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  "author": "[{\"given_name\": \"Michael\", \"name\": \"Lombardo\", 
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  "author": "[{\"given_name\": \"Michael\", \"name\": \"Lombardo\", 
            
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\"email\": \"michael.lombardo@slf.ch\", \"data_credit\": []}, 
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\"email\": \"michael.lombardo@slf.ch\", \"data_credit\": []}, 
            
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{\"given_name\": \"Amelie\", \"name\": \"Fees\", \"email\": 
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{\"given_name\": \"Amelie\", \"name\": \"Fees\", \"email\": 
            
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\"amelie.fees@slf.ch\", \"data_credit\": [], \"identifier\": \"\", 
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\"amelie.fees@slf.ch\", \"data_credit\": [], \"identifier\": \"\", 
            
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\"affiliation\": \"WSL Institute for Snow and Avalanche Research 
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\"affiliation\": \"WSL Institute for Snow and Avalanche Research 
            
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SLF\"}, {\"given_name\": \"Anders\", \"name\": \"Kaestner\", 
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SLF\"}, {\"given_name\": \"Anders\", \"name\": \"Kaestner\", 
            
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\"email\": \"anders.kaestner@psi.ch\", \"data_credit\": [], 
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\"email\": \"anders.kaestner@psi.ch\", \"data_credit\": [], 
            
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\"identifier\": \"\", \"affiliation\": \"Paul Scherrer Institute 
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\"identifier\": \"\", \"affiliation\": \"Paul Scherrer Institute 
            
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PSI\"}, {\"given_name\": \"Alec\", \"name\": \"van Herwijnen\", 
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PSI\"}, {\"given_name\": \"Alec\", \"name\": \"van Herwijnen\", 
            
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\"email\": \"vanherwijnen@wsl.ch\", \"data_credit\": [], 
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\"email\": \"vanherwijnen@wsl.ch\", \"data_credit\": [], 
            
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\"identifier\": \"\", \"affiliation\": \"WSL Institute for Snow and 
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\"identifier\": \"\", \"affiliation\": \"WSL Institute for Snow and 
            
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Avalanche Research SLF\"}, {\"given_name\": \"J\\u00fcrg\", \"name\": 
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Avalanche Research SLF\"}, {\"given_name\": \"J\\u00fcrg\", \"name\": 
            
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\"Schweizer\", \"email\": \"schweizer@slf.ch\", \"data_credit\": [], 
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\"Schweizer\", \"email\": \"schweizer@slf.ch\", \"data_credit\": [], 
            
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\"identifier\": \"0000-0001-5076-2968\", \"affiliation\": \"WSL 
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\"identifier\": \"0000-0001-5076-2968\", \"affiliation\": \"WSL 
            
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Institute for Snow and Avalanche Research SLF\"}, {\"given_name\": 
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Institute for Snow and Avalanche Research SLF\"}, {\"given_name\": 
            
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\"Peter\", \"name\": \"Lehmann\", \"email\": 
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\"Peter\", \"name\": \"Lehmann\", \"email\": 
            
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\"peter.lehmann@env.ethz.ch\", \"data_credit\": [], \"identifier\": 
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\"peter.lehmann@env.ethz.ch\", \"data_credit\": [], \"identifier\": 
            
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\"\", \"affiliation\": \"ETH\"}]",
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\"\", \"affiliation\": \"ETH\"}]",
            
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  "date": 
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  "date": 
            
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:\"collected\",\"date\":\"2022-12-03\",\"end_date\":\"2022-12-07\"}]",
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:\"collected\",\"date\":\"2022-12-03\",\"end_date\":\"2022-12-07\"}]",
            
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  "doi": "10.16904/envidat.572",
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  "doi": "10.16904/envidat.572",
            
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  "funding": "[{\"institution\":\"Swiss National Science 
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  "funding": "[{\"institution\":\"Swiss National Science 
            
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tion\",\"grant_number\":\"200021-212949\",\"institution_url\":\"\"}]",
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tion\",\"grant_number\":\"200021-212949\",\"institution_url\":\"\"}]",
            
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  "groups": [],
            
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  "id": "44ba7f26-f741-4b92-a4ff-8e99dd8f689c",
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  "id": "44ba7f26-f741-4b92-a4ff-8e99dd8f689c",
            
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  "license_id": "cc-by",
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  "license_id": "cc-by",
            
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  "license_title": "Creative Commons Attribution",
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  "license_title": "Creative Commons Attribution",
            
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  "license_url": "https://creativecommons.org/licenses/by/4.0/",
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  "license_url": "https://creativecommons.org/licenses/by/4.0/",
            
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  "maintainer": 
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  "maintainer": 
            
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.lombardo@slf.ch\",\"given_name\":\"Michael\",\"name\":\"Lombardo\"}",
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.lombardo@slf.ch\",\"given_name\":\"Michael\",\"name\":\"Lombardo\"}",
            
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  "maintainer_email": null,
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  "maintainer_email": null,
            
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  "metadata_created": "2025-01-08T10:02:49.361051",
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  "metadata_created": "2025-01-08T10:02:49.361051",
            
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  "metadata_modified": "2025-01-21T09:23:41.292197",
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  "metadata_modified": "2025-01-21T09:24:15.768260",
            
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  "name": 
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  "name": 
            
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"capillary-rise-rise-experiments-in-snow-using-neutron-radiography",
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"capillary-rise-rise-experiments-in-snow-using-neutron-radiography",
            
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  "notes": "This dataset consists of data related to capillary rise 
40
  "notes": "This dataset consists of data related to capillary rise 
            
41
experiments performed with neutron radiography. There are 4 videos of 
41
experiments performed with neutron radiography. There are 4 videos of 
            
42
capillary rise experiments as well as the files used to perform the 
42
capillary rise experiments as well as the files used to perform the 
            
43
inverse fitting with Hydrus. The videos show the upward flow of water 
43
inverse fitting with Hydrus. The videos show the upward flow of water 
            
44
in glass columns filled with sand and snow or sand, gravel, and snow. 
44
in glass columns filled with sand and snow or sand, gravel, and snow. 
            
45
The videos show the 2D evolution of the unitless optical density with 
45
The videos show the 2D evolution of the unitless optical density with 
            
46
time. The Hydrus files were used to fit the parameter values of the 
46
time. The Hydrus files were used to fit the parameter values of the 
            
47
Mualem-van Genuchten model. The experiments were performed at the Paul 
47
Mualem-van Genuchten model. The experiments were performed at the Paul 
            
48
Scherrer Institute (PSI) in Villigen, Switzerland. ",
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Scherrer Institute (PSI) in Villigen, Switzerland. ",
            
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  "num_resources": 4,
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  "num_resources": 4,
            
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  "num_tags": 6,
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  "num_tags": 6,
            
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  "organization": {
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  "organization": {
            
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    "approval_status": "approved",
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    "approval_status": "approved",
            
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    "created": "2019-09-27T12:40:13.473824",
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    "created": "2019-09-27T12:40:13.473824",
            
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    "description": "Snow avalanches \u2013 a type of fast-moving mass 
54
    "description": "Snow avalanches \u2013 a type of fast-moving mass 
            
55
movement \u2013 occur in snow covered mountain areas throughout the 
55
movement \u2013 occur in snow covered mountain areas throughout the 
            
56
world and may cause property damage and loss of life as they interfere 
56
world and may cause property damage and loss of life as they interfere 
            
57
with human activities. Most avalanches release from terrain steeper 
57
with human activities. Most avalanches release from terrain steeper 
            
58
than about 30\u00b0 during or soon after snow storms, or are triggered 
58
than about 30\u00b0 during or soon after snow storms, or are triggered 
            
59
by snow loading due to wind, or by a temperature change. Snow slab 
59
by snow loading due to wind, or by a temperature change. Snow slab 
            
60
avalanches can also be triggered artificially by, for example, people 
60
avalanches can also be triggered artificially by, for example, people 
            
61
(usually unintentionally) or intentionally by explosives used as part 
61
(usually unintentionally) or intentionally by explosives used as part 
            
62
of avalanche control programs. Today, most avalanche fatalities are 
62
of avalanche control programs. Today, most avalanche fatalities are 
            
63
recreationists. Independent of the triggering mode, the snowpack 
63
recreationists. Independent of the triggering mode, the snowpack 
            
64
layering is decisive for the instability of the snowpack which 
64
layering is decisive for the instability of the snowpack which 
            
65
consists of layers with varying properties. The complex microstructure 
65
consists of layers with varying properties. The complex microstructure 
            
66
of snow and spatial variations in snow layer properties across the 
66
of snow and spatial variations in snow layer properties across the 
            
67
terrain limit the predictability of snow avalanches. Even today, it is 
67
terrain limit the predictability of snow avalanches. Even today, it is 
            
68
not possible to predict the exact location, time and extent of an 
68
not possible to predict the exact location, time and extent of an 
            
69
avalanche event. Improving avalanche prediction requires a better 
69
avalanche event. Improving avalanche prediction requires a better 
            
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understanding of the underlying processes. ",
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understanding of the underlying processes. ",
            
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    "name": "avalanche-formation",
            
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    "state": "active",
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    "state": "active",
            
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    "title": "Avalanche Formation and Dynamics",
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    "title": "Avalanche Formation and Dynamics",
            
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    "type": "organization"
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    "type": "organization"
            
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  "private": false,
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  "publication": 
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  "publication": 
            
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"{\"publisher\":\"EnviDat\",\"publication_year\":\"2025\"}",
            
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  "publication_state": "published",
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the hydraulic conductivity.",
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the hydraulic conductivity.",
            
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