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\"software\", \"publication\"], \"email\": 
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\"software\", \"publication\"], \"email\": 
            
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\"michael.haugeneder@slf.ch\", \"given_name\": \"Michael\", 
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\"michael.haugeneder@slf.ch\", \"given_name\": \"Michael\", 
            
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\"identifier\": \"0000-0003-3228-9868\", \"name\": \"Haugeneder\"}, 
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\"identifier\": \"0000-0003-3228-9868\", \"name\": \"Haugeneder\"}, 
            
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{\"affiliation\": \"SLF\", \"affiliation_02\": \"EPFL\", 
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{\"affiliation\": \"SLF\", \"affiliation_02\": \"EPFL\", 
            
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\"affiliation_03\": \"\", \"email\": \"lehning@slf.ch\", 
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\"affiliation_03\": \"\", \"email\": \"lehning@slf.ch\", 
            
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\"given_name\": \"Michael\", \"identifier\": \"\", \"name\": 
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\"given_name\": \"Michael\", \"identifier\": \"\", \"name\": 
            
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\"Lehning\"}, {\"affiliation\": \"SLF\", \"affiliation_02\": \"\", 
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\"Lehning\"}, {\"affiliation\": \"SLF\", \"affiliation_02\": \"\", 
            
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\"affiliation_03\": \"\", \"email\": \"jonas@slf.ch\", \"given_name\": 
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\"affiliation_03\": \"\", \"email\": \"jonas@slf.ch\", \"given_name\": 
            
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\"Tobias\", \"identifier\": \"\", \"name\": \"Jonas\"}, 
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\"Tobias\", \"identifier\": \"\", \"name\": \"Jonas\"}, 
            
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{\"affiliation\": \"SLF\", \"affiliation_02\": \"\", 
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{\"affiliation\": \"SLF\", \"affiliation_02\": \"\", 
            
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\"affiliation_03\": \"\", \"email\": \"mott@slf.ch\", \"given_name\": 
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\"affiliation_03\": \"\", \"email\": \"mott@slf.ch\", \"given_name\": 
            
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\"Rebecca\", \"identifier\": \"\", \"name\": \"Mott\"}]",
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\"Rebecca\", \"identifier\": \"\", \"name\": \"Mott\"}]",
            
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  "author_email": null,
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  "date": "[{\"date\": \"2021-04-28\", \"date_type\": \"collected\", 
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  "date": "[{\"date\": \"2021-04-28\", \"date_type\": \"collected\", 
            
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\"end_date\": \"\"}]",
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\"end_date\": \"\"}]",
            
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  "doi": "10.16904/envidat.299",
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  "doi": "10.16904/envidat.299",
            
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  "funding": "[{\"grant_number\": \"\", \"institution\": \"SNF\", 
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  "funding": "[{\"grant_number\": \"\", \"institution\": \"SNF\", 
            
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\"institution_url\": \"https://p3.snf.ch/project-188554\"}]",
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  "language": "en",
            
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  "license_id": "wsl-data",
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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\": \"SLF\", \"email\": 
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  "maintainer": "{\"affiliation\": \"SLF\", \"email\": 
            
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\"michael.haugeneder@slf.ch\", \"given_name\": \"Michael\", 
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\"michael.haugeneder@slf.ch\", \"given_name\": \"Michael\", 
            
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\"identifier\": \"0000-0003-3228-9868\", \"name\": \"Haugeneder\"}",
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\"identifier\": \"0000-0003-3228-9868\", \"name\": \"Haugeneder\"}",
            
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  "metadata_created": "2022-02-24T16:15:53.573278",
            
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  "metadata_modified": "2022-02-25T10:57:10.149867",
            
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  "name": "weird",
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  "name": "weird",
            
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  "notes": "We present a novel method for quantifying surface heat 
38
  "notes": "We present a novel method for quantifying surface heat 
            
39
exchange over heterogeneous land surfaces at ultra-high 
39
exchange over heterogeneous land surfaces at ultra-high 
            
40
spatio-temporal resolution.  Therefore, a thermal infrared camera 
40
spatio-temporal resolution.  Therefore, a thermal infrared camera 
            
41
records 30Hz sequences of infrared frames of upright screens, that are 
41
records 30Hz sequences of infrared frames of upright screens, that are 
            
42
deployed across the transition from bare ground to snow. The screen's 
42
deployed across the transition from bare ground to snow. The screen's 
            
43
surface temperature serves as a proxy for the local air temperature. 
43
surface temperature serves as a proxy for the local air temperature. 
            
44
In addition to information on the stratification of the near-surface 
44
In addition to information on the stratification of the near-surface 
            
45
atmospheric layer, estimations of the 2D wind field can be obtained 
45
atmospheric layer, estimations of the 2D wind field can be obtained 
            
46
evaluating the temperature dynamics.\r\nHere you find the data and the 
46
evaluating the temperature dynamics.\r\nHere you find the data and the 
            
47
code used to create the plots in the publication. After finishing the 
47
code used to create the plots in the publication. After finishing the 
            
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review process, the dataset might change.",
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review process, the dataset might change.",
            
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  "num_resources": 3,
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  "num_resources": 3,
            
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  "num_tags": 8,
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  "num_tags": 8,
            
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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": "2021-08-23T15:25:48.676190",
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    "created": "2021-08-23T15:25:48.676190",
            
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    "description": "The research group \u00abSnow Hydrology\u00bb 
54
    "description": "The research group \u00abSnow Hydrology\u00bb 
            
55
investigates snow as a component of the hydrological cycle. In the 
55
investigates snow as a component of the hydrological cycle. In the 
            
56
Alps a significant percentage of precipitation comes in the form of 
56
Alps a significant percentage of precipitation comes in the form of 
            
57
snow. The timing of snow melt thus influences the annual dynamics of 
57
snow. The timing of snow melt thus influences the annual dynamics of 
            
58
runoff from alpine watersheds. Of particular interest for our research 
58
runoff from alpine watersheds. Of particular interest for our research 
            
59
is to enhance estimations of snow water resources and subsequent melt 
59
is to enhance estimations of snow water resources and subsequent melt 
            
60
water discharge.\r\n\r\nThe research group covers a broad range of 
60
water discharge.\r\n\r\nThe research group covers a broad range of 
            
61
projects and methods. The latest measuring techniques are used to 
61
projects and methods. The latest measuring techniques are used to 
            
62
investigate snow distribution patterns in alpine terrain, e.g. laser 
62
investigate snow distribution patterns in alpine terrain, e.g. laser 
            
63
scanning or radar technology. We use different types of numerical 
63
scanning or radar technology. We use different types of numerical 
            
64
models to calculate snow water resources based on input data from 
64
models to calculate snow water resources based on input data from 
            
65
meteorological monitoring networks. These models are being used to 
65
meteorological monitoring networks. These models are being used to 
            
66
predict the consequences of climate change on the water balance of 
66
predict the consequences of climate change on the water balance of 
            
67
mountain watersheds. The models also constitute a valuable tool for 
67
mountain watersheds. The models also constitute a valuable tool for 
            
68
our operational services, such as periodic snow hydrological 
68
our operational services, such as periodic snow hydrological 
            
69
bulletins, which contribute to the federal flood prevention and 
69
bulletins, which contribute to the federal flood prevention and 
            
70
forecasting system.\r\n\r\nThe research group \u00abSnow 
70
forecasting system.\r\n\r\nThe research group \u00abSnow 
            
71
Hydrology\u00bb is based in Davos and ensures the link between other 
71
Hydrology\u00bb is based in Davos and ensures the link between other 
            
72
Davosian research groups and the research unit \u201dMountain 
72
Davosian research groups and the research unit \u201dMountain 
            
73
Hydrology and Mass Movements\u201d in Birmensdorf.",
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Hydrology and Mass Movements\u201d in Birmensdorf.",
            
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    "id": "d66115d3-c4f9-4f6e-8ff1-5791549e0386",
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    "image_url": "",
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    "image_url": "",
            
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    "is_organization": true,
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    "is_organization": true,
            
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    "name": "snow-hydrology",
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    "name": "snow-hydrology",
            
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    "state": "active",
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    "state": "active",
            
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    "title": "Snow Hydrology",
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    "title": "Snow Hydrology",
            
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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": "d66115d3-c4f9-4f6e-8ff1-5791549e0386",
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  "private": false,
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  "private": false,
            
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  "publication": "{\"publication_year\": \"2022\", \"publisher\": 
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  "publication": "{\"publication_year\": \"2022\", \"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": "Quantifying Surface Heat Exchange over 
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  "related_publications": "Quantifying Surface Heat Exchange over 
            
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Heterogeneous Land Surfaces at Ultra-High Spatio-Temporal Resolution; 
89
Heterogeneous Land Surfaces at Ultra-High Spatio-Temporal Resolution; 
            
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submitted and under review",
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submitted and under review",
            
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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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      "description": "Data measured with a 3D short-path ultrasonic 
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      "description": "Data measured with a 3D short-path ultrasonic 
            
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anemometer in close vicinity to the screens. Note that the time stamps 
101
anemometer in close vicinity to the screens. Note that the time stamps 
            
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are in local time (GMT+2).",
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method. Written in JULIA.",
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method. Written in JULIA.",
            
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      "description": "Sequence of 2700 frames recorded with the 
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      "description": "Sequence of 2700 frames recorded with the 
            
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thermal IR cam. The data is stored as the variable 'irdata' in the .nc 
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thermal IR cam. The data is stored as the variable 'irdata' in the .nc 
            
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file.",
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      "name": "IRdata",
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      "display_name": "SNOW-ATMOSPHERE INTERACTIONS",
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      "name": "SNOW-ATMOSPHERE INTERACTIONS",
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      "name": "SNOW-ATMOSPHERE INTERACTIONS",
            
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      "state": "active",
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      "state": "active",
            
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      "vocabulary_id": null
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      "display_name": "SURFACE HEAT EXCHANGE",
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      "display_name": "SURFACE HEAT EXCHANGE",
            
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      "id": "cb61d6bd-bf4d-4fd6-a8e2-8dbbbd90d418",
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      "id": "cb61d6bd-bf4d-4fd6-a8e2-8dbbbd90d418",
            
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      "name": "SURFACE HEAT EXCHANGE",
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  ],
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  ],
            
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  "title": "Quantifying Surface Heat Exchange over Heterogeneous Land 
249
  "title": "Quantifying Surface Heat Exchange over Heterogeneous Land 
            
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Surfaces at Ultra-High Spatio-Temporal Resolution",
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Surfaces at Ultra-High Spatio-Temporal Resolution",
            
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  "version": "1.0"
            
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}
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}