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  "author": "[{\"affiliation\": \"SLF\", \"affiliation_02\": \"EPFL\", 
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  "author": "[{\"affiliation\": \"SLF\", \"affiliation_02\": \"EPFL\", 
            
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\"affiliation_03\": \"\", \"data_credit\": [\"collection\", 
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\"affiliation_03\": \"\", \"data_credit\": [\"collection\", 
            
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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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  "creator_user_id": "ebd22060-c56d-419b-a56e-9e171f19e7e5",
            
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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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\"institution_url\": \"https://p3.snf.ch/project-188554\"}]",
            
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  "groups": [],
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  "groups": [],
            
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  "language": "en",
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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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  "maintainer_email": null,
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  "maintainer_email": null,
            
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  "metadata_created": "2022-02-24T16:15:53.573278",
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  "metadata_created": "2022-02-24T16:15:53.573278",
            
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  "metadata_modified": "2022-05-16T11:45:05.118395",
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  "metadata_modified": "2022-10-04T07:05:00.002285",
            
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  "name": "weird",
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  "name": "weird",
            
n
38
  "notes": "We present a novel method for quantifying surface heat 
n
38
  "notes": "The lateral transport of heat above abrupt 
            
39
exchange over heterogeneous land surfaces at ultra-high 
39
(sub-)metre-scale steps in land surface temperature influences the 
            
40
spatio-temporal resolution.  Therefore, a thermal infrared camera 
40
local surface energy balance. We present a novel experimental method 
            
41
records 30Hz sequences of infrared frames of upright screens, that are 
41
to investigate the stratification and dynamics of the near-surface 
            
42
deployed across the transition from bare ground to snow. The screen's 
42
atmospheric layer over a heterogeneous land surface. Using a high 
            
43
resolution thermal infrared camera pointing at synthetic screens, a 
            
44
30Hz sequence of frames is recorded. The screens are deployed upright 
            
45
and horizontally aligned with the prevailing wind direction. The 
            
43
surface temperature serves as a proxy for the local air temperature. 
46
screen\u2019s surface temperature serves as a proxy for the local air 
            
44
In addition to information on the stratification of the near-surface 
47
temperature. We developed a method to estimate near-surface 
            
45
atmospheric layer, estimations of the 2D wind field can be obtained 
48
two-dimensional wind fields at centimetre resolution from tracking the 
            
46
evaluating the temperature dynamics.\r\nHere you find the data and the 
49
air temperature pattern on the screens. Wind field estimations are 
            
50
validated with near-surface three-dimensional short-path ultrasonic 
            
51
data. To demonstrate the capabilities of the screen method, we present 
            
52
results from a comprehensive field campaign at an alpine research site 
            
53
during patchy snow cover conditions. The measurements reveal an 
            
54
extremely heterogeneous near-surface atmospheric layer. Vertical 
            
55
profiles of horizontal and vertical wind speed reflect multiple layers 
            
56
of different static stability within 2m above the surface. A dynamic, 
            
57
thin stable internal boundary layer (SIBL) develops above the leading 
            
58
edge of snow patches protecting the snow surface from warmer air 
            
59
above. During pronounced gusts the warm air from aloft entrains into 
            
60
the SIBL and reaches down to the snow surface adding energy to the 
            
61
snow pack. Measured vertical turbulent sensible heat fluxes are shown 
            
62
to be consistent with air temperature and wind speed profiles obtained 
            
63
using the screen method and confirm its capabilities to investigate 
            
64
complex in situ near-surface heat exchange processes.\r\nHere you find 
            
47
documented code used to create the plots in the publication.",
65
the data and the documented code used to create the plots in the 
            
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publication.",
            
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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 
72
    "description": "The research group \u00abSnow Hydrology\u00bb 
            
54
investigates snow as a component of the hydrological cycle. In the 
73
investigates snow as a component of the hydrological cycle. In the 
            
55
Alps a significant percentage of precipitation comes in the form of 
74
Alps a significant percentage of precipitation comes in the form of 
            
56
snow. The timing of snow melt thus influences the annual dynamics of 
75
snow. The timing of snow melt thus influences the annual dynamics of 
            
57
runoff from alpine watersheds. Of particular interest for our research 
76
runoff from alpine watersheds. Of particular interest for our research 
            
58
is to enhance estimations of snow water resources and subsequent melt 
77
is to enhance estimations of snow water resources and subsequent melt 
            
59
water discharge.\r\n\r\nThe research group covers a broad range of 
78
water discharge.\r\n\r\nThe research group covers a broad range of 
            
60
projects and methods. The latest measuring techniques are used to 
79
projects and methods. The latest measuring techniques are used to 
            
61
investigate snow distribution patterns in alpine terrain, e.g. laser 
80
investigate snow distribution patterns in alpine terrain, e.g. laser 
            
62
scanning or radar technology. We use different types of numerical 
81
scanning or radar technology. We use different types of numerical 
            
63
models to calculate snow water resources based on input data from 
82
models to calculate snow water resources based on input data from 
            
64
meteorological monitoring networks. These models are being used to 
83
meteorological monitoring networks. These models are being used to 
            
65
predict the consequences of climate change on the water balance of 
84
predict the consequences of climate change on the water balance of 
            
66
mountain watersheds. The models also constitute a valuable tool for 
85
mountain watersheds. The models also constitute a valuable tool for 
            
67
our operational services, such as periodic snow hydrological 
86
our operational services, such as periodic snow hydrological 
            
68
bulletins, which contribute to the federal flood prevention and 
87
bulletins, which contribute to the federal flood prevention and 
            
69
forecasting system.\r\n\r\nThe research group \u00abSnow 
88
forecasting system.\r\n\r\nThe research group \u00abSnow 
            
70
Hydrology\u00bb is based in Davos and ensures the link between other 
89
Hydrology\u00bb is based in Davos and ensures the link between other 
            
71
Davosian research groups and the research unit \u201dMountain 
90
Davosian research groups and the research unit \u201dMountain 
            
72
Hydrology and Mass Movements\u201d in Birmensdorf.",
91
Hydrology and Mass Movements\u201d in Birmensdorf.",
            
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    "id": "d66115d3-c4f9-4f6e-8ff1-5791549e0386",
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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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  "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": "A Novel Method to Quantify Near-Surface 
106
  "related_publications": "A Novel Method to Quantify Near-Surface 
            
88
Boundary-Layer Dynamics at Ultra-High Spatio-Temporal Resolution; 
107
Boundary-Layer Dynamics at Ultra-High Spatio-Temporal Resolution; 
            
t
89
submitted and under review",
t
108
accepted for publication in Boundary-Layer Meteorology",
            
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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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      "created": "2022-02-24T16:22:51.056409",
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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 
119
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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      "description": "folder containing the source code for the WEIRD 
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      "description": "folder containing the source code for the WEIRD 
            
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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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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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      "display_name": "NEAR-SURFACE ATMOSPHERIC LAYER",
            
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      "id": "93a597d5-cb9f-43d2-b7ca-dd50a368608b",
            
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      "name": "NEAR-SURFACE ATMOSPHERIC LAYER",
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      "name": "NEAR-SURFACE ATMOSPHERIC LAYER",
            
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      "state": "active",
            
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      "display_name": "PATCHY SNOW COVER",
            
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      "name": "PATCHY SNOW COVER",
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      "name": "PATCHY SNOW COVER",
            
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242
      "state": "active",
            
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      "vocabulary_id": null
            
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    },
            
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    {
            
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      "display_name": "SNOW MELT",
246
      "display_name": "SNOW MELT",
            
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      "id": "4452e5c9-c707-4c61-bd1c-28816181a043",
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      "id": "4452e5c9-c707-4c61-bd1c-28816181a043",
            
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      "name": "SNOW MELT",
248
      "name": "SNOW MELT",
            
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      "state": "active",
249
      "state": "active",
            
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      "vocabulary_id": null
250
      "vocabulary_id": null
            
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    },
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    },
            
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    {
252
    {
            
234
      "display_name": "SNOW-ATMOSPHERE INTERACTIONS",
253
      "display_name": "SNOW-ATMOSPHERE INTERACTIONS",
            
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      "id": "9d4df93a-3291-49a2-8c72-565088f48c09",
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      "id": "9d4df93a-3291-49a2-8c72-565088f48c09",
            
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      "name": "SNOW-ATMOSPHERE INTERACTIONS",
255
      "name": "SNOW-ATMOSPHERE INTERACTIONS",
            
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      "state": "active",
256
      "state": "active",
            
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      "vocabulary_id": null
257
      "vocabulary_id": null
            
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    },
258
    },
            
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    {
259
    {
            
241
      "display_name": "SURFACE HEAT EXCHANGE",
260
      "display_name": "SURFACE HEAT EXCHANGE",
            
242
      "id": "cb61d6bd-bf4d-4fd6-a8e2-8dbbbd90d418",
261
      "id": "cb61d6bd-bf4d-4fd6-a8e2-8dbbbd90d418",
            
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      "name": "SURFACE HEAT EXCHANGE",
262
      "name": "SURFACE HEAT EXCHANGE",
            
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      "state": "active",
263
      "state": "active",
            
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      "vocabulary_id": null
264
      "vocabulary_id": null
            
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    }
265
    }
            
247
  ],
266
  ],
            
248
  "title": "Quantifying Surface Heat Exchange over Heterogeneous Land 
267
  "title": "Quantifying Surface Heat Exchange over Heterogeneous Land 
            
249
Surfaces at Ultra-High Spatio-Temporal Resolution",
268
Surfaces at Ultra-High Spatio-Temporal Resolution",
            
250
  "type": "dataset",
269
  "type": "dataset",
            
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  "url": null,
270
  "url": null,
            
252
  "version": "1.0"
271
  "version": "1.0"
            
253
}
272
}