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Research SLF, Davos, Switzerland\", \"affiliation_02\": \"\", 
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Research SLF, Davos, Switzerland\", \"affiliation_02\": \"\", 
            
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\"email\": \"bastian.bergfeld@slf.ch\", \"given_name\": \"Bastian\", 
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\"email\": \"bastian.bergfeld@slf.ch\", \"given_name\": \"Bastian\", 
            
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\"identifier\": \"0000-0002-3316-1922\", \"name\": \"Bergfeld\"}, 
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\"identifier\": \"0000-0002-3316-1922\", \"name\": \"Bergfeld\"}, 
            
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{\"affiliation\": \"WSL Institute for Snow and Avalanche Research SLF, 
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{\"affiliation\": \"WSL Institute for Snow and Avalanche Research SLF, 
            
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Davos, Switzerland\", \"affiliation_02\": \"\", \"affiliation_03\": 
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Davos, Switzerland\", \"affiliation_02\": \"\", \"affiliation_03\": 
            
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\"\", \"data_credit\": [\"collection\", \"supervision\"], \"email\": 
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\"vanherwijnen@slf.ch\", \"given_name\": \"Alec\", \"identifier\": 
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\"vanherwijnen@slf.ch\", \"given_name\": \"Alec\", \"identifier\": 
            
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\"0000-0001-5637-6486\", \"name\": \"van Herwijnen\"}, 
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\"0000-0001-5637-6486\", \"name\": \"van Herwijnen\"}, 
            
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{\"affiliation\": \"WSL Institute for Snow and Avalanche Research SLF, 
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{\"affiliation\": \"WSL Institute for Snow and Avalanche Research SLF, 
            
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Davos, Switzerland\", \"affiliation_02\": \"\", \"affiliation_03\": 
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Davos, Switzerland\", \"affiliation_02\": \"\", \"affiliation_03\": 
            
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\"\", \"data_credit\": \"software\", \"email\": 
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\"\", \"data_credit\": \"software\", \"email\": 
            
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\"benjamin.reuter@slf.ch\", \"given_name\": \"Benjamin\", 
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\"benjamin.reuter@slf.ch\", \"given_name\": \"Benjamin\", 
            
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\"identifier\": \"0000-0002-7302-3858\", \"name\": \"Reuter\"}, 
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\"identifier\": \"0000-0002-7302-3858\", \"name\": \"Reuter\"}, 
            
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{\"affiliation\": \"WSL Institute for Snow and Avalanche Research SLF, 
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{\"affiliation\": \"WSL Institute for Snow and Avalanche Research SLF, 
            
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Davos, Switzerland\", \"affiliation_02\": \"\", \"affiliation_03\": 
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Davos, Switzerland\", \"affiliation_02\": \"\", \"affiliation_03\": 
            
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\"\", \"email\": \"gr\\u00e9goire.bobillier@slf.ch\", \"given_name\": 
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\"Gr\\u00e9goire\", \"identifier\": \"0000-0002-6913-5611\", \"name\": 
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\"Gr\\u00e9goire\", \"identifier\": \"0000-0002-6913-5611\", \"name\": 
            
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\"Bobillier\"}, {\"affiliation\": \"Institute for Mechanical Systems, 
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\"Bobillier\"}, {\"affiliation\": \"Institute for Mechanical Systems, 
            
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ETH Zurich, Zurich, Switzerland\", \"affiliation_02\": \"\", 
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ETH Zurich, Zurich, Switzerland\", \"affiliation_02\": \"\", 
            
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\"affiliation_03\": \"\", \"data_credit\": \"supervision\", \"email\": 
            
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\"dual@imes.mavt.ethz.ch\", \"given_name\": \"J\\u00fcrg\", 
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\"dual@imes.mavt.ethz.ch\", \"given_name\": \"J\\u00fcrg\", 
            
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{\"affiliation\": \"WSL Institute for Snow and Avalanche Research SLF, 
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{\"affiliation\": \"WSL Institute for Snow and Avalanche Research SLF, 
            
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Davos, Switzerland\", \"affiliation_02\": \"\", \"affiliation_03\": 
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Davos, Switzerland\", \"affiliation_02\": \"\", \"affiliation_03\": 
            
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\"\", \"data_credit\": \"supervision\", \"email\": 
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\"\", \"data_credit\": \"supervision\", \"email\": 
            
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\"schweizer@slf.ch\", \"given_name\": \"J\\u00fcrg\", \"identifier\": 
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\"schweizer@slf.ch\", \"given_name\": \"J\\u00fcrg\", \"identifier\": 
            
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\"0000-0001-5076-2968\", \"name\": \"Schweizer\"}]",
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\"0000-0001-5076-2968\", \"name\": \"Schweizer\"}]",
            
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  "date": "[{\"date\": \"2021-06-23\", \"date_type\": \"collected\", 
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  "date": "[{\"date\": \"2021-06-23\", \"date_type\": \"collected\", 
            
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  "doi": "10.16904/envidat.231",
            
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  "funding": "[{\"grant_number\": \"200021_169424\", \"institution\": 
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  "funding": "[{\"grant_number\": \"200021_169424\", \"institution\": 
            
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\"Swiss National Science Foundation\", \"institution_url\": \"\"}]",
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\"Swiss National Science Foundation\", \"institution_url\": \"\"}]",
            
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  "license_title": "WSL Data Policy",
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  "license_title": "WSL Data Policy",
            
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  "license_url": 
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  "license_url": 
            
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ps://www.wsl.ch/en/about-wsl/programmes-and-initiatives/envidat.html",
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ps://www.wsl.ch/en/about-wsl/programmes-and-initiatives/envidat.html",
            
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  "maintainer": "{\"affiliation\": \"WSL Institute for Snow and 
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  "maintainer": "{\"affiliation\": \"WSL Institute for Snow and 
            
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Avalanche Research SLF, Davos, Switzerland\", \"email\": 
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Avalanche Research SLF, Davos, Switzerland\", \"email\": 
            
49
\"bastian.bergfeld@slf.ch\", \"given_name\": \"Bastian\", 
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\"bastian.bergfeld@slf.ch\", \"given_name\": \"Bastian\", 
            
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\"identifier\": \"0000-0002-3316-1922\", \"name\": \"Bergfeld\"}",
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\"identifier\": \"0000-0002-3316-1922\", \"name\": \"Bergfeld\"}",
            
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  "maintainer_email": null,
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  "maintainer_email": null,
            
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  "metadata_created": "2021-06-23T14:00:28.699523",
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  "metadata_created": "2021-06-23T14:00:28.699523",
            
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  "metadata_modified": "2021-06-23T15:57:15.472067",
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  "metadata_modified": "2021-06-25T08:50:39.617295",
            
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  "name": 
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  "name": 
            
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agation-in-weak-snowpack-layers-insights-from-high-speed-photography",
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agation-in-weak-snowpack-layers-insights-from-high-speed-photography",
            
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  "notes": "This data set includes material and results described in 
56
  "notes": "This data set includes material and results described in 
            
57
the related research article (Bergfeld et al. (2021)). \r\n# Context: 
57
the related research article (Bergfeld et al. (2021)). \r\n# Context: 
            
58
\r\nIn order to study crack propagation in weak snow pack layers in 
58
\r\nIn order to study crack propagation in weak snow pack layers in 
            
59
great detail, we recorded Propagation Saw Test (PST) experiments using 
59
great detail, we recorded Propagation Saw Test (PST) experiments using 
            
60
a high-speed camera and applied digital image correlation (DIC) to 
60
a high-speed camera and applied digital image correlation (DIC) to 
            
61
derive displacement and strain fields in the slab, weak layer, and 
61
derive displacement and strain fields in the slab, weak layer, and 
            
62
substrate. We demonstrated the versatility and accuracy of the DIC 
62
substrate. We demonstrated the versatility and accuracy of the DIC 
            
63
method by showing measurements from three PST experiments, resulting 
63
method by showing measurements from three PST experiments, resulting 
            
64
in slab fracture, crack arrest and full propagation in the related 
64
in slab fracture, crack arrest and full propagation in the related 
            
65
publication. \r\n# Content:\r\n- Supplementary material for related 
65
publication. \r\n# Content:\r\n- Supplementary material for related 
            
66
publication\r\n- Ilustrative videos showing crack propagation\r\n- 
66
publication\r\n- Ilustrative videos showing crack propagation\r\n- 
            
67
High-speed recordings of the Experiments \r\n(the raw .cine files are 
67
High-speed recordings of the Experiments \r\n(the raw .cine files are 
            
68
available upon request)\r\n",
68
available upon request)\r\n",
            
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  "num_resources": 3,
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  "num_resources": 3,
            
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  "num_tags": 5,
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  "num_tags": 5,
            
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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 
74
    "description": "Snow avalanches \u2013 a type of fast-moving mass 
            
75
movement \u2013 occur in snow covered mountain areas throughout the 
75
movement \u2013 occur in snow covered mountain areas throughout the 
            
76
world and may cause property damage and loss of life as they interfere 
76
world and may cause property damage and loss of life as they interfere 
            
77
with human activities. Most avalanches release from terrain steeper 
77
with human activities. Most avalanches release from terrain steeper 
            
78
than about 30\u00b0 during or soon after snow storms, or are triggered 
78
than about 30\u00b0 during or soon after snow storms, or are triggered 
            
79
by snow loading due to wind, or by a temperature change. Snow slab 
79
by snow loading due to wind, or by a temperature change. Snow slab 
            
80
avalanches can also be triggered artificially by, for example, people 
80
avalanches can also be triggered artificially by, for example, people 
            
81
(usually unintentionally) or intentionally by explosives used as part 
81
(usually unintentionally) or intentionally by explosives used as part 
            
82
of avalanche control programs. Today, most avalanche fatalities are 
82
of avalanche control programs. Today, most avalanche fatalities are 
            
83
recreationists. Independent of the triggering mode, the snowpack 
83
recreationists. Independent of the triggering mode, the snowpack 
            
84
layering is decisive for the instability of the snowpack which 
84
layering is decisive for the instability of the snowpack which 
            
85
consists of layers with varying properties. The complex microstructure 
85
consists of layers with varying properties. The complex microstructure 
            
86
of snow and spatial variations in snow layer properties across the 
86
of snow and spatial variations in snow layer properties across the 
            
87
terrain limit the predictability of snow avalanches. Even today, it is 
87
terrain limit the predictability of snow avalanches. Even today, it is 
            
88
not possible to predict the exact location, time and extent of an 
88
not possible to predict the exact location, time and extent of an 
            
89
avalanche event. Improving avalanche prediction requires a better 
89
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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    "id": "a357f01f-845b-4b61-9ad0-f204d3332c52",
            
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    "image_url": "2019-09-27-104013.456832slf.png",
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    "image_url": "2019-09-27-104013.456832slf.png",
            
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    "is_organization": true,
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    "state": "active",
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  "publication": "{\"publication_year\": \"2021\", \"publisher\": 
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  "publication": "{\"publication_year\": \"2021\", \"publisher\": 
            
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\"EnviDat\"}",
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\"EnviDat\"}",
            
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  "publication_state": "published",
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  "publication_state": "published",
            
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  "related_datasets": "",
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  "related_datasets": "",
            
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  "related_publications": "https://doi.org/10.5194/tc-2020-360",
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  "related_publications": "https://doi.org/10.5194/tc-2020-360",
            
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      "description": "# Supplementary material to the publication 
            
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Bergfeld et al 2021\r\n- description of the reverse crack\r\n- 
            
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additional snow pack parameters derived from the SMP measurements",
            
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      "description": "The videos show the cracking process in three 
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      "description": "The videos show the cracking process in three 
            
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example Propagation Saw Tests (flat field). The upper panel shows 
145
example Propagation Saw Tests (flat field). The upper panel shows 
            
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strain on top of the recorded movie frames. The second row shows 
146
strain on top of the recorded movie frames. The second row shows 
            
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vertical (*w*, blue line) and horizontal (*u*, orange line) 
147
vertical (*w*, blue line) and horizontal (*u*, orange line) 
            
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displacement fields. The third and fourth row show the first and 
148
displacement fields. The third and fourth row show the first and 
            
120
second time derivatives, namely the velocity and acceleration field. 
149
second time derivatives, namely the velocity and acceleration field. 
            
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",
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      "description": "# Supplementary material to the publication 

            
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Bergfeld et al 2021\r\n- description of the reverse crack\r\n- 

            
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additional snow pack parameters derived from the SMP measurements",

            
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  "tags": [
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  "tags": [
            
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    {
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    {
            
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      "display_name": "CRACK PROPAGATION",
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      "display_name": "CRACK PROPAGATION",
            
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      "name": "EXPERIMENT",
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    {
            
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      "display_name": "SNOW",
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      "display_name": "SNOW",
            
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      "id": "c4e9ea3f-6149-45ce-8631-c872b96a9537",
            
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      "name": "SNOW",
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      "display_name": "SNOW AVALANCHE",
            
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      "id": "6083a08c-fd24-4e5a-bb20-559021b89c92",
            
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      "name": "SNOW AVALANCHE",
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      "name": "SNOW AVALANCHE",
            
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      "display_name": "SNOW MECHANICS",
            
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      "id": "31bab9c5-b32e-452d-bce1-f7500696beab",
            
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      "name": "SNOW MECHANICS",
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      "state": "active",
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    }
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    }
            
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  ],
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  ],
            
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  "title": "Crack propagation in weak snowpack layers: Insights from 
244
  "title": "Crack propagation in weak snowpack layers: Insights from 
            
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high-speed photography",
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high-speed photography",
            
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  "type": "dataset",
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  "version": "1.0"
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}
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}