Changes
On September 20, 2023 at 9:03:29 AM UTC,
Nander Wever:
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| f | 1 | { | f | 1 | { |
| 2 | "author": "[{\"affiliation\": \"University of Colorado Boulder, | 2 | "author": "[{\"affiliation\": \"University of Colorado Boulder, | ||
| 3 | Boulder, Colorado, USA\", \"affiliation_02\": \"\", | 3 | Boulder, Colorado, USA\", \"affiliation_02\": \"\", | ||
| 4 | \"affiliation_03\": \"\", \"email\": \"nander.wever@colorado.edu\", | 4 | \"affiliation_03\": \"\", \"email\": \"nander.wever@colorado.edu\", | ||
| 5 | \"given_name\": \"Nander\", \"identifier\": \"0000-0002-4829-8585\", | 5 | \"given_name\": \"Nander\", \"identifier\": \"0000-0002-4829-8585\", | ||
| 6 | \"name\": \"Wever\"}]", | 6 | \"name\": \"Wever\"}]", | ||
| 7 | "author_email": null, | 7 | "author_email": null, | ||
| 8 | "creator_user_id": "9ac4efe2-5526-4212-848e-6e1271dfb98f", | 8 | "creator_user_id": "9ac4efe2-5526-4212-848e-6e1271dfb98f", | ||
| 9 | "date": "[{\"date\": \"2018-12-21\", \"date_type\": \"collected\", | 9 | "date": "[{\"date\": \"2018-12-21\", \"date_type\": \"collected\", | ||
| 10 | \"end_date\": \"2019-01-11\"}]", | 10 | \"end_date\": \"2019-01-11\"}]", | ||
| 11 | "doi": "10.16904/envidat.328", | 11 | "doi": "10.16904/envidat.328", | ||
| 12 | "funding": "[{\"grant_number\": \"BR/165/A2:Mass2Ant\", | 12 | "funding": "[{\"grant_number\": \"BR/165/A2:Mass2Ant\", | ||
| 13 | \"institution\": \"BELSPO\", \"institution_url\": | 13 | \"institution\": \"BELSPO\", \"institution_url\": | ||
| 14 | belspo.be/belspo//Fedra/proj.asp?l=de&COD=BR%2F165%2FA2%2FMass2Ant\"}, | 14 | belspo.be/belspo//Fedra/proj.asp?l=de&COD=BR%2F165%2FA2%2FMass2Ant\"}, | ||
| 15 | {\"grant_number\": \"P2ELP2_172299\", \"institution\": \"Swiss | 15 | {\"grant_number\": \"P2ELP2_172299\", \"institution\": \"Swiss | ||
| 16 | National Science Foundation\", \"institution_url\": | 16 | National Science Foundation\", \"institution_url\": | ||
| 17 | \"https://data.snf.ch/grants?q=172299\"}]", | 17 | \"https://data.snf.ch/grants?q=172299\"}]", | ||
| 18 | "groups": [], | 18 | "groups": [], | ||
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| 20 | "isopen": true, | 20 | "isopen": true, | ||
| 21 | "language": "en", | 21 | "language": "en", | ||
| 22 | "license_id": "odc-odbl", | 22 | "license_id": "odc-odbl", | ||
| 23 | "license_title": "ODbL with Database Contents License (DbCL)", | 23 | "license_title": "ODbL with Database Contents License (DbCL)", | ||
| 24 | "license_url": "https://opendefinition.org/licenses/odc-odbl", | 24 | "license_url": "https://opendefinition.org/licenses/odc-odbl", | ||
| 25 | "maintainer": "{\"affiliation\": \"University of Colorado Boulder, | 25 | "maintainer": "{\"affiliation\": \"University of Colorado Boulder, | ||
| 26 | Boulder, Colorado, USA\", \"email\": \"nander.wever@colorado.edu\", | 26 | Boulder, Colorado, USA\", \"email\": \"nander.wever@colorado.edu\", | ||
| 27 | \"given_name\": \"Nander\", \"identifier\": \"0000-0002-4829-8585\", | 27 | \"given_name\": \"Nander\", \"identifier\": \"0000-0002-4829-8585\", | ||
| 28 | \"name\": \"Wever\"}", | 28 | \"name\": \"Wever\"}", | ||
| 29 | "maintainer_email": null, | 29 | "maintainer_email": null, | ||
| 30 | "metadata_created": "2022-05-26T19:57:28.992927", | 30 | "metadata_created": "2022-05-26T19:57:28.992927", | ||
| n | 31 | "metadata_modified": "2023-09-20T08:43:06.396095", | n | 31 | "metadata_modified": "2023-09-20T09:03:28.935058", |
| 32 | "name": | 32 | "name": | ||
| 33 | terrestrial-laser-scans-on-hammarryggen-ice-rise-dml-east-antarctica", | 33 | terrestrial-laser-scans-on-hammarryggen-ice-rise-dml-east-antarctica", | ||
| 34 | "notes": "Surface topography maps (spatial extent: 400 m x 400 m) | 34 | "notes": "Surface topography maps (spatial extent: 400 m x 400 m) | ||
| 35 | obtained at approximately 300 m from the top of the Hammarryggen Ice | 35 | obtained at approximately 300 m from the top of the Hammarryggen Ice | ||
| 36 | Rise in Dronning Maud Land, East Antarctica, using a Riegl VZ-6000 | 36 | Rise in Dronning Maud Land, East Antarctica, using a Riegl VZ-6000 | ||
| 37 | Terrestrial Laser Scanner (TLS). Scans were obtained on 5 days in the | 37 | Terrestrial Laser Scanner (TLS). Scans were obtained on 5 days in the | ||
| 38 | 2018-2019 Austral summer: on December 21 and 27, and January 2, 4 and | 38 | 2018-2019 Austral summer: on December 21 and 27, and January 2, 4 and | ||
| 39 | 11. By using reflectors installed on bamboo poles, scans were | 39 | 11. By using reflectors installed on bamboo poles, scans were | ||
| 40 | registered with respect to the reflectors, such that the difference | 40 | registered with respect to the reflectors, such that the difference | ||
| 41 | between two successive scans reveals the spatial patterns of erosion | 41 | between two successive scans reveals the spatial patterns of erosion | ||
| 42 | and deposition of snow. On each scan day, we used multiple scan | 42 | and deposition of snow. On each scan day, we used multiple scan | ||
| 43 | positions to create one combined point cloud. After applying an octree | 43 | positions to create one combined point cloud. After applying an octree | ||
| 44 | filter on the point cloud, a 3D surface was obtained. For each day, | 44 | filter on the point cloud, a 3D surface was obtained. For each day, | ||
| 45 | the dataset contains a 1 mm and a 10 cm octree filter resolution file, | 45 | the dataset contains a 1 mm and a 10 cm octree filter resolution file, | ||
| 46 | only including points in a 400 m x 400 m area centered around the scan | 46 | only including points in a 400 m x 400 m area centered around the scan | ||
| 47 | positions.\r\n\r\nNotes:\r\n\r\n* All files in the dataset are in the | 47 | positions.\r\n\r\nNotes:\r\n\r\n* All files in the dataset are in the | ||
| 48 | same coordinate system. However, this coordinate system is arbitrary | 48 | same coordinate system. However, this coordinate system is arbitrary | ||
| 49 | (i.e., not related to any global coordinate system).\r\n\r\n* From the | 49 | (i.e., not related to any global coordinate system).\r\n\r\n* From the | ||
| 50 | installed reflectors, 4 reflectors could be used over the full period. | 50 | installed reflectors, 4 reflectors could be used over the full period. | ||
| 51 | The scan accuracy is generally higher within the area enclosed by the | 51 | The scan accuracy is generally higher within the area enclosed by the | ||
| 52 | reflectors.\r\n\r\n* The scans from January 2 were found to have | 52 | reflectors.\r\n\r\n* The scans from January 2 were found to have | ||
| 53 | exhibited small tilt during the scan and are of lesser | 53 | exhibited small tilt during the scan and are of lesser | ||
| 54 | accuracy.\r\n\r\n* By walking along fixed corridors, disturbance of | 54 | accuracy.\r\n\r\n* By walking along fixed corridors, disturbance of | ||
| 55 | the snow was limited.", | 55 | the snow was limited.", | ||
| 56 | "num_resources": 11, | 56 | "num_resources": 11, | ||
| 57 | "num_tags": 5, | 57 | "num_tags": 5, | ||
| 58 | "organization": { | 58 | "organization": { | ||
| 59 | "approval_status": "approved", | 59 | "approval_status": "approved", | ||
| 60 | "created": "2018-11-15T15:30:05.707541", | 60 | "created": "2018-11-15T15:30:05.707541", | ||
| 61 | "description": "", | 61 | "description": "", | ||
| 62 | "id": "f2a8afe5-e84e-454b-b5d9-6c1bf682eabd", | 62 | "id": "f2a8afe5-e84e-454b-b5d9-6c1bf682eabd", | ||
| 63 | "image_url": "", | 63 | "image_url": "", | ||
| 64 | "is_organization": true, | 64 | "is_organization": true, | ||
| 65 | "name": "snow-processes", | 65 | "name": "snow-processes", | ||
| 66 | "state": "active", | 66 | "state": "active", | ||
| 67 | "title": "Snow Processes", | 67 | "title": "Snow Processes", | ||
| 68 | "type": "organization" | 68 | "type": "organization" | ||
| 69 | }, | 69 | }, | ||
| 70 | "owner_org": "f2a8afe5-e84e-454b-b5d9-6c1bf682eabd", | 70 | "owner_org": "f2a8afe5-e84e-454b-b5d9-6c1bf682eabd", | ||
| 71 | "private": false, | 71 | "private": false, | ||
| 72 | "publication": "{\"publication_year\": \"2022\", \"publisher\": | 72 | "publication": "{\"publication_year\": \"2022\", \"publisher\": | ||
| 73 | \"EnviDat\"}", | 73 | \"EnviDat\"}", | ||
| 74 | "publication_state": "published", | 74 | "publication_state": "published", | ||
| 75 | "related_datasets": "* | 75 | "related_datasets": "* | ||
| 76 | micropen-and-manual-snowpits-from-dronning-maud-land-east-antarctica", | 76 | micropen-and-manual-snowpits-from-dronning-maud-land-east-antarctica", | ||
| 77 | "related_publications": "* Wever, N., Keenan, E., Amory, C., | 77 | "related_publications": "* Wever, N., Keenan, E., Amory, C., | ||
| 78 | Lehning, M, Sigmund, A., Huwald, H., Lenaerts, J.T.M.: Observations | 78 | Lehning, M, Sigmund, A., Huwald, H., Lenaerts, J.T.M.: Observations | ||
| 79 | and\r\nsimulations of new snow density in the drifting snow dominated | 79 | and\r\nsimulations of new snow density in the drifting snow dominated | ||
| 80 | environment of Antarctica. In Review for J. Glaciol.", | 80 | environment of Antarctica. In Review for J. Glaciol.", | ||
| 81 | "relationships_as_object": [], | 81 | "relationships_as_object": [], | ||
| 82 | "relationships_as_subject": [], | 82 | "relationships_as_subject": [], | ||
| 83 | "resource_type": "dataset", | 83 | "resource_type": "dataset", | ||
| 84 | "resource_type_general": "dataset", | 84 | "resource_type_general": "dataset", | ||
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