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\"affiliation_03\": \"\", \"given_name\": \"Sebastian\", 
            
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\"identifier\": \"\", \"email\": \"sebastian.schloegl@slf.ch\", 
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\"identifier\": \"\", \"email\": \"sebastian.schloegl@slf.ch\", 
            
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\"affiliation_02\": \"\"}, {\"name\": \"Mott\", \"affiliation\": 
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\"affiliation_02\": \"\"}, {\"name\": \"Mott\", \"affiliation\": 
            
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\"SLF\", \"affiliation_03\": \"\", \"given_name\": \"Rebecca\", 
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\"SLF\", \"affiliation_03\": \"\", \"given_name\": \"Rebecca\", 
            
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\"identifier\": \"\", \"email\": \"mott@slf.ch\", \"affiliation_02\": 
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\"identifier\": \"\", \"email\": \"mott@slf.ch\", \"affiliation_02\": 
            
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\"\"}, {\"name\": \"Lehning\", \"affiliation\": \"SLF\", 
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\"\"}, {\"name\": \"Lehning\", \"affiliation\": \"SLF\", 
            
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\"affiliation_03\": \"\", \"given_name\": \"Michael\", \"identifier\": 
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\"affiliation_03\": \"\", \"given_name\": \"Michael\", \"identifier\": 
            
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\"\", \"email\": \"lehning@slf.ch\", \"affiliation_02\": \"\"}]",
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\"\", \"email\": \"lehning@slf.ch\", \"affiliation_02\": \"\"}]",
            
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  "author_email": null,
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  "author_email": null,
            
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  "creator_user_id": "094d57a1-87c6-477c-b586-649e78da5ee5",
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  "creator_user_id": "094d57a1-87c6-477c-b586-649e78da5ee5",
            
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  "date": "[{\"date\": \"2018-12-06\", \"date_type\": \"created\", 
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  "date": "[{\"date\": \"2018-12-06\", \"date_type\": \"created\", 
            
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\"end_date\": \"\"}]",
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\"end_date\": \"\"}]",
            
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  "doi": "10.16904/envidat.584",
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  "doi": "10.16904/envidat.584",
            
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  "extras": [
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  ],
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  ],
            
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  "funding": "[{\"grant_number\": \"\", \"institution\": \"Funding 
            
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information not available.\", \"institution_url\": \"\"}]",
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information not available.\", \"institution_url\": \"\"}]",
            
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\"given_name\": \"Sebastian\", \"name\": \"Schl\u00f6gl\", \"email\": 
            
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\"sebastian.schloegl@slf.ch\"}",
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\"sebastian.schloegl@slf.ch\"}",
            
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  "metadata_created": "2018-06-26T14:22:43.588250",
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  "metadata_created": "2018-06-26T14:22:43.588250",
            
n
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  "metadata_modified": "2025-02-05T12:49:20.094164",
n
36
  "metadata_modified": "2025-02-05T12:49:20.716792",
            
37
  "name": 
37
  "name": 
            
38
stability-corrections-perform-in-the-stable-boundary-layer-over-snow",
38
stability-corrections-perform-in-the-stable-boundary-layer-over-snow",
            
39
  "notes": "We used five different atmospheric turbulence datasets 
39
  "notes": "We used five different atmospheric turbulence datasets 
            
40
from four test sites, with these sites showing differences in their 
40
from four test sites, with these sites showing differences in their 
            
41
topographical characteristics. We chose one typical alpine test site 
41
topographical characteristics. We chose one typical alpine test site 
            
42
with high topographical complexity (Weissfluhjoch, Davos, Switzerland) 
42
with high topographical complexity (Weissfluhjoch, Davos, Switzerland) 
            
43
and three test sites consisting of one glacier site (Plaine Morte, 
43
and three test sites consisting of one glacier site (Plaine Morte, 
            
44
Crans-Montana, Switzerland) and two polar sites (Greenland and 
44
Crans-Montana, Switzerland) and two polar sites (Greenland and 
            
45
Antarctica) representing a quasi-ideal site with homogeneous surface 
45
Antarctica) representing a quasi-ideal site with homogeneous surface 
            
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and quasi infinite fetch in all directions.\r\nThe turbulent sensible 
46
and quasi infinite fetch in all directions.\r\nThe turbulent sensible 
            
47
heat flux was calculated using the eddy-covariance method. Note that 
47
heat flux was calculated using the eddy-covariance method. Note that 
            
48
the sonic temperature fluctuations have been converted into virtual 
48
the sonic temperature fluctuations have been converted into virtual 
            
49
temperature fluctuations. \r\nThree-dimensional wind velocity and air 
49
temperature fluctuations. \r\nThree-dimensional wind velocity and air 
            
50
temperature were processed using a linear detrending (Rannik and 
50
temperature were processed using a linear detrending (Rannik and 
            
51
Vesala, 1999) and a planar fit approach (Massmann and Lee, 2002) to 
51
Vesala, 1999) and a planar fit approach (Massmann and Lee, 2002) to 
            
52
rotate the coordinate system. Air temperature, relative humidity and 
52
rotate the coordinate system. Air temperature, relative humidity and 
            
53
air pressure from weather stations were used to calculate air 
53
air pressure from weather stations were used to calculate air 
            
54
properties, which are required for the data processing. The weather 
54
properties, which are required for the data processing. The weather 
            
55
stations are located in the immediate vicinity of the turbulence tower 
55
stations are located in the immediate vicinity of the turbulence tower 
            
56
and are affected by the same air masses. Turbulence data were averaged 
56
and are affected by the same air masses. Turbulence data were averaged 
            
57
to 30-min intervals, whilst changing to a 15-min time interval 
57
to 30-min intervals, whilst changing to a 15-min time interval 
            
58
marginally affects the heat fluxes at the Weissfluhjoch test site 
58
marginally affects the heat fluxes at the Weissfluhjoch test site 
            
59
(Mott et al., 2011). Note that we define a negative sensible heat flux 
59
(Mott et al., 2011). Note that we define a negative sensible heat flux 
            
60
as being directed towards the snow surface and a positive sensible 
60
as being directed towards the snow surface and a positive sensible 
            
61
heat flux as being directed upwards.\r\nThe selected datasets and 
61
heat flux as being directed upwards.\r\nThe selected datasets and 
            
62
corresponding test sites are briefly introduced 
62
corresponding test sites are briefly introduced 
            
63
below:\r\n\r\nWeissfluhjoch 2007 (WFJ07): A vertical set-up of two 
63
below:\r\n\r\nWeissfluhjoch 2007 (WFJ07): A vertical set-up of two 
            
64
three-dimensional ultrasonic anemometers (CSAT3, Campbell Scientific, 
64
three-dimensional ultrasonic anemometers (CSAT3, Campbell Scientific, 
            
65
Inc.) was used at the traditional field site Weissfluhjoch (2540 m 
65
Inc.) was used at the traditional field site Weissfluhjoch (2540 m 
            
66
asl.) to measure three-dimensional wind velocity and air temperature 
66
asl.) to measure three-dimensional wind velocity and air temperature 
            
67
at a frequency of 20 Hz. The sensors were mounted 3 m and 5 m above 
67
at a frequency of 20 Hz. The sensors were mounted 3 m and 5 m above 
            
68
the ground and provided reliable data for 50 days between 11 February 
68
the ground and provided reliable data for 50 days between 11 February 
            
69
2007 and 24 April 2007. Further information on the field campaign can 
69
2007 and 24 April 2007. Further information on the field campaign can 
            
70
be found in St\u00f6ssel et al. (2010) and Mott et al. 
70
be found in St\u00f6ssel et al. (2010) and Mott et al. 
            
71
(2011).\r\n\r\nWeissfluhjoch 2011-13 (WFJ11): Three-dimensional wind 
71
(2011).\r\n\r\nWeissfluhjoch 2011-13 (WFJ11): Three-dimensional wind 
            
72
velocity and air temperature were recorded at 5 m above the ground at 
72
velocity and air temperature were recorded at 5 m above the ground at 
            
73
a frequency of 10 Hz with a three-dimensional ultrasonic anemometer 
73
a frequency of 10 Hz with a three-dimensional ultrasonic anemometer 
            
74
(CSAT3). The analysis was conducted for data obtained between February 
74
(CSAT3). The analysis was conducted for data obtained between February 
            
75
and March in the years 2011-13.\r\n \r\nPlaine Morte 2007 (PM07): Two 
75
and March in the years 2011-13.\r\n \r\nPlaine Morte 2007 (PM07): Two 
            
76
three-dimensional ultrasonic anemometers (CSAT3) were installed on a 
76
three-dimensional ultrasonic anemometers (CSAT3) were installed on a 
            
77
horizontal boom facing opposite directions (west-north-west vs. 
77
horizontal boom facing opposite directions (west-north-west vs. 
            
78
east-south-east) at 3.75 m above the ground to measure air temperature 
78
east-south-east) at 3.75 m above the ground to measure air temperature 
            
79
and three-dimensional wind velocity at 20 Hz. The data were collected 
79
and three-dimensional wind velocity at 20 Hz. The data were collected 
            
80
at the almost flat field site on the Plaine Morte glacier (2750 m 
80
at the almost flat field site on the Plaine Morte glacier (2750 m 
            
81
asl.) near Crans-Montana, Switzerland from February to April 2007. 
81
asl.) near Crans-Montana, Switzerland from February to April 2007. 
            
82
High quality meteorological data were additionally recorded and used 
82
High quality meteorological data were additionally recorded and used 
            
83
to force the model. A detailed description about the set-up at the 
83
to force the model. A detailed description about the set-up at the 
            
84
Plaine Morte glacier can be found in Huwald et al. (2009) and Bou-Zeid 
84
Plaine Morte glacier can be found in Huwald et al. (2009) and Bou-Zeid 
            
85
et al. (2010).  \r\n\r\nGreenland 2000 (GR00): High-frequency 
85
et al. (2010).  \r\n\r\nGreenland 2000 (GR00): High-frequency 
            
86
three-dimensional ultrasonic anemometer measurements (CSAT3) were 
86
three-dimensional ultrasonic anemometer measurements (CSAT3) were 
            
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recorded at 50 Hz at the Summit Camp (72.3 \u00b0N, 38.8 \u00b0W, 3208 
87
recorded at 50 Hz at the Summit Camp (72.3 \u00b0N, 38.8 \u00b0W, 3208 
            
88
m asl.) located on the northern dome of the Greenland ice sheet. Data 
88
m asl.) located on the northern dome of the Greenland ice sheet. Data 
            
89
were collected at 1 m and 2 m above the snow surface during summer in 
89
were collected at 1 m and 2 m above the snow surface during summer in 
            
90
2000 and 2001. Additionally, meteorological measurements were obtained 
90
2000 and 2001. Additionally, meteorological measurements were obtained 
            
91
for the post processing and used to force the model. More information 
91
for the post processing and used to force the model. More information 
            
92
about the field campaign can be found in Cullen et al. (2007, 
92
about the field campaign can be found in Cullen et al. (2007, 
            
93
2014).\r\n\r\nAntarctica 2000 (AA00): A set-up of three vertical 
93
2014).\r\n\r\nAntarctica 2000 (AA00): A set-up of three vertical 
            
94
three-dimensional ultrasonic anemometers (DA-600, Kaijo Denki) were 
94
three-dimensional ultrasonic anemometers (DA-600, Kaijo Denki) were 
            
95
installed at Mizuho Station (70\u00b042' S, 44\u00b020' E, 2230 m 
95
installed at Mizuho Station (70\u00b042' S, 44\u00b020' E, 2230 m 
            
96
asl.) in Eastern Antarctica at 0.2, 1 and 25 m and recorded turbulence 
96
asl.) in Eastern Antarctica at 0.2, 1 and 25 m and recorded turbulence 
            
97
data at a frequency of 100 Hz from October to November 2000. Longwave 
97
data at a frequency of 100 Hz from October to November 2000. Longwave 
            
98
and shortwave radiation, relative humidity, air and snow surface 
98
and shortwave radiation, relative humidity, air and snow surface 
            
99
temperature were additionally measured and used to force the model. 
99
temperature were additionally measured and used to force the model. 
            
100
More information about the field campaign can be found in Nishimura 
100
More information about the field campaign can be found in Nishimura 
            
101
and Nemoto (2005).\r\n",
101
and Nemoto (2005).\r\n",
            
102
  "num_resources": 10,
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  "num_resources": 10,
            
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  "num_tags": 5,
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  "num_tags": 5,
            
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  "organization": {
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  "organization": {
            
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    "approval_status": "approved",
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    "approval_status": "approved",
            
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    "created": "2016-11-17T12:24:20.447699",
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    "created": "2016-11-17T12:24:20.447699",
            
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    "description": "CRYOS is the EPFL laboratory of the WSL/SLF - EPFL 
107
    "description": "CRYOS is the EPFL laboratory of the WSL/SLF - EPFL 
            
108
joint appointment for Prof. Michael Lehning. At his WSL side, Prof. 
108
joint appointment for Prof. Michael Lehning. At his WSL side, Prof. 
            
109
Michael Lehning is head of the research unit \"Snow and Permafrost\" 
109
Michael Lehning is head of the research unit \"Snow and Permafrost\" 
            
110
at SLF in Davos.\r\n \r\n###General Mission\r\nThe laboratory of 
110
at SLF in Davos.\r\n \r\n###General Mission\r\nThe laboratory of 
            
111
cryospheric sciences investigates the processes that shape snow and 
111
cryospheric sciences investigates the processes that shape snow and 
            
112
ice in mountains and polar regions. In particular, snow cover 
112
ice in mountains and polar regions. In particular, snow cover 
            
113
processes, snow-atmosphere interactions and mountain hydrology are in 
113
processes, snow-atmosphere interactions and mountain hydrology are in 
            
114
the focus of current research. This includes a strive for deeper 
114
the focus of current research. This includes a strive for deeper 
            
115
understanding of the complicated mass and energy exchange processes 
115
understanding of the complicated mass and energy exchange processes 
            
116
within, above and below a snow cover but also predictions of future 
116
within, above and below a snow cover but also predictions of future 
            
117
snow and ice in mountains and high latitudes. A newer work area is the 
117
snow and ice in mountains and high latitudes. A newer work area is the 
            
118
risk management and optimization in the field of renewable energy 
118
risk management and optimization in the field of renewable energy 
            
119
production based on our detailed understanding of water, wind and 
119
production based on our detailed understanding of water, wind and 
            
120
radiation processes in mountains.\r\n\r\nMore information: 
120
radiation processes in mountains.\r\n\r\nMore information: 
            
121
http://cryos.epfl.ch/",
121
http://cryos.epfl.ch/",
            
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    "id": "b2ef52fe-c56a-4973-8309-24837f3848ed",
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    "image_url": "2019-03-26-151807.125593CRYOSLogoFinal.jpg",
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    "image_url": "2019-03-26-151807.125593CRYOSLogoFinal.jpg",
            
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    "is_organization": true,
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    "is_organization": true,
            
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    "name": "cryos",
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    "name": "cryos",
            
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    "state": "active",
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    "state": "active",
            
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    "title": "CRYOS",
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    "title": "CRYOS",
            
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    "type": "organization"
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    "type": "organization"
            
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  "publication": "{\"publisher\": \"Boundary-Layer-Meteorology\", 
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  "publication": "{\"publisher\": \"Boundary-Layer-Meteorology\", 
            
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\"publication_year\": \"2017\"}",
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\"publication_year\": \"2017\"}",
            
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  "publication_state": "",
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  "publication_state": "reserved",
            
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  "related_publications": "* wsl:14116",
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  "related_publications": "* wsl:14116",
            
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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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  "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": "2018-06-26T14:23:38.819202",
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      "created": "2018-06-26T14:23:38.819202",
            
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      "description": "lower sensor",
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      "description": "lower sensor",
            
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      "doi": "",
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      "doi": "",
            
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      "format": "ZIP",
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      "format": "ZIP",
            
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