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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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\"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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\"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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\"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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  "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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  "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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  "metadata_created": "2025-01-08T10:02:49.361051",
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  "metadata_modified": "2025-01-10T09:07:42.176084",
            
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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 4 videos of capillary rise 
40
  "notes": "This dataset consists of 4 videos of capillary rise 
            
41
experiments performed with neutron radiography. The videos show the 
41
experiments performed with neutron radiography. The videos show the 
            
42
upward flow of water in glass columns filled with sand and snow or 
42
upward flow of water in glass columns filled with sand and snow or 
            
43
sand, gravel, and snow. The videos show the 2D evolution of the 
43
sand, gravel, and snow. The videos show the 2D evolution of the 
            
44
unitless optical density with time. The experiments were performed at 
44
unitless optical density with time. The experiments were performed at 
            
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the Paul Scherrer Institute (PSI) in Villigen, Switzerland. ",
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the Paul Scherrer Institute (PSI) in Villigen, Switzerland. ",
            
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  "num_resources": 2,
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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 
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    "description": "Snow avalanches \u2013 a type of fast-moving mass 
            
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movement \u2013 occur in snow covered mountain areas throughout the 
52
movement \u2013 occur in snow covered mountain areas throughout the 
            
53
world and may cause property damage and loss of life as they interfere 
53
world and may cause property damage and loss of life as they interfere 
            
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with human activities. Most avalanches release from terrain steeper 
54
with human activities. Most avalanches release from terrain steeper 
            
55
than about 30\u00b0 during or soon after snow storms, or are triggered 
55
than about 30\u00b0 during or soon after snow storms, or are triggered 
            
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by snow loading due to wind, or by a temperature change. Snow slab 
56
by snow loading due to wind, or by a temperature change. Snow slab 
            
57
avalanches can also be triggered artificially by, for example, people 
57
avalanches can also be triggered artificially by, for example, people 
            
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(usually unintentionally) or intentionally by explosives used as part 
58
(usually unintentionally) or intentionally by explosives used as part 
            
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of avalanche control programs. Today, most avalanche fatalities are 
59
of avalanche control programs. Today, most avalanche fatalities are 
            
60
recreationists. Independent of the triggering mode, the snowpack 
60
recreationists. Independent of the triggering mode, the snowpack 
            
61
layering is decisive for the instability of the snowpack which 
61
layering is decisive for the instability of the snowpack which 
            
62
consists of layers with varying properties. The complex microstructure 
62
consists of layers with varying properties. The complex microstructure 
            
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of snow and spatial variations in snow layer properties across the 
63
of snow and spatial variations in snow layer properties across the 
            
64
terrain limit the predictability of snow avalanches. Even today, it is 
64
terrain limit the predictability of snow avalanches. Even today, it is 
            
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not possible to predict the exact location, time and extent of an 
65
not possible to predict the exact location, time and extent of an 
            
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avalanche event. Improving avalanche prediction requires a better 
66
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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    "state": "active",
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    "title": "Avalanche Formation and Dynamics",
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  "publication": 
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  "publication": 
            
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      "name": "TRANSPORT",
175
      "name": "TRANSPORT",
            
176
      "state": "active",
176
      "state": "active",
            
177
      "vocabulary_id": null
177
      "vocabulary_id": null
            
178
    },
178
    },
            
179
    {
179
    {
            
180
      "display_name": "WATER",
180
      "display_name": "WATER",
            
181
      "id": "bfb14386-9f8c-42df-a144-1d000dfb5f16",
181
      "id": "bfb14386-9f8c-42df-a144-1d000dfb5f16",
            
182
      "name": "WATER",
182
      "name": "WATER",
            
183
      "state": "active",
183
      "state": "active",
            
184
      "vocabulary_id": null
184
      "vocabulary_id": null
            
185
    }
185
    }
            
186
  ],
186
  ],
            
187
  "title": "Capillary rise rise experiments in snow using neutron 
187
  "title": "Capillary rise rise experiments in snow using neutron 
            
188
radiography",
188
radiography",
            
189
  "type": "dataset",
189
  "type": "dataset",
            
190
  "url": null
190
  "url": null
            
191
}
191
}