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Research SLF\", \"affiliation_02\": \"\", \"affiliation_03\": \"\", 
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Research SLF\", \"affiliation_02\": \"\", \"affiliation_03\": \"\", 
            
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\"data_credit\": [\"collection\", \"validation\", \"curation\", 
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\"software\", \"publication\"], \"email\": 
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\"software\", \"publication\"], \"email\": 
            
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\"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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{\"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\", \"affiliation_02\": \"SLF\", \"affiliation_03\": \"\", 
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SLF\", \"affiliation_02\": \"SLF\", \"affiliation_03\": \"\", 
            
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\"data_credit\": [\"collection\", \"validation\", \"supervision\"], 
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\"data_credit\": [\"collection\", \"validation\", \"supervision\"], 
            
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\"email\": \"vanherwijnen@slf.ch\", \"given_name\": \"Alec\", 
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\"email\": \"vanherwijnen@slf.ch\", \"given_name\": \"Alec\", 
            
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\"identifier\": \"0000-0001-5637-6486\", \"name\": \"van Herwijnen\"}, 
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\"identifier\": \"0000-0001-5637-6486\", \"name\": \"van Herwijnen\"}, 
            
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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\", \"affiliation_02\": \"WSL\", \"affiliation_03\": \"ETH\", 
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SLF\", \"affiliation_02\": \"WSL\", \"affiliation_03\": \"ETH\", 
            
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\"data_credit\": \"supervision\", \"email\": \"schweizer@slf.ch\", 
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\"data_credit\": \"supervision\", \"email\": \"schweizer@slf.ch\", 
            
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\"given_name\": \"J\\u00fcrg\", \"identifier\": 
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\"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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  "author_email": null,
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  "author_email": null,
            
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  "creator_user_id": "c8312541-12f8-4533-a778-53f3d3e6a99b",
            
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  "date": "[{\"date\": \"2019-01-04\", \"date_type\": \"collected\", 
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  "date": "[{\"date\": \"2019-01-04\", \"date_type\": \"collected\", 
            
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\"end_date\": \"2019-03-19\"}]",
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\"end_date\": \"2019-03-19\"}]",
            
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  "doi": "10.16904/envidat.365",
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  "doi": "10.16904/envidat.365",
            
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  "funding": "[{\"grant_number\": \"Grant/Award: 200021_169424\", 
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  "funding": "[{\"grant_number\": \"Grant/Award: 200021_169424\", 
            
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\"institution\": \"Swiss National Science Foundation\", 
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\"institution\": \"Swiss National Science Foundation\", 
            
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\"institution_url\": \"\"}]",
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  "license_id": "wsl-data",
            
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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\", \"email\": \"bastian.bergfeld@slf.ch\", 
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Avalanche Research SLF\", \"email\": \"bastian.bergfeld@slf.ch\", 
            
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\"given_name\": \"Bastian\", \"identifier\": \"0000-0002-3316-1922\", 
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\"given_name\": \"Bastian\", \"identifier\": \"0000-0002-3316-1922\", 
            
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\"name\": \"Bergfeld\"}",
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\"name\": \"Bergfeld\"}",
            
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  "metadata_created": "2023-01-23T09:20:46.332986",
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  "metadata_modified": "2023-01-24T05:35:30.282574",
            
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  "name": 
41
  "name": 
            
42
ries-data-on-dynamic-crack-propagation-in-long-propagation-saw-tests",
42
ries-data-on-dynamic-crack-propagation-in-long-propagation-saw-tests",
            
43
  "notes": "This data set includes material and results described in 
43
  "notes": "This data set includes material and results described in 
            
44
the related research article:\r\n\r\nBergfeld, B., van Herwijnen A., 
44
the related research article:\r\n\r\nBergfeld, B., van Herwijnen A., 
            
45
Bobillier, G., Rosendahl P., Wei\u00dfgraeber P., Adam V., Dual, J., 
45
Bobillier, G., Rosendahl P., Wei\u00dfgraeber P., Adam V., Dual, J., 
            
46
and Schweizer, J.: Temporal evolution of crack propagation 
46
and Schweizer, J.: Temporal evolution of crack propagation 
            
47
characteristics in a weak snowpack layer: conditions of crack arrest 
47
characteristics in a weak snowpack layer: conditions of crack arrest 
            
48
and\r\nsustained propagation, Natural Hazards and Earth System 
48
and\r\nsustained propagation, Natural Hazards and Earth System 
            
49
Sciences, 2023.",
49
Sciences, 2023.",
            
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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 
55
    "description": "Snow avalanches \u2013 a type of fast-moving mass 
            
56
movement \u2013 occur in snow covered mountain areas throughout the 
56
movement \u2013 occur in snow covered mountain areas throughout the 
            
57
world and may cause property damage and loss of life as they interfere 
57
world and may cause property damage and loss of life as they interfere 
            
58
with human activities. Most avalanches release from terrain steeper 
58
with human activities. Most avalanches release from terrain steeper 
            
59
than about 30\u00b0 during or soon after snow storms, or are triggered 
59
than about 30\u00b0 during or soon after snow storms, or are triggered 
            
60
by snow loading due to wind, or by a temperature change. Snow slab 
60
by snow loading due to wind, or by a temperature change. Snow slab 
            
61
avalanches can also be triggered artificially by, for example, people 
61
avalanches can also be triggered artificially by, for example, people 
            
62
(usually unintentionally) or intentionally by explosives used as part 
62
(usually unintentionally) or intentionally by explosives used as part 
            
63
of avalanche control programs. Today, most avalanche fatalities are 
63
of avalanche control programs. Today, most avalanche fatalities are 
            
64
recreationists. Independent of the triggering mode, the snowpack 
64
recreationists. Independent of the triggering mode, the snowpack 
            
65
layering is decisive for the instability of the snowpack which 
65
layering is decisive for the instability of the snowpack which 
            
66
consists of layers with varying properties. The complex microstructure 
66
consists of layers with varying properties. The complex microstructure 
            
67
of snow and spatial variations in snow layer properties across the 
67
of snow and spatial variations in snow layer properties across the 
            
68
terrain limit the predictability of snow avalanches. Even today, it is 
68
terrain limit the predictability of snow avalanches. Even today, it is 
            
69
not possible to predict the exact location, time and extent of an 
69
not possible to predict the exact location, time and extent of an 
            
70
avalanche event. Improving avalanche prediction requires a better 
70
avalanche event. Improving avalanche prediction requires a better 
            
71
understanding of the underlying processes. ",
71
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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    "is_organization": true,
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    "is_organization": true,
            
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    "name": "avalanche-formation",
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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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  },
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  },
            
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  "owner_org": "a357f01f-845b-4b61-9ad0-f204d3332c52",
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  "owner_org": "a357f01f-845b-4b61-9ad0-f204d3332c52",
            
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  "private": false,
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  "private": false,
            
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  "publication": "{\"publication_year\": \"2023\", \"publisher\": 
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  "publication": "{\"publication_year\": \"2023\", \"publisher\": 
            
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\"EnviDat\"}",
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\"EnviDat\"}",
            
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  "publication_state": "pub_pending",
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  "publication_state": "reserved",
            
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  "related_datasets": "",
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  "related_datasets": "",
            
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  "related_publications": "Bergfeld, B., van Herwijnen, A., Bobillier, 
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  "related_publications": "Bergfeld, B., van Herwijnen, A., Bobillier, 
            
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G., Rosendahl P., Wei\u00dfgraeber P., Adam V., Dual, J., and 
87
G., Rosendahl P., Wei\u00dfgraeber P., Adam V., Dual, J., and 
            
88
Schweizer, J.: Temporal evolution of crack propagation characteristics 
88
Schweizer, J.: Temporal evolution of crack propagation characteristics 
            
89
in a weak snowpack layer: conditions of crack arrest and\r\nsustained 
89
in a weak snowpack layer: conditions of crack arrest and\r\nsustained 
            
90
propagation, Natural Hazards and Earth System Sciences, 2023.",
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propagation, Natural Hazards and Earth System Sciences, 2023.",
            
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  "relationships_as_object": [],
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  "relationships_as_object": [],
            
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  "relationships_as_subject": [],
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  "relationships_as_subject": [],
            
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  "resource_type": "dataset",
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  "resource_type": "dataset",
            
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  "resource_type_general": "dataset",
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  "resource_type_general": "dataset",
            
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  "resources": [
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      "description": "Snowpack data includes the elastic modulus 
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      "description": "Snowpack data includes the elastic modulus 
            
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(stiffness properties) of the slab, the elastic modulus of the weak 
101
(stiffness properties) of the slab, the elastic modulus of the weak 
            
102
layer, and the specific fracture energy of the weak layer determined 
102
layer, and the specific fracture energy of the weak layer determined 
            
103
with a homogeneous and a layered slab model. During crack propagation, 
103
with a homogeneous and a layered slab model. During crack propagation, 
            
104
we measured the crack speed, touchdown distance, crack arrest length 
104
we measured the crack speed, touchdown distance, crack arrest length 
            
105
and energy dissipation due to compaction and dynamic fracture.",
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and energy dissipation due to compaction and dynamic fracture.",
            
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      "created": "2023-01-23T09:45:55.282510",
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      "created": "2023-01-23T09:45:55.282510",
            
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      "description": "The videos show the cracking process in the 
133
      "description": "The videos show the cracking process in the 
            
134
Propagation Saw Tests (flat field). The upper panel shows strain on 
134
Propagation Saw Tests (flat field). The upper panel shows strain on 
            
135
top of the recorded movie frames. The second row shows vertical (w, 
135
top of the recorded movie frames. The second row shows vertical (w, 
            
136
blue line) and horizontal (u, orange line) displacement fields. The 
136
blue line) and horizontal (u, orange line) displacement fields. The 
            
137
third and fourth row show the first and second time derivatives, 
137
third and fourth row show the first and second time derivatives, 
            
138
namely the velocity and acceleration field.\r\n",
138
namely the velocity and acceleration field.\r\n",
            
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      "name": " Videos of crack propagation",
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      "name": " Videos of crack propagation",
            
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      "description": "Index of self-sustained crack propagation SSP 
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      "description": "Index of self-sustained crack propagation SSP 
            
167
(ssp_measured.xlsx) with time. The self-sustained crack propagation 
167
(ssp_measured.xlsx) with time. The self-sustained crack propagation 
            
168
index SSP was also modelled for simulated snow stratigraphy 
168
index SSP was also modelled for simulated snow stratigraphy 
            
169
(ssp_modelled.xlsx) using crack speed and critical cut length 
169
(ssp_modelled.xlsx) using crack speed and critical cut length 
            
170
parameterizations from Heierli (2005) and Richter et al. (2019), 
170
parameterizations from Heierli (2005) and Richter et al. (2019), 
            
171
respectively.",
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respectively.",
            
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      "description": "The snow cover model SNOWPACK (version 3.60) was 
            
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used to simulate the evolving snow stratigraphy at our field site. The 
200
used to simulate the evolving snow stratigraphy at our field site. The 
            
201
model was driven with data from an automatic weather station which was 
201
model was driven with data from an automatic weather station which was 
            
202
located 100m next to the field site (FLS_bunker_snowpack.smet). The 
202
located 100m next to the field site (FLS_bunker_snowpack.smet). The 
            
203
SNOWPACK initiation file (FLS_bunker_snowpack.ini) contains the 
203
SNOWPACK initiation file (FLS_bunker_snowpack.ini) contains the 
            
204
selected model parameters that result in the modeled snow stratigraphy 
204
selected model parameters that result in the modeled snow stratigraphy 
            
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(FLS_bunker_snowpack.pro).",
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    {
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      "display_name": "CRACK PROPAGATION",
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      "display_name": "CRACK PROPAGATION",
            
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      "id": "387726dc-dbe2-4c70-bdf1-414144a5ed04",
            
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      "name": "EXPERIMENT",
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      "name": "EXPERIMENT",
            
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      "state": "active",
            
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      "vocabulary_id": null
            
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    },
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    },
            
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    {
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    {
            
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      "display_name": "PROPAGATION SAW TEST",
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      "display_name": "PROPAGATION SAW TEST",
            
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      "id": "7e60b749-5e17-403a-9f87-c93b4ea16825",
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      "id": "7e60b749-5e17-403a-9f87-c93b4ea16825",
            
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      "name": "PROPAGATION SAW TEST",
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      "name": "PROPAGATION SAW TEST",
            
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      "state": "active",
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      "state": "active",
            
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    {
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    {
            
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      "display_name": "SNOW AVALANCHE",
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      "display_name": "SNOW AVALANCHE",
            
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      "id": "6083a08c-fd24-4e5a-bb20-559021b89c92",
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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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      "state": "active",
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      "state": "active",
            
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      "vocabulary_id": null
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      "vocabulary_id": null
            
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    },
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    },
            
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    {
271
    {
            
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      "display_name": "SNOW MECHANICS",
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      "display_name": "SNOW MECHANICS",
            
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      "id": "31bab9c5-b32e-452d-bce1-f7500696beab",
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      "id": "31bab9c5-b32e-452d-bce1-f7500696beab",
            
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      "name": "SNOW MECHANICS",
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      "name": "SNOW MECHANICS",
            
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      "state": "active",
            
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      "vocabulary_id": null
            
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    }
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    }
            
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  ],
278
  ],
            
279
  "title": "Time series data on dynamic crack propagation in long 
279
  "title": "Time series data on dynamic crack propagation in long 
            
280
propagation saw tests",
280
propagation saw tests",
            
281
  "type": "dataset",
281
  "type": "dataset",
            
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282
  "url": null,
            
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  "version": "1.0"
283
  "version": "1.0"
            
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}
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}