866ece350", | 118 | "id": "8df558b1-dbdb-4daf-9519-661866ece350", | ||
| 119 | "name": "Thaw Slumps", | 119 | "name": "Thaw Slumps", | ||
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| 121 | "vocabulary_id": null | 121 | "vocabulary_id": null | ||
| 122 | }, | 122 | }, | ||
| 123 | { | 123 | { | ||
| 124 | "display_name": "Thermokarst", | 124 | "display_name": "Thermokarst", | ||
| 125 | "id": "b430c74d-efa4-4ece-85ad-384962cba114", | 125 | "id": "b430c74d-efa4-4ece-85ad-384962cba114", | ||
| 126 | "name": "Thermokarst", | 126 | "name": "Thermokarst", | ||
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| 129 | } | 129 | } | ||
| 130 | ], | 130 | ], | ||
| 131 | "title": "Particulate dominance of organic carbon mobilization from | 131 | "title": "Particulate dominance of organic carbon mobilization from | ||
| 132 | thaw slumps on the Peel Plateau, NT", | 132 | thaw slumps on the Peel Plateau, NT", | ||
| 133 | "type": "dataset", | 133 | "type": "dataset", | ||
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| 135 | "version": null | 135 | "version": null | ||
| 136 | } | 136 | } |