Changes
On March 25, 2024 at 1:29:28 PM UTC, Oceane Hames:
-
Updated description of snowBedFoam: an OpenFOAM Eulerian-Lagrangian solver for modelling snow transport from
snowBedFoam 1.0. is a snow transport solver implemented in the computational fluid dynamics software OpenFOAM (The OpenFOAM Foundation, 2024). It is adapted from the standard multi-phase flow solver DPMFoam for application in snow-influenced environments. To simulate aeolian snow transport, snowBedFoam 1.0. handles coupled Eulerian–Lagrangian phases, which involve a finite number of particles (snow) spread in a continuous phase (air). The snow erosion and deposition are modelled through physics-based equations similar to the ones employed in the well-established LES-Lagrangian Stochastic Model (Comola and Lehning, 2017 ; Sharma et al., 2018 ; Melo et al., 2022). This modelling approach is computationally intensive and thus adapted to simulate snow movement and distribution on small scale terrain. First, snowBedFoam 1.0. was applied to topographical data collected on Arctic sea ice during the MOSAiC expedition (Clemens-Sewall, 2021). Together with atmospheric data from the MOSAiC Met City (Shupe et al., 2021) used for the fluid forcing, the model was able to accurately simulate the zones of erosion and deposition of snow along a complex ice ridge structure (Hames et al., 2022). Second, snowBedFoam 1.0. was used to simulate the snow distribution around the German Antarctic research station Neumayer Station III. The effect of snow properties, fluid forcing and aerodynamic structures on the snow accumulation were assessed. snowBedFoam 1.0 was implemented in 2 different OpenFOAM versions, namely OpenFOAM-2.3.0 and OpenFOAM-5.0. The latter offers more options for turbulence models and boundary conditions. The fundamental model equations were not changed from one implementation to the other, thus both still correspond to snowBedFoam 1.0. The two branches are called snowBedFoam-v1-2.3.0 (OpenFOAM-2.3.0) and snowBedFoam-v1-5.0 (OpenFOAM-5.0). The core codes of snowBedFoam 1.0. are directly accessible on the WSL/SLF GitLab repository (more details in the Resources section).
tosnowBedFoam 1.0. is a snow transport solver implemented in the computational fluid dynamics software OpenFOAM. It is adapted from the standard multi-phase flow solver DPMFoam for application in snow-influenced environments. To simulate aeolian snow transport, snowBedFoam 1.0. handles coupled Eulerian–Lagrangian phases, which involve a finite number of particles (snow) spread in a continuous phase (air). The snow erosion and deposition are modelled through physics-based equations similar to the ones employed in the well-established LES-Lagrangian Stochastic Model (Comola and Lehning, 2017 ; Sharma et al., 2018 ; Melo et al., 2022). This modelling approach is computationally intensive and thus adapted to simulate snow movement and distribution on small scale terrain. First, snowBedFoam 1.0. was applied to topographical data collected on Arctic sea ice during the MOSAiC expedition (Clemens-Sewall, 2021). Together with atmospheric data from the MOSAiC Met City (Shupe et al., 2021) used for the fluid forcing, the model was able to accurately simulate the zones of erosion and deposition of snow along a complex ice ridge structure (Hames et al., 2022). Second, snowBedFoam 1.0. was used to simulate the snow distribution around the German Antarctic research station Neumayer Station III. The effect of snow properties, fluid forcing and aerodynamic structures on the snow accumulation were assessed. snowBedFoam 1.0 was implemented in 2 different OpenFOAM versions, namely OpenFOAM-2.3.0 and OpenFOAM-5.0. The latter offers more options for turbulence models and boundary conditions. The fundamental model equations were not changed from one implementation to the other, thus both still correspond to snowBedFoam 1.0. The two branches are called snowBedFoam-v1-2.3.0 (OpenFOAM-2.3.0) and snowBedFoam-v1-5.0 (OpenFOAM-5.0). The core codes of snowBedFoam 1.0. are directly accessible on the WSL/SLF GitLab repository (more details in the Resources section).
f | 1 | { | f | 1 | { |
2 | "author": "[{\"affiliation\": \"WSL\", \"affiliation_02\": \"SLF\", | 2 | "author": "[{\"affiliation\": \"WSL\", \"affiliation_02\": \"SLF\", | ||
3 | \"affiliation_03\": \"EPFL\", \"data_credit\": \"software\", | 3 | \"affiliation_03\": \"EPFL\", \"data_credit\": \"software\", | ||
4 | \"email\": \"hames.oceane@gmail.com\", \"given_name\": | 4 | \"email\": \"hames.oceane@gmail.com\", \"given_name\": | ||
5 | \"Oc\\u00e9ane\", \"identifier\": \"\", \"name\": \"Hames\"}, | 5 | \"Oc\\u00e9ane\", \"identifier\": \"\", \"name\": \"Hames\"}, | ||
6 | {\"affiliation\": \"EPFL\", \"affiliation_02\": \"CRYOS\", | 6 | {\"affiliation\": \"EPFL\", \"affiliation_02\": \"CRYOS\", | ||
7 | \"affiliation_03\": \"\", \"data_credit\": [\"software\", | 7 | \"affiliation_03\": \"\", \"data_credit\": [\"software\", | ||
8 | \"supervision\"], \"email\": \"mahdi.jafari@epfl.ch\", \"given_name\": | 8 | \"supervision\"], \"email\": \"mahdi.jafari@epfl.ch\", \"given_name\": | ||
9 | \"Mahdi\", \"identifier\": \"\", \"name\": \"Jafari\"}, | 9 | \"Mahdi\", \"identifier\": \"\", \"name\": \"Jafari\"}, | ||
10 | {\"affiliation\": \"WSL\", \"affiliation_02\": \"SLF\", | 10 | {\"affiliation\": \"WSL\", \"affiliation_02\": \"SLF\", | ||
11 | \"affiliation_03\": \"EPFL\", \"data_credit\": \"supervision\", | 11 | \"affiliation_03\": \"EPFL\", \"data_credit\": \"supervision\", | ||
12 | \"email\": \"lehning@slf.ch\", \"given_name\": \"Michael\", | 12 | \"email\": \"lehning@slf.ch\", \"given_name\": \"Michael\", | ||
13 | \"identifier\": \"\", \"name\": \"Lehning\"}]", | 13 | \"identifier\": \"\", \"name\": \"Lehning\"}]", | ||
14 | "author_email": null, | 14 | "author_email": null, | ||
15 | "creator_user_id": "16379126-7832-4ddf-b7b2-4e1f408d532e", | 15 | "creator_user_id": "16379126-7832-4ddf-b7b2-4e1f408d532e", | ||
16 | "date": "[{\"date\": \"2019-12-03\", \"date_type\": \"created\", | 16 | "date": "[{\"date\": \"2019-12-03\", \"date_type\": \"created\", | ||
17 | \"end_date\": \"\"}]", | 17 | \"end_date\": \"\"}]", | ||
18 | "doi": "10.16904/envidat.223", | 18 | "doi": "10.16904/envidat.223", | ||
19 | "funding": "[{\"grant_number\": \"\", \"institution\": \"Swiss | 19 | "funding": "[{\"grant_number\": \"\", \"institution\": \"Swiss | ||
20 | National Science Foundation\", \"institution_url\": | 20 | National Science Foundation\", \"institution_url\": | ||
21 | \"http://www.snf.ch/en/Pages/default.aspx\"}]", | 21 | \"http://www.snf.ch/en/Pages/default.aspx\"}]", | ||
22 | "groups": [], | 22 | "groups": [], | ||
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24 | "isopen": true, | 24 | "isopen": true, | ||
25 | "language": "en", | 25 | "language": "en", | ||
26 | "license_id": "cc-by-sa", | 26 | "license_id": "cc-by-sa", | ||
27 | "license_title": "Creative Commons Attribution Share-Alike | 27 | "license_title": "Creative Commons Attribution Share-Alike | ||
28 | (CC-BY-SA)", | 28 | (CC-BY-SA)", | ||
29 | "license_url": "https://creativecommons.org/licenses/by-sa/4.0/", | 29 | "license_url": "https://creativecommons.org/licenses/by-sa/4.0/", | ||
30 | "maintainer": "{\"affiliation\": \"WSL\", \"email\": | 30 | "maintainer": "{\"affiliation\": \"WSL\", \"email\": | ||
31 | \"hames.oceane@gmail.com\", \"given_name\": \"Oc\u00e9ane\", | 31 | \"hames.oceane@gmail.com\", \"given_name\": \"Oc\u00e9ane\", | ||
32 | \"identifier\": \"\", \"name\": \"Hames\"}", | 32 | \"identifier\": \"\", \"name\": \"Hames\"}", | ||
33 | "maintainer_email": null, | 33 | "maintainer_email": null, | ||
34 | "metadata_created": "2021-05-20T09:50:58.431619", | 34 | "metadata_created": "2021-05-20T09:50:58.431619", | ||
n | 35 | "metadata_modified": "2024-03-25T12:11:24.984258", | n | 35 | "metadata_modified": "2024-03-25T13:29:28.799184", |
36 | "name": "snow-accumulation-on-arctic-sea-ice-during-mosaic", | 36 | "name": "snow-accumulation-on-arctic-sea-ice-during-mosaic", | ||
37 | "notes": "snowBedFoam 1.0. is a snow transport solver implemented in | 37 | "notes": "snowBedFoam 1.0. is a snow transport solver implemented in | ||
t | 38 | the computational fluid dynamics software OpenFOAM (The OpenFOAM | t | 38 | the computational fluid dynamics software OpenFOAM. It is adapted from |
39 | Foundation, 2024). It is adapted from the standard multi-phase flow | 39 | the standard multi-phase flow solver DPMFoam for application in | ||
40 | solver DPMFoam for application in snow-influenced environments. \n\nTo | 40 | snow-influenced environments. \n\nTo simulate aeolian snow transport, | ||
41 | simulate aeolian snow transport, snowBedFoam 1.0. handles coupled | 41 | snowBedFoam 1.0. handles coupled Eulerian\u2013Lagrangian phases, | ||
42 | Eulerian\u2013Lagrangian phases, which involve a finite number of | 42 | which involve a finite number of particles (snow) spread in a | ||
43 | particles (snow) spread in a continuous phase (air). The snow erosion | 43 | continuous phase (air). The snow erosion and deposition are modelled | ||
44 | and deposition are modelled through physics-based equations similar to | 44 | through physics-based equations similar to the ones employed in the | ||
45 | the ones employed in the well-established LES-Lagrangian Stochastic | 45 | well-established LES-Lagrangian Stochastic Model (Comola and Lehning, | ||
46 | Model (Comola and Lehning, 2017 ; Sharma et al., 2018 ; Melo et al., | 46 | 2017 ; Sharma et al., 2018 ; Melo et al., 2022). This modelling | ||
47 | 2022). This modelling approach is computationally intensive and thus | 47 | approach is computationally intensive and thus adapted to simulate | ||
48 | adapted to simulate snow movement and distribution on small scale | 48 | snow movement and distribution on small scale terrain.\n\nFirst, | ||
49 | terrain.\n\nFirst, snowBedFoam 1.0. was applied to topographical data | 49 | snowBedFoam 1.0. was applied to topographical data collected on Arctic | ||
50 | collected on Arctic sea ice during the MOSAiC expedition | 50 | sea ice during the MOSAiC expedition (Clemens-Sewall, 2021). Together | ||
51 | (Clemens-Sewall, 2021). Together with atmospheric data from the MOSAiC | 51 | with atmospheric data from the MOSAiC Met City (Shupe et al., 2021) | ||
52 | Met City (Shupe et al., 2021) used for the fluid forcing, the model | 52 | used for the fluid forcing, the model was able to accurately simulate | ||
53 | was able to accurately simulate the zones of erosion and deposition of | 53 | the zones of erosion and deposition of snow along a complex ice ridge | ||
54 | snow along a complex ice ridge structure (Hames et al., 2022). | 54 | structure (Hames et al., 2022). \n\nSecond, snowBedFoam 1.0. was used | ||
55 | \n\nSecond, snowBedFoam 1.0. was used to simulate the snow | 55 | to simulate the snow distribution around the German Antarctic research | ||
56 | distribution around the German Antarctic research station Neumayer | ||||
57 | Station III. The effect of snow properties, fluid forcing and | 56 | station Neumayer Station III. The effect of snow properties, fluid | ||
58 | aerodynamic structures on the snow accumulation were assessed. | 57 | forcing and aerodynamic structures on the snow accumulation were | ||
59 | \n\nsnowBedFoam 1.0 was implemented in 2 different OpenFOAM versions, | 58 | assessed. \n\nsnowBedFoam 1.0 was implemented in 2 different OpenFOAM | ||
60 | namely OpenFOAM-2.3.0 and OpenFOAM-5.0. The latter offers more options | 59 | versions, namely OpenFOAM-2.3.0 and OpenFOAM-5.0. The latter offers | ||
61 | for turbulence models and boundary conditions. The fundamental model | 60 | more options for turbulence models and boundary conditions. The | ||
62 | equations were not changed from one implementation to the other, thus | 61 | fundamental model equations were not changed from one implementation | ||
63 | both still correspond to snowBedFoam 1.0. The two branches are called | 62 | to the other, thus both still correspond to snowBedFoam 1.0. The two | ||
64 | snowBedFoam-v1-2.3.0 (OpenFOAM-2.3.0) and snowBedFoam-v1-5.0 | 63 | branches are called snowBedFoam-v1-2.3.0 (OpenFOAM-2.3.0) and | ||
65 | (OpenFOAM-5.0). The core codes of snowBedFoam 1.0. are directly | 64 | snowBedFoam-v1-5.0 (OpenFOAM-5.0). The core codes of snowBedFoam 1.0. | ||
66 | accessible on the WSL/SLF GitLab repository (more details in the | 65 | are directly accessible on the WSL/SLF GitLab repository (more details | ||
67 | Resources section).\n ", | 66 | in the Resources section).\n ", | ||
68 | "num_resources": 6, | 67 | "num_resources": 6, | ||
69 | "num_tags": 6, | 68 | "num_tags": 6, | ||
70 | "organization": { | 69 | "organization": { | ||
71 | "approval_status": "approved", | 70 | "approval_status": "approved", | ||
72 | "created": "2016-11-17T12:24:20.447699", | 71 | "created": "2016-11-17T12:24:20.447699", | ||
73 | "description": "CRYOS is the EPFL laboratory of the WSL/SLF - EPFL | 72 | "description": "CRYOS is the EPFL laboratory of the WSL/SLF - EPFL | ||
74 | joint appointment for Prof. Michael Lehning. At his WSL side, Prof. | 73 | joint appointment for Prof. Michael Lehning. At his WSL side, Prof. | ||
75 | Michael Lehning is head of the research unit \"Snow and Permafrost\" | 74 | Michael Lehning is head of the research unit \"Snow and Permafrost\" | ||
76 | at SLF in Davos.\r\n \r\n###General Mission\r\nThe laboratory of | 75 | at SLF in Davos.\r\n \r\n###General Mission\r\nThe laboratory of | ||
77 | cryospheric sciences investigates the processes that shape snow and | 76 | cryospheric sciences investigates the processes that shape snow and | ||
78 | ice in mountains and polar regions. In particular, snow cover | 77 | ice in mountains and polar regions. In particular, snow cover | ||
79 | processes, snow-atmosphere interactions and mountain hydrology are in | 78 | processes, snow-atmosphere interactions and mountain hydrology are in | ||
80 | the focus of current research. This includes a strive for deeper | 79 | the focus of current research. This includes a strive for deeper | ||
81 | understanding of the complicated mass and energy exchange processes | 80 | understanding of the complicated mass and energy exchange processes | ||
82 | within, above and below a snow cover but also predictions of future | 81 | within, above and below a snow cover but also predictions of future | ||
83 | snow and ice in mountains and high latitudes. A newer work area is the | 82 | snow and ice in mountains and high latitudes. A newer work area is the | ||
84 | risk management and optimization in the field of renewable energy | 83 | risk management and optimization in the field of renewable energy | ||
85 | production based on our detailed understanding of water, wind and | 84 | production based on our detailed understanding of water, wind and | ||
86 | radiation processes in mountains.\r\n\r\nMore information: | 85 | radiation processes in mountains.\r\n\r\nMore information: | ||
87 | http://cryos.epfl.ch/", | 86 | http://cryos.epfl.ch/", | ||
88 | "id": "b2ef52fe-c56a-4973-8309-24837f3848ed", | 87 | "id": "b2ef52fe-c56a-4973-8309-24837f3848ed", | ||
89 | "image_url": "2019-03-26-151807.125593CRYOSLogoFinal.jpg", | 88 | "image_url": "2019-03-26-151807.125593CRYOSLogoFinal.jpg", | ||
90 | "is_organization": true, | 89 | "is_organization": true, | ||
91 | "name": "cryos", | 90 | "name": "cryos", | ||
92 | "state": "active", | 91 | "state": "active", | ||
93 | "title": "CRYOS", | 92 | "title": "CRYOS", | ||
94 | "type": "organization" | 93 | "type": "organization" | ||
95 | }, | 94 | }, | ||
96 | "owner_org": "b2ef52fe-c56a-4973-8309-24837f3848ed", | 95 | "owner_org": "b2ef52fe-c56a-4973-8309-24837f3848ed", | ||
97 | "private": false, | 96 | "private": false, | ||
98 | "publication": "{\"publication_year\": \"2021\", \"publisher\": | 97 | "publication": "{\"publication_year\": \"2021\", \"publisher\": | ||
99 | \"EnviDat\"}", | 98 | \"EnviDat\"}", | ||
100 | "publication_state": "published", | 99 | "publication_state": "published", | ||
101 | "related_datasets": "* Atmospheric Radiation Measurement (ARM) user | 100 | "related_datasets": "* Atmospheric Radiation Measurement (ARM) user | ||
102 | facility. 2019. Ka ARM Zenith Radar (KAZRCFRGE). 2019-11-06 to | 101 | facility. 2019. Ka ARM Zenith Radar (KAZRCFRGE). 2019-11-06 to | ||
103 | 2019-11-13, ARM Mobile Facility (MOS) MOSAIC (Drifting Obs - Study of | 102 | 2019-11-13, ARM Mobile Facility (MOS) MOSAIC (Drifting Obs - Study of | ||
104 | Arctic Climate); AMF2 (M1). Compiled by I. Lindenmaier, K. Johnson, D. | 103 | Arctic Climate); AMF2 (M1). Compiled by I. Lindenmaier, K. Johnson, D. | ||
105 | Nelson, B. Isom, J. Hardin, A. Matthews, T. Wendler and V. Castro. ARM | 104 | Nelson, B. Isom, J. Hardin, A. Matthews, T. Wendler and V. Castro. ARM | ||
106 | Data Center. doi:10.5439/1498936.\n\n* David Clemens-Sewall. 2021. | 105 | Data Center. doi:10.5439/1498936.\n\n* David Clemens-Sewall. 2021. | ||
107 | Terrestrial Laser Scans of the Snow 2 area of the Multidisciplinary | 106 | Terrestrial Laser Scans of the Snow 2 area of the Multidisciplinary | ||
108 | drifting Observatory for the Study of Arctic Climate from November 6 | 107 | drifting Observatory for the Study of Arctic Climate from November 6 | ||
109 | and 13 2019. urn:node:ARCTIC. doi:10.18739/A2DZ03304.\n\n* Shupe et | 108 | and 13 2019. urn:node:ARCTIC. doi:10.18739/A2DZ03304.\n\n* Shupe et | ||
110 | al. 2021. MOSAiC atmospheric data from MET tower. [Note: a more | 109 | al. 2021. MOSAiC atmospheric data from MET tower. [Note: a more | ||
111 | complete reference (DOI) will be added after publication of the | 110 | complete reference (DOI) will be added after publication of the | ||
112 | dataset.]\n\n\n\n\n\n\n", | 111 | dataset.]\n\n\n\n\n\n\n", | ||
113 | "related_publications": "* Comola, F., and Lehning, M. (2017), | 112 | "related_publications": "* Comola, F., and Lehning, M. (2017), | ||
114 | Energy- and momentum-conserving model of splash entrainment in sand | 113 | Energy- and momentum-conserving model of splash entrainment in sand | ||
115 | and snow saltation, Geophys. Res. Lett., 44, 1601\u2013 1609, | 114 | and snow saltation, Geophys. Res. Lett., 44, 1601\u2013 1609, | ||
116 | doi:10.1002/2016GL071822.\n\n* Hames, O., Jafari, M., Wagner, D. N., | 115 | doi:10.1002/2016GL071822.\n\n* Hames, O., Jafari, M., Wagner, D. N., | ||
117 | Raphael, I., Clemens-Sewall, D., Polashenski, C., Shupe, M. D., | 116 | Raphael, I., Clemens-Sewall, D., Polashenski, C., Shupe, M. D., | ||
118 | Schneebeli, M., and Lehning, M. (2022). Modeling the small-scale | 117 | Schneebeli, M., and Lehning, M. (2022). Modeling the small-scale | ||
119 | deposition of snow onto structured Arctic sea ice during a MOSAiC | 118 | deposition of snow onto structured Arctic sea ice during a MOSAiC | ||
120 | storm using snowBedFoam 1.0. Geoscientific Model Development, | 119 | storm using snowBedFoam 1.0. Geoscientific Model Development, | ||
121 | 15(16):6429\u20136449.\n\n* Melo, D. B., Sharma, V., Comola, F., | 120 | 15(16):6429\u20136449.\n\n* Melo, D. B., Sharma, V., Comola, F., | ||
122 | Sigmund, A., & Lehning, M. (2022). Modeling snow saltation: The effect | 121 | Sigmund, A., & Lehning, M. (2022). Modeling snow saltation: The effect | ||
123 | of grain size and interparticle cohesion. Journal of Geophysical | 122 | of grain size and interparticle cohesion. Journal of Geophysical | ||
124 | Research: Atmospheres, 127, e2021JD035260. | 123 | Research: Atmospheres, 127, e2021JD035260. | ||
125 | https://doi.org/10.1029/2021JD035260 \n\n* Sharma, V., Comola, F., and | 124 | https://doi.org/10.1029/2021JD035260 \n\n* Sharma, V., Comola, F., and | ||
126 | Lehning, M.: On the suitability of the Thorpe\u2013Mason model for | 125 | Lehning, M.: On the suitability of the Thorpe\u2013Mason model for | ||
127 | calculating sublimation of saltating snow, The Cryosphere, 12, | 126 | calculating sublimation of saltating snow, The Cryosphere, 12, | ||
128 | 3499\u20133509, https://doi.org/10.5194/tc-12-3499-2018, | 127 | 3499\u20133509, https://doi.org/10.5194/tc-12-3499-2018, | ||
129 | 2018.\n\n\n\n", | 128 | 2018.\n\n\n\n", | ||
130 | "relationships_as_object": [], | 129 | "relationships_as_object": [], | ||
131 | "relationships_as_subject": [], | 130 | "relationships_as_subject": [], | ||
132 | "resource_type": "software", | 131 | "resource_type": "software", | ||
133 | "resource_type_general": "software", | 132 | "resource_type_general": "software", | ||
134 | "resources": [ | 133 | "resources": [ | ||
135 | { | 134 | { | ||
136 | "cache_last_updated": null, | 135 | "cache_last_updated": null, | ||
137 | "cache_url": null, | 136 | "cache_url": null, | ||
138 | "created": "2021-05-20T11:33:52.788535", | 137 | "created": "2021-05-20T11:33:52.788535", | ||
139 | "description": "This is the initial draft of the paper where the | 138 | "description": "This is the initial draft of the paper where the | ||
140 | snowBedFoam 1.0. results are tested against Terrestrial Laser Scan | 139 | snowBedFoam 1.0. results are tested against Terrestrial Laser Scan | ||
141 | (TLS) measurements of snow dynamics on Arctic sea ice (MOSAiC | 140 | (TLS) measurements of snow dynamics on Arctic sea ice (MOSAiC | ||
142 | expedition). It highlights the numerical limitations of our model as | 141 | expedition). It highlights the numerical limitations of our model as | ||
143 | well as the measurement uncertainties, which may occur in such extreme | 142 | well as the measurement uncertainties, which may occur in such extreme | ||
144 | environments.", | 143 | environments.", | ||
145 | "doi": "", | 144 | "doi": "", | ||
146 | "format": "PDF", | 145 | "format": "PDF", | ||
147 | "hash": "", | 146 | "hash": "", | ||
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149 | "last_modified": null, | 148 | "last_modified": null, | ||
150 | "metadata_modified": "2021-07-23T06:08:29.844192", | 149 | "metadata_modified": "2021-07-23T06:08:29.844192", | ||
151 | "mimetype": null, | 150 | "mimetype": null, | ||
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153 | "name": "Paper Draft", | 152 | "name": "Paper Draft", | ||
154 | "package_id": "8bdc13ec-e59e-4f08-aa0d-646745fb76a6", | 153 | "package_id": "8bdc13ec-e59e-4f08-aa0d-646745fb76a6", | ||
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158 | \"mb\"}", | 157 | \"mb\"}", | ||
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160 | "restricted": "{\"level\": \"public\", \"allowed_users\": \"\", | 159 | "restricted": "{\"level\": \"public\", \"allowed_users\": \"\", | ||
161 | \"shared_secret\": \"\"}", | 160 | \"shared_secret\": \"\"}", | ||
162 | "size": 3025070, | 161 | "size": 3025070, | ||
163 | "state": "active", | 162 | "state": "active", | ||
164 | "url": | 163 | "url": | ||
165 | 6e-afa2-4a08-bb12-351648d1e1f9/download/snowbedfoam_mosaicseaice.pdf", | 164 | 6e-afa2-4a08-bb12-351648d1e1f9/download/snowbedfoam_mosaicseaice.pdf", | ||
166 | "url_type": "upload" | 165 | "url_type": "upload" | ||
167 | }, | 166 | }, | ||
168 | { | 167 | { | ||
169 | "cache_last_updated": null, | 168 | "cache_last_updated": null, | ||
170 | "cache_url": null, | 169 | "cache_url": null, | ||
171 | "created": "2021-06-11T11:09:58.514378", | 170 | "created": "2021-06-11T11:09:58.514378", | ||
172 | "description": "OpenFOAM-2.3.0. scripts containing the | 171 | "description": "OpenFOAM-2.3.0. scripts containing the | ||
173 | implemented Eulerian-Lagrangian snow transport model.\r\n\r\nThe code | 172 | implemented Eulerian-Lagrangian snow transport model.\r\n\r\nThe code | ||
174 | file provided here is not updated. The most recent version of the | 173 | file provided here is not updated. The most recent version of the | ||
175 | script can be found on the WSL/SLF GitLab repository: | 174 | script can be found on the WSL/SLF GitLab repository: | ||
176 | https://gitlabext.wsl.ch/atmospheric-models/snowbedfoam-v1-0.git", | 175 | https://gitlabext.wsl.ch/atmospheric-models/snowbedfoam-v1-0.git", | ||
177 | "doi": "None", | 176 | "doi": "None", | ||
178 | "format": ".zip", | 177 | "format": ".zip", | ||
179 | "hash": "", | 178 | "hash": "", | ||
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197 | "url_type": "upload" | 196 | "url_type": "upload" | ||
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199 | { | 198 | { | ||
200 | "cache_last_updated": null, | 199 | "cache_last_updated": null, | ||
201 | "cache_url": null, | 200 | "cache_url": null, | ||
202 | "created": "2021-07-02T11:49:43.470036", | 201 | "created": "2021-07-02T11:49:43.470036", | ||
203 | "description": "Extract from the preliminary MOSAiC atmospheric | 202 | "description": "Extract from the preliminary MOSAiC atmospheric | ||
204 | data (Level 2) for the time period 6th to 13th of November, 2019. | 203 | data (Level 2) for the time period 6th to 13th of November, 2019. | ||
205 | \r\nThis data was used to set up the fluid forcing parameters in the | 204 | \r\nThis data was used to set up the fluid forcing parameters in the | ||
206 | snowBedFoam simulations on MOSAiC sea ice. It is being published in | 205 | snowBedFoam simulations on MOSAiC sea ice. It is being published in | ||
207 | this repository with the kind permission from Matthew Shupe and his | 206 | this repository with the kind permission from Matthew Shupe and his | ||
208 | team. \r\nThe final processed and quality controlled version of this | 207 | team. \r\nThe final processed and quality controlled version of this | ||
209 | dataset (Level 3) has not been published yet. A complete reference | 208 | dataset (Level 3) has not been published yet. A complete reference | ||
210 | will be added in this description once it is released.", | 209 | will be added in this description once it is released.", | ||
211 | "doi": "None", | 210 | "doi": "None", | ||
212 | "format": "zip-compressed folder of csv", | 211 | "format": "zip-compressed folder of csv", | ||
213 | "hash": "", | 212 | "hash": "", | ||
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219 | "name": "MOSAiC Met City preliminary (Level 2) wind data ", | 218 | "name": "MOSAiC Met City preliminary (Level 2) wind data ", | ||
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227 | "size": 37737, | 226 | "size": 37737, | ||
228 | "state": "active", | 227 | "state": "active", | ||
229 | "url": | 228 | "url": | ||
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231 | "url_type": "upload" | 230 | "url_type": "upload" | ||
232 | }, | 231 | }, | ||
233 | { | 232 | { | ||
234 | "cache_last_updated": null, | 233 | "cache_last_updated": null, | ||
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236 | "created": "2024-03-25T11:32:23.549021", | 235 | "created": "2024-03-25T11:32:23.549021", | ||
237 | "description": "OpenFOAM-5.0 scripts containing the implemented | 236 | "description": "OpenFOAM-5.0 scripts containing the implemented | ||
238 | Eulerian-Lagrangian snow transport model.\n\nThe code file provided | 237 | Eulerian-Lagrangian snow transport model.\n\nThe code file provided | ||
239 | here is not updated. The most recent version of the script can be | 238 | here is not updated. The most recent version of the script can be | ||
240 | found on the WSL/SLF GitLab repository: | 239 | found on the WSL/SLF GitLab repository: | ||
241 | https://gitlabext.wsl.ch/atmospheric-models/snowbedfoam-v1-0.git", | 240 | https://gitlabext.wsl.ch/atmospheric-models/snowbedfoam-v1-0.git", | ||
242 | "doi": "", | 241 | "doi": "", | ||
243 | "format": "ZIP", | 242 | "format": "ZIP", | ||
244 | "hash": "", | 243 | "hash": "", | ||
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266 | "created": "2024-03-25T11:42:20.757421", | 265 | "created": "2024-03-25T11:42:20.757421", | ||
267 | "description": "Files containing the topographical data | 266 | "description": "Files containing the topographical data | ||
268 | barometrically measured in June 2009 around the German Antarctic | 267 | barometrically measured in June 2009 around the German Antarctic | ||
269 | Research station Neumayer III. Those measurements are compared to the | 268 | Research station Neumayer III. Those measurements are compared to the | ||
270 | snowBedFoam simulations to assess the ability of the model to | 269 | snowBedFoam simulations to assess the ability of the model to | ||
271 | reproduce real snow distribution observations.", | 270 | reproduce real snow distribution observations.", | ||
272 | "doi": "", | 271 | "doi": "", | ||
273 | "format": "ZIP", | 272 | "format": "ZIP", | ||
274 | "hash": "", | 273 | "hash": "", | ||
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278 | "mimetype": "application/zip", | 277 | "mimetype": "application/zip", | ||
279 | "mimetype_inner": null, | 278 | "mimetype_inner": null, | ||
280 | "name": "Snowdrift measurements around Neumayer Station III", | 279 | "name": "Snowdrift measurements around Neumayer Station III", | ||
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289 | "url": | 288 | "url": | ||
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291 | "url_type": "upload" | 290 | "url_type": "upload" | ||
292 | }, | 291 | }, | ||
293 | { | 292 | { | ||
294 | "cache_last_updated": null, | 293 | "cache_last_updated": null, | ||
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296 | "created": "2024-03-25T11:51:47.809789", | 295 | "created": "2024-03-25T11:51:47.809789", | ||
297 | "description": "Snow distribution results around Neumayer | 296 | "description": "Snow distribution results around Neumayer | ||
298 | Station III obtained for the sensitivity analysis and comparison to | 297 | Station III obtained for the sensitivity analysis and comparison to | ||
299 | measurements. The file contains several sub-folders, namely:\n-COMP: | 298 | measurements. The file contains several sub-folders, namely:\n-COMP: | ||
300 | simulation output for the comparison to measurements;\n-FLOW: | 299 | simulation output for the comparison to measurements;\n-FLOW: | ||
301 | simulation output for the study of wind forcing | 300 | simulation output for the study of wind forcing | ||
302 | impact;\n-simulation_exampleCase: example case of a snowBedFoam | 301 | impact;\n-simulation_exampleCase: example case of a snowBedFoam | ||
303 | simulation with the reference Neumayer Station mesh;\n-SNOW: | 302 | simulation with the reference Neumayer Station mesh;\n-SNOW: | ||
304 | simulation output for the study of snow properties impact;\n-STRUCT: | 303 | simulation output for the study of snow properties impact;\n-STRUCT: | ||
305 | simulation output for the study of structure properties impact.\n\n", | 304 | simulation output for the study of structure properties impact.\n\n", | ||
306 | "doi": "", | 305 | "doi": "", | ||
307 | "format": "ZIP", | 306 | "format": "ZIP", | ||
308 | "hash": "", | 307 | "hash": "", | ||
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312 | "mimetype": "application/zip", | 311 | "mimetype": "application/zip", | ||
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314 | "name": "Neumayer III simulations", | 313 | "name": "Neumayer III simulations", | ||
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321 | "size": 296665509, | 320 | "size": 296665509, | ||
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325 | "url_type": "upload" | 324 | "url_type": "upload" | ||
326 | } | 325 | } | ||
327 | ], | 326 | ], | ||
328 | "spatial": | 327 | "spatial": | ||
329 | 3705433648492],[90,84.24187622276202],[53.4375,84.24187622276202]]]}", | 328 | 3705433648492],[90,84.24187622276202],[53.4375,84.24187622276202]]]}", | ||
330 | "spatial_info": "Switzerland", | 329 | "spatial_info": "Switzerland", | ||
331 | "state": "active", | 330 | "state": "active", | ||
332 | "subtitle": "", | 331 | "subtitle": "", | ||
333 | "tags": [ | 332 | "tags": [ | ||
334 | { | 333 | { | ||
335 | "display_name": "ANTARCTICA", | 334 | "display_name": "ANTARCTICA", | ||
336 | "id": "7e2647cf-cb96-44bb-800e-e4468384ebe7", | 335 | "id": "7e2647cf-cb96-44bb-800e-e4468384ebe7", | ||
337 | "name": "ANTARCTICA", | 336 | "name": "ANTARCTICA", | ||
338 | "state": "active", | 337 | "state": "active", | ||
339 | "vocabulary_id": null | 338 | "vocabulary_id": null | ||
340 | }, | 339 | }, | ||
341 | { | 340 | { | ||
342 | "display_name": "ARCTIC SEA ICE", | 341 | "display_name": "ARCTIC SEA ICE", | ||
343 | "id": "f98cc601-3e57-4af1-a8b5-3e1770bd0420", | 342 | "id": "f98cc601-3e57-4af1-a8b5-3e1770bd0420", | ||
344 | "name": "ARCTIC SEA ICE", | 343 | "name": "ARCTIC SEA ICE", | ||
345 | "state": "active", | 344 | "state": "active", | ||
346 | "vocabulary_id": null | 345 | "vocabulary_id": null | ||
347 | }, | 346 | }, | ||
348 | { | 347 | { | ||
349 | "display_name": "MOSAIC", | 348 | "display_name": "MOSAIC", | ||
350 | "id": "e97c8f27-76a3-4c98-9627-b3731f6720e4", | 349 | "id": "e97c8f27-76a3-4c98-9627-b3731f6720e4", | ||
351 | "name": "MOSAIC", | 350 | "name": "MOSAIC", | ||
352 | "state": "active", | 351 | "state": "active", | ||
353 | "vocabulary_id": null | 352 | "vocabulary_id": null | ||
354 | }, | 353 | }, | ||
355 | { | 354 | { | ||
356 | "display_name": "OPENFOAM", | 355 | "display_name": "OPENFOAM", | ||
357 | "id": "e1854139-4856-4dc6-9546-19f39fa235a7", | 356 | "id": "e1854139-4856-4dc6-9546-19f39fa235a7", | ||
358 | "name": "OPENFOAM", | 357 | "name": "OPENFOAM", | ||
359 | "state": "active", | 358 | "state": "active", | ||
360 | "vocabulary_id": null | 359 | "vocabulary_id": null | ||
361 | }, | 360 | }, | ||
362 | { | 361 | { | ||
363 | "display_name": "SNOW DEPOSITION", | 362 | "display_name": "SNOW DEPOSITION", | ||
364 | "id": "ff281882-e1c0-4119-9c10-5929c5222ef9", | 363 | "id": "ff281882-e1c0-4119-9c10-5929c5222ef9", | ||
365 | "name": "SNOW DEPOSITION", | 364 | "name": "SNOW DEPOSITION", | ||
366 | "state": "active", | 365 | "state": "active", | ||
367 | "vocabulary_id": null | 366 | "vocabulary_id": null | ||
368 | }, | 367 | }, | ||
369 | { | 368 | { | ||
370 | "display_name": "SNOW TRANSPORT", | 369 | "display_name": "SNOW TRANSPORT", | ||
371 | "id": "506cb5dc-8200-41ac-b0a4-fdd2db5cd539", | 370 | "id": "506cb5dc-8200-41ac-b0a4-fdd2db5cd539", | ||
372 | "name": "SNOW TRANSPORT", | 371 | "name": "SNOW TRANSPORT", | ||
373 | "state": "active", | 372 | "state": "active", | ||
374 | "vocabulary_id": null | 373 | "vocabulary_id": null | ||
375 | } | 374 | } | ||
376 | ], | 375 | ], | ||
377 | "title": "snowBedFoam: an OpenFOAM Eulerian-Lagrangian solver for | 376 | "title": "snowBedFoam: an OpenFOAM Eulerian-Lagrangian solver for | ||
378 | modelling snow transport", | 377 | modelling snow transport", | ||
379 | "type": "dataset", | 378 | "type": "dataset", | ||
380 | "url": null, | 379 | "url": null, | ||
381 | "version": "1.0" | 380 | "version": "1.0" | ||
382 | } | 381 | } |