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On December 1, 2023 at 10:41:04 AM MST, andrew_speakman:
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f | 1 | { | f | 1 | { |
2 | "Creator": "Robert H. Fraser, Steven V. Kokelj, Trevor C. Lantz, | 2 | "Creator": "Robert H. Fraser, Steven V. Kokelj, Trevor C. Lantz, | ||
3 | Morgan McFarlane-Winchester, Ian Olthof and Denis Lacelle", | 3 | Morgan McFarlane-Winchester, Ian Olthof and Denis Lacelle", | ||
4 | "author": null, | 4 | "author": null, | ||
5 | "author_email": null, | 5 | "author_email": null, | ||
6 | "creator_user_id": "8667495d-e311-4e09-9000-9dc13a2ca069", | 6 | "creator_user_id": "8667495d-e311-4e09-9000-9dc13a2ca069", | ||
7 | "description": "", | 7 | "description": "", | ||
8 | "funding_program": "", | 8 | "funding_program": "", | ||
9 | "geographic_range": [ | 9 | "geographic_range": [ | ||
10 | "Beaufort Delta" | 10 | "Beaufort Delta" | ||
11 | ], | 11 | ], | ||
12 | "groups": [], | 12 | "groups": [], | ||
13 | "id": "87d79b97-fde1-43e2-a99b-c1aaf4d7cbad", | 13 | "id": "87d79b97-fde1-43e2-a99b-c1aaf4d7cbad", | ||
14 | "isopen": false, | 14 | "isopen": false, | ||
15 | "license_id": "notspecified", | 15 | "license_id": "notspecified", | ||
16 | "license_title": "License Not Specified", | 16 | "license_title": "License Not Specified", | ||
17 | "local_relevance": "Exploring permafrost effects", | 17 | "local_relevance": "Exploring permafrost effects", | ||
18 | "maintainer": null, | 18 | "maintainer": null, | ||
19 | "maintainer_email": null, | 19 | "maintainer_email": null, | ||
20 | "metadata_created": "2023-12-01T17:40:22.493611", | 20 | "metadata_created": "2023-12-01T17:40:22.493611", | ||
n | 21 | "metadata_modified": "2023-12-01T17:41:04.731945", | n | 21 | "metadata_modified": "2023-12-01T17:41:04.916799", |
22 | "metatags": "Remote Sensing,Permafrost,Research", | 22 | "metatags": "Remote Sensing,Permafrost,Research", | ||
23 | "modified_date": "2018-06-12", | 23 | "modified_date": "2018-06-12", | ||
24 | "name": "climate-sensitivity-of-high-arctic-permafrost", | 24 | "name": "climate-sensitivity-of-high-arctic-permafrost", | ||
25 | "notes": "This paper shows that climate-driven thaw of hilltop | 25 | "notes": "This paper shows that climate-driven thaw of hilltop | ||
26 | ice-wedge networks is rapidly transforming uplands across Banks Island | 26 | ice-wedge networks is rapidly transforming uplands across Banks Island | ||
27 | in the Canadian Arctic Archipelago.", | 27 | in the Canadian Arctic Archipelago.", | ||
28 | "num_resources": 1, | 28 | "num_resources": 1, | ||
29 | "num_tags": 3, | 29 | "num_tags": 3, | ||
30 | "organization": { | 30 | "organization": { | ||
31 | "approval_status": "approved", | 31 | "approval_status": "approved", | ||
32 | "created": "2023-11-27T14:46:04.433050", | 32 | "created": "2023-11-27T14:46:04.433050", | ||
33 | "description": "", | 33 | "description": "", | ||
34 | "id": "aacbbdf0-754a-482e-aa28-46c7eb1f4525", | 34 | "id": "aacbbdf0-754a-482e-aa28-46c7eb1f4525", | ||
35 | "image_url": "", | 35 | "image_url": "", | ||
36 | "is_organization": true, | 36 | "is_organization": true, | ||
37 | "name": "natural-resources-canada", | 37 | "name": "natural-resources-canada", | ||
38 | "state": "active", | 38 | "state": "active", | ||
39 | "title": "Natural Resources Canada", | 39 | "title": "Natural Resources Canada", | ||
40 | "type": "organization" | 40 | "type": "organization" | ||
41 | }, | 41 | }, | ||
42 | "owner_org": "aacbbdf0-754a-482e-aa28-46c7eb1f4525", | 42 | "owner_org": "aacbbdf0-754a-482e-aa28-46c7eb1f4525", | ||
43 | "private": false, | 43 | "private": false, | ||
44 | "relationships_as_object": [], | 44 | "relationships_as_object": [], | ||
45 | "relationships_as_subject": [], | 45 | "relationships_as_subject": [], | ||
46 | "release_date": "2018-06-12", | 46 | "release_date": "2018-06-12", | ||
47 | "resources": [ | 47 | "resources": [ | ||
48 | { | 48 | { | ||
49 | "cache_last_updated": null, | 49 | "cache_last_updated": null, | ||
50 | "cache_url": null, | 50 | "cache_url": null, | ||
51 | "created": "2023-12-01T17:41:04.747831", | 51 | "created": "2023-12-01T17:41:04.747831", | ||
52 | "datastore_active": false, | 52 | "datastore_active": false, | ||
53 | "datastore_contains_all_records_of_source_file": false, | 53 | "datastore_contains_all_records_of_source_file": false, | ||
54 | "description": null, | 54 | "description": null, | ||
55 | "format": "PDF", | 55 | "format": "PDF", | ||
56 | "hash": "", | 56 | "hash": "", | ||
57 | "id": "c6f20cc2-86b3-4bd0-aebe-9147810bda06", | 57 | "id": "c6f20cc2-86b3-4bd0-aebe-9147810bda06", | ||
58 | "last_modified": "2023-12-01T17:41:04.724748", | 58 | "last_modified": "2023-12-01T17:41:04.724748", | ||
n | 59 | "metadata_modified": "2023-12-01T17:41:04.738481", | n | 59 | "metadata_modified": "2023-12-01T17:41:04.923105", |
60 | "mimetype": "application/pdf", | 60 | "mimetype": "application/pdf", | ||
61 | "mimetype_inner": null, | 61 | "mimetype_inner": null, | ||
62 | "name": "Climate Sensitivity of High Arctic Permafrost Terrain | 62 | "name": "Climate Sensitivity of High Arctic Permafrost Terrain | ||
63 | Demonstrated by Widespread Ice-Wedge Thermokarst on Banks Island", | 63 | Demonstrated by Widespread Ice-Wedge Thermokarst on Banks Island", | ||
64 | "package_id": "87d79b97-fde1-43e2-a99b-c1aaf4d7cbad", | 64 | "package_id": "87d79b97-fde1-43e2-a99b-c1aaf4d7cbad", | ||
65 | "position": 0, | 65 | "position": 0, | ||
66 | "resource_type": null, | 66 | "resource_type": null, | ||
67 | "size": 12437757, | 67 | "size": 12437757, | ||
68 | "state": "active", | 68 | "state": "active", | ||
69 | "url": | 69 | "url": | ||
70 | 0cc2-86b3-4bd0-aebe-9147810bda06/download/remotesensing-10-00954.pdf", | 70 | 0cc2-86b3-4bd0-aebe-9147810bda06/download/remotesensing-10-00954.pdf", | ||
71 | "url_type": "upload" | 71 | "url_type": "upload" | ||
72 | } | 72 | } | ||
73 | ], | 73 | ], | ||
t | 74 | "state": "draft", | t | 74 | "state": "active", |
75 | "summary": "Ice wedges form due to thermal contraction, cracking of | 75 | "summary": "Ice wedges form due to thermal contraction, cracking of | ||
76 | the ground and infilling typically by snowmelt that refreezes to form | 76 | the ground and infilling typically by snowmelt that refreezes to form | ||
77 | a vein of ice. Over millennia, repeated cracking can cause large ice | 77 | a vein of ice. Over millennia, repeated cracking can cause large ice | ||
78 | wedges to develop. The broad distribution and thaw sensitivity of | 78 | wedges to develop. The broad distribution and thaw sensitivity of | ||
79 | ice-wedge networks suggests that evolution of polygonal terrain will | 79 | ice-wedge networks suggests that evolution of polygonal terrain will | ||
80 | have a major influence on landscape form and ecological and | 80 | have a major influence on landscape form and ecological and | ||
81 | biogeochemical processes across a warming circumpolar Arctic.", | 81 | biogeochemical processes across a warming circumpolar Arctic.", | ||
82 | "tags": [ | 82 | "tags": [ | ||
83 | { | 83 | { | ||
84 | "display_name": "Permafrost", | 84 | "display_name": "Permafrost", | ||
85 | "id": "ae8cf607-cab9-443a-9c5e-0a7a51698419", | 85 | "id": "ae8cf607-cab9-443a-9c5e-0a7a51698419", | ||
86 | "name": "Permafrost", | 86 | "name": "Permafrost", | ||
87 | "state": "active", | 87 | "state": "active", | ||
88 | "vocabulary_id": null | 88 | "vocabulary_id": null | ||
89 | }, | 89 | }, | ||
90 | { | 90 | { | ||
91 | "display_name": "Remote Sensing", | 91 | "display_name": "Remote Sensing", | ||
92 | "id": "dc4f64a0-95da-45ab-bf8a-197c40a71a8d", | 92 | "id": "dc4f64a0-95da-45ab-bf8a-197c40a71a8d", | ||
93 | "name": "Remote Sensing", | 93 | "name": "Remote Sensing", | ||
94 | "state": "active", | 94 | "state": "active", | ||
95 | "vocabulary_id": null | 95 | "vocabulary_id": null | ||
96 | }, | 96 | }, | ||
97 | { | 97 | { | ||
98 | "display_name": "Research", | 98 | "display_name": "Research", | ||
99 | "id": "9ce08dce-f710-4692-8be5-23a0beedaf90", | 99 | "id": "9ce08dce-f710-4692-8be5-23a0beedaf90", | ||
100 | "name": "Research", | 100 | "name": "Research", | ||
101 | "state": "active", | 101 | "state": "active", | ||
102 | "vocabulary_id": null | 102 | "vocabulary_id": null | ||
103 | } | 103 | } | ||
104 | ], | 104 | ], | ||
105 | "title": "Climate Sensitivity of High Arctic Permafrost Terrain | 105 | "title": "Climate Sensitivity of High Arctic Permafrost Terrain | ||
106 | Demonstrated by Widespread Ice-Wedge Thermokarst on Banks Island", | 106 | Demonstrated by Widespread Ice-Wedge Thermokarst on Banks Island", | ||
107 | "type": "dataset", | 107 | "type": "dataset", | ||
108 | "url": null, | 108 | "url": null, | ||
109 | "version": null | 109 | "version": null | ||
110 | } | 110 | } |