Changes
On May 21, 2024 at 12:27:05 PM UTC,
-
Updated description of resource t2_3m.zip in Turbulence in The Strongly Heterogeneous Near-Surface Boundary Layer over Patchy Snow to
Raw eddy covariance data from tower 2 at 3m height. Instrument is Campell Scientifc CSAT 3
-
Changed value of field
resource_size
of resource t2_3m.zip to{"size_value":"","size_units":""}
(previously{"size_value":"","size_units":"kb"}
) in Turbulence in The Strongly Heterogeneous Near-Surface Boundary Layer over Patchy Snow
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7 | \"lehning@slf.ch\", \"given_name\": \"Michael\", \"identifier\": | 7 | \"lehning@slf.ch\", \"given_name\": \"Michael\", \"identifier\": | ||
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10 | \"email\": \"mott@slf.ch\", \"given_name\": \"Rebecca\", | 10 | \"email\": \"mott@slf.ch\", \"given_name\": \"Rebecca\", | ||
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14 | "date": "[{\"date\": \"2021-05-21\", \"date_type\": \"collected\", | 14 | "date": "[{\"date\": \"2021-05-21\", \"date_type\": \"collected\", | ||
15 | \"end_date\": \"2021-06-11\"}]", | 15 | \"end_date\": \"2021-06-11\"}]", | ||
16 | "doi": "10.16904/envidat.399", | 16 | "doi": "10.16904/envidat.399", | ||
17 | "funding": "[{\"grant_number\": \"188554\", \"institution\": | 17 | "funding": "[{\"grant_number\": \"188554\", \"institution\": | ||
18 | \"SNF\", \"institution_url\": | 18 | \"SNF\", \"institution_url\": | ||
19 | \"https://data.snf.ch/grants/grant/188554\"}]", | 19 | \"https://data.snf.ch/grants/grant/188554\"}]", | ||
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24 | "license_id": "wsl-data", | 24 | "license_id": "wsl-data", | ||
25 | "license_title": "WSL Data Policy", | 25 | "license_title": "WSL Data Policy", | ||
26 | "license_url": | 26 | "license_url": | ||
27 | ps://www.wsl.ch/en/about-wsl/programmes-and-initiatives/envidat.html", | 27 | ps://www.wsl.ch/en/about-wsl/programmes-and-initiatives/envidat.html", | ||
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30 | \"identifier\": \"0000-0003-3228-9868\", \"name\": \"Haugeneder\"}", | 30 | \"identifier\": \"0000-0003-3228-9868\", \"name\": \"Haugeneder\"}", | ||
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n | 33 | "metadata_modified": "2024-05-21T12:26:43.093455", | n | 33 | "metadata_modified": "2024-05-21T12:27:05.191778", |
34 | "name": "turbulence-patchy-snow-cover", | 34 | "name": "turbulence-patchy-snow-cover", | ||
35 | "notes": "This dataset contains the raw data that is analyzed in the | 35 | "notes": "This dataset contains the raw data that is analyzed in the | ||
36 | publication entitled \"Turbulence in The Strongly Heterogeneous | 36 | publication entitled \"Turbulence in The Strongly Heterogeneous | ||
37 | Near-Surface Boundary Layer over Patchy Snow\". Please find | 37 | Near-Surface Boundary Layer over Patchy Snow\". Please find | ||
38 | information on the individual data files in the description of the | 38 | information on the individual data files in the description of the | ||
39 | files.", | 39 | files.", | ||
40 | "num_resources": 6, | 40 | "num_resources": 6, | ||
41 | "num_tags": 5, | 41 | "num_tags": 5, | ||
42 | "organization": { | 42 | "organization": { | ||
43 | "approval_status": "approved", | 43 | "approval_status": "approved", | ||
44 | "created": "2021-08-23T15:25:48.676190", | 44 | "created": "2021-08-23T15:25:48.676190", | ||
45 | "description": "The research group \u00abSnow Hydrology\u00bb | 45 | "description": "The research group \u00abSnow Hydrology\u00bb | ||
46 | investigates snow as a component of the hydrological cycle. In the | 46 | investigates snow as a component of the hydrological cycle. In the | ||
47 | Alps a significant percentage of precipitation comes in the form of | 47 | Alps a significant percentage of precipitation comes in the form of | ||
48 | snow. The timing of snow melt thus influences the annual dynamics of | 48 | snow. The timing of snow melt thus influences the annual dynamics of | ||
49 | runoff from alpine watersheds. Of particular interest for our research | 49 | runoff from alpine watersheds. Of particular interest for our research | ||
50 | is to enhance estimations of snow water resources and subsequent melt | 50 | is to enhance estimations of snow water resources and subsequent melt | ||
51 | water discharge.\r\n\r\nThe research group covers a broad range of | 51 | water discharge.\r\n\r\nThe research group covers a broad range of | ||
52 | projects and methods. The latest measuring techniques are used to | 52 | projects and methods. The latest measuring techniques are used to | ||
53 | investigate snow distribution patterns in alpine terrain, e.g. laser | 53 | investigate snow distribution patterns in alpine terrain, e.g. laser | ||
54 | scanning or radar technology. We use different types of numerical | 54 | scanning or radar technology. We use different types of numerical | ||
55 | models to calculate snow water resources based on input data from | 55 | models to calculate snow water resources based on input data from | ||
56 | meteorological monitoring networks. These models are being used to | 56 | meteorological monitoring networks. These models are being used to | ||
57 | predict the consequences of climate change on the water balance of | 57 | predict the consequences of climate change on the water balance of | ||
58 | mountain watersheds. The models also constitute a valuable tool for | 58 | mountain watersheds. The models also constitute a valuable tool for | ||
59 | our operational services, such as periodic snow hydrological | 59 | our operational services, such as periodic snow hydrological | ||
60 | bulletins, which contribute to the federal flood prevention and | 60 | bulletins, which contribute to the federal flood prevention and | ||
61 | forecasting system.\r\n\r\nThe research group \u00abSnow | 61 | forecasting system.\r\n\r\nThe research group \u00abSnow | ||
62 | Hydrology\u00bb is based in Davos and ensures the link between other | 62 | Hydrology\u00bb is based in Davos and ensures the link between other | ||
63 | Davosian research groups and the research unit \u201dMountain | 63 | Davosian research groups and the research unit \u201dMountain | ||
64 | Hydrology and Mass Movements\u201d in Birmensdorf.", | 64 | Hydrology and Mass Movements\u201d in Birmensdorf.", | ||
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66 | "image_url": "", | 66 | "image_url": "", | ||
67 | "is_organization": true, | 67 | "is_organization": true, | ||
68 | "name": "snow-hydrology", | 68 | "name": "snow-hydrology", | ||
69 | "state": "active", | 69 | "state": "active", | ||
70 | "title": "Snow Hydrology", | 70 | "title": "Snow Hydrology", | ||
71 | "type": "organization" | 71 | "type": "organization" | ||
72 | }, | 72 | }, | ||
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74 | "private": false, | 74 | "private": false, | ||
75 | "publication": "{\"publication_year\": \"2023\", \"publisher\": | 75 | "publication": "{\"publication_year\": \"2023\", \"publisher\": | ||
76 | \"EnviDat\"}", | 76 | \"EnviDat\"}", | ||
77 | "publication_state": "published", | 77 | "publication_state": "published", | ||
78 | "related_datasets": "", | 78 | "related_datasets": "", | ||
79 | "related_publications": " | 79 | "related_publications": " | ||
80 | https://www.dora.lib4ri.ch/wsl/islandora/object/wsl:35982", | 80 | https://www.dora.lib4ri.ch/wsl/islandora/object/wsl:35982", | ||
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286 | "vocabulary_id": null | 287 | "vocabulary_id": null | ||
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289 | "title": "Turbulence in The Strongly Heterogeneous Near-Surface | 290 | "title": "Turbulence in The Strongly Heterogeneous Near-Surface | ||
290 | Boundary Layer over Patchy Snow", | 291 | Boundary Layer over Patchy Snow", | ||
291 | "type": "dataset", | 292 | "type": "dataset", | ||
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293 | "version": "1.0" | 294 | "version": "1.0" | ||
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