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{
            
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  "author": "[{\"name\": \"Mott\", \"affiliation\": \"WSL Institute 
2
  "author": "[{\"name\": \"Mott\", \"affiliation\": \"WSL Institute 
            
3
for Snow and Avalanche Research SLF, Davos, Switzerland\", 
3
for Snow and Avalanche Research SLF, Davos, Switzerland\", 
            
4
\"affiliation_03\": \"\", \"given_name\": \"Rebecca\", \"identifier\": 
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\"affiliation_03\": \"\", \"given_name\": \"Rebecca\", \"identifier\": 
            
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\"\", \"email\": \"mott@slf.ch\", \"affiliation_02\": \"\"}, 
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\"\", \"email\": \"mott@slf.ch\", \"affiliation_02\": \"\"}, 
            
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{\"name\": \"Schl\\u00f6gl\", \"affiliation\": \"\\u00c8cole 
6
{\"name\": \"Schl\\u00f6gl\", \"affiliation\": \"\\u00c8cole 
            
7
Polytechnique F\\u00e8d\\u00e8rale de Lausanne, Lausanne, Switzerland 
7
Polytechnique F\\u00e8d\\u00e8rale de Lausanne, Lausanne, Switzerland 
            
8
School of Architecture, Civil and Environmental Engineering, 
8
School of Architecture, Civil and Environmental Engineering, 
            
9
Laboratory of Cryospheric Sciences (CRYOS) and WSL Institute for Snow 
9
Laboratory of Cryospheric Sciences (CRYOS) and WSL Institute for Snow 
            
10
and Avalanche Research SLF, Davos, Switzerland\", \"affiliation_03\": 
10
and Avalanche Research SLF, Davos, Switzerland\", \"affiliation_03\": 
            
11
\"\", \"given_name\": \"Sebastian\", \"identifier\": \"\", \"email\": 
11
\"\", \"given_name\": \"Sebastian\", \"identifier\": \"\", \"email\": 
            
12
\"sebastian.schloegl@slf.ch\", \"affiliation_02\": \"\"}, {\"name\": 
12
\"sebastian.schloegl@slf.ch\", \"affiliation_02\": \"\"}, {\"name\": 
            
13
\"Dirks\", \"affiliation\": \"WSL Institute for Snow and Avalanche 
13
\"Dirks\", \"affiliation\": \"WSL Institute for Snow and Avalanche 
            
14
Research SLF, Davos, Switzerland\", \"affiliation_03\": \"\", 
14
Research SLF, Davos, Switzerland\", \"affiliation_03\": \"\", 
            
15
\"given_name\": \"Lisa\", \"identifier\": \"\", \"email\": 
15
\"given_name\": \"Lisa\", \"identifier\": \"\", \"email\": 
            
16
\"lisa.dirks@stmail.uni-bayreuth.de\", \"affiliation_02\": \"\"}, 
16
\"lisa.dirks@stmail.uni-bayreuth.de\", \"affiliation_02\": \"\"}, 
            
17
{\"name\": \"Lehning\", \"affiliation\": \"\\u00c8cole Polytechnique 
17
{\"name\": \"Lehning\", \"affiliation\": \"\\u00c8cole Polytechnique 
            
18
F\\u00e8d\\u00e8rale de Lausanne, Lausanne, Switzerland School of 
18
F\\u00e8d\\u00e8rale de Lausanne, Lausanne, Switzerland School of 
            
19
Architecture, Civil and Environmental Engineering, Laboratory of 
19
Architecture, Civil and Environmental Engineering, Laboratory of 
            
20
Cryospheric Sciences (CRYOS) and WSL Institute for Snow and Avalanche 
20
Cryospheric Sciences (CRYOS) and WSL Institute for Snow and Avalanche 
            
21
Research SLF, Davos, Switzerland\", \"affiliation_03\": \"\", 
21
Research SLF, Davos, Switzerland\", \"affiliation_03\": \"\", 
            
22
\"affiliation_02\": \"\", \"identifier\": \"\", \"email\": 
22
\"affiliation_02\": \"\", \"identifier\": \"\", \"email\": 
            
23
\"lehning@slf.ch\", \"given_name\": \"Michael\"}]",
23
\"lehning@slf.ch\", \"given_name\": \"Michael\"}]",
            
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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\": \"2014-04-17\", \"date_type\": \"created\", 
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  "date": "[{\"date\": \"2014-04-17\", \"date_type\": \"created\", 
            
27
\"end_date\": \"2014-05-28\"}, {\"date\": \"2015-04-15\", 
27
\"end_date\": \"2014-05-28\"}, {\"date\": \"2015-04-15\", 
            
28
\"date_type\": \"created\", \"end_date\": \"2015-05-29\"}, {\"date\": 
28
\"date_type\": \"created\", \"end_date\": \"2015-05-29\"}, {\"date\": 
            
29
\"2016-04-21\", \"date_type\": \"created\", \"end_date\": 
29
\"2016-04-21\", \"date_type\": \"created\", \"end_date\": 
            
30
\"2016-06-06\"}]",
30
\"2016-06-06\"}]",
            
31
  "doi": "10.16904/10",
31
  "doi": "10.16904/10",
            
32
  "extras": [
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  "extras": [
            
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    {
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    {
            
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      "key": "dora_link",
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      "key": "dora_link",
            
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      "value": ""
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      "value": ""
            
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    }
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    }
            
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  ],
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  ],
            
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  "funding": "[{\"grant_number\": \"\", \"institution\": \"Funding 
38
  "funding": "[{\"grant_number\": \"\", \"institution\": \"Funding 
            
39
information not available.\", \"institution_url\": \"\"}]",
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information not available.\", \"institution_url\": \"\"}]",
            
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  "groups": [],
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  "groups": [],
            
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  "id": "7e8c6dac-80cf-49d7-bd85-2a61d3336e6f",
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  "id": "7e8c6dac-80cf-49d7-bd85-2a61d3336e6f",
            
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  "isopen": true,
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  "isopen": true,
            
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  "language": "en",
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  "language": "en",
            
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  "license_id": "odc-odbl",
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  "license_id": "odc-odbl",
            
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  "license_title": "ODbL with Database Contents License (DbCL)",
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  "license_title": "ODbL with Database Contents License (DbCL)",
            
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  "license_url": "https://opendefinition.org/licenses/odc-odbl",
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  "license_url": "https://opendefinition.org/licenses/odc-odbl",
            
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  "maintainer": "{\"affiliation\": \"SLF\", \"identifier\": \"\", 
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  "maintainer": "{\"affiliation\": \"SLF\", \"identifier\": \"\", 
            
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\"given_name\": \"Rebecca\", \"name\": \"Mott\", \"email\": 
48
\"given_name\": \"Rebecca\", \"name\": \"Mott\", \"email\": 
            
49
\"mott@slf.ch\"}",
49
\"mott@slf.ch\"}",
            
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  "maintainer_email": null,
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  "maintainer_email": null,
            
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  "metadata_created": "2017-07-19T07:02:01.970488",
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  "metadata_created": "2017-07-19T07:02:01.970488",
            
n
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  "metadata_modified": "2023-09-13T14:22:55.374790",
n
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  "metadata_modified": "2023-09-13T14:23:02.542400",
            
53
  "name": "10-16904-10",
53
  "name": "10-16904-10",
            
54
  "notes": "This dataset contains eddy-covariance measurements in the 
54
  "notes": "This dataset contains eddy-covariance measurements in the 
            
55
ablation period of 2014-2016. Measurements were taken from two 
55
ablation period of 2014-2016. Measurements were taken from two 
            
56
turbulence towers over a long-lasting snow patch, which are 5 m apart 
56
turbulence towers over a long-lasting snow patch, which are 5 m apart 
            
57
from each other (2014 and 2015). The turbulence towers were equipped 
57
from each other (2014 and 2015). The turbulence towers were equipped 
            
58
with two YOUNG ultrasonic anemometers mounted 0.7 m (in 2014) and 3.3 
58
with two YOUNG ultrasonic anemometers mounted 0.7 m (in 2014) and 3.3 
            
59
m (in 2015) above snow-free ground, two ultrasonic anemometers (CSAT3, 
59
m (in 2015) above snow-free ground, two ultrasonic anemometers (CSAT3, 
            
60
Campbell Scientific, Inc.) mounted at 2.6 m (in 2014) and 2.2 m (in 
60
Campbell Scientific, Inc.) mounted at 2.6 m (in 2014) and 2.2 m (in 
            
61
2015) above snow-free ground and one anemometer (DA-600, Kaijo Denki) 
61
2015) above snow-free ground and one anemometer (DA-600, Kaijo Denki) 
            
62
mounted at 0.3 m above snow surface.  \r\n\r\nThe measurement setup 
62
mounted at 0.3 m above snow surface.  \r\n\r\nThe measurement setup 
            
63
changed in 2016 and includes a measurement above the snow-free ground 
63
changed in 2016 and includes a measurement above the snow-free ground 
            
64
in upwind direction (Swiss coordinates: 790191/176689). The 
64
in upwind direction (Swiss coordinates: 790191/176689). The 
            
65
measurement tower is equipped with one ultrasonic anemometer (CSAT3, 
65
measurement tower is equipped with one ultrasonic anemometer (CSAT3, 
            
66
Campbell Scientific, Inc.) in 3.3 m above the snow-free ground. 
66
Campbell Scientific, Inc.) in 3.3 m above the snow-free ground. 
            
67
Additionally, one measurement tower is installed above the 
67
Additionally, one measurement tower is installed above the 
            
68
long-Lasting snow patch and equipped with the same setup as 
68
long-Lasting snow patch and equipped with the same setup as 
            
69
2015.\r\n\r\nTurbulence data were sampled at a frequency of 20 Hz. The 
69
2015.\r\n\r\nTurbulence data were sampled at a frequency of 20 Hz. The 
            
70
processing of the data to quality controlled fluxes has been done with 
70
processing of the data to quality controlled fluxes has been done with 
            
71
the Biomicrometeorology flux software (Thomas et al., 2009). The 
71
the Biomicrometeorology flux software (Thomas et al., 2009). The 
            
72
program applies plausibility tests and a despiking test after Vickers 
72
program applies plausibility tests and a despiking test after Vickers 
            
73
and Mahrt (1997) on the measured data. The routine further applies a 
73
and Mahrt (1997) on the measured data. The routine further applies a 
            
74
time-lag correction and considers the deployment (e.g.  the sonic 
74
time-lag correction and considers the deployment (e.g.  the sonic 
            
75
azimuth). A frequency response correction (Moore, 1986) is done and a 
75
azimuth). A frequency response correction (Moore, 1986) is done and a 
            
76
three-dimensional rotation is performed. Finally, quality 
76
three-dimensional rotation is performed. Finally, quality 
            
77
assurance/quality control (QA/QC) flags after Foken et al., (2004) are 
77
assurance/quality control (QA/QC) flags after Foken et al., (2004) are 
            
78
issued and fast Fourier transform power and co-spectra are calculated.  
78
issued and fast Fourier transform power and co-spectra are calculated.  
            
79
The change in snow height is considered in the post-processing for 
79
The change in snow height is considered in the post-processing for 
            
80
every measurement day. The turbulence data were averaged to 30 minute 
80
every measurement day. The turbulence data were averaged to 30 minute 
            
81
intervals. ",
81
intervals. ",
            
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  "num_resources": 16,
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  "num_resources": 16,
            
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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 
87
    "description": "CRYOS is the EPFL laboratory of the WSL/SLF - EPFL 
            
88
joint appointment for Prof. Michael Lehning. At his WSL side, Prof. 
88
joint appointment for Prof. Michael Lehning. At his WSL side, Prof. 
            
89
Michael Lehning is head of the research unit \"Snow and Permafrost\" 
89
Michael Lehning is head of the research unit \"Snow and Permafrost\" 
            
90
at SLF in Davos.\r\n \r\n###General Mission\r\nThe laboratory of 
90
at SLF in Davos.\r\n \r\n###General Mission\r\nThe laboratory of 
            
91
cryospheric sciences investigates the processes that shape snow and 
91
cryospheric sciences investigates the processes that shape snow and 
            
92
ice in mountains and polar regions. In particular, snow cover 
92
ice in mountains and polar regions. In particular, snow cover 
            
93
processes, snow-atmosphere interactions and mountain hydrology are in 
93
processes, snow-atmosphere interactions and mountain hydrology are in 
            
94
the focus of current research. This includes a strive for deeper 
94
the focus of current research. This includes a strive for deeper 
            
95
understanding of the complicated mass and energy exchange processes 
95
understanding of the complicated mass and energy exchange processes 
            
96
within, above and below a snow cover but also predictions of future 
96
within, above and below a snow cover but also predictions of future 
            
97
snow and ice in mountains and high latitudes. A newer work area is the 
97
snow and ice in mountains and high latitudes. A newer work area is the 
            
98
risk management and optimization in the field of renewable energy 
98
risk management and optimization in the field of renewable energy 
            
99
production based on our detailed understanding of water, wind and 
99
production based on our detailed understanding of water, wind and 
            
100
radiation processes in mountains.\r\n\r\nMore information: 
100
radiation processes in mountains.\r\n\r\nMore information: 
            
101
http://cryos.epfl.ch/",
101
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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    "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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  "publication": "{\"publisher\": \"WSL Institute for Snow and 
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  "publication": "{\"publisher\": \"WSL Institute for Snow and 
            
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Avalanche Research SLF\", \"publication_year\": \"2017\"}",
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Avalanche Research SLF\", \"publication_year\": \"2017\"}",
            
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  "publication_state": "published",
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  "publication_state": "published",
            
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  "related_publications": "",
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  "related_publications": "",
            
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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": "2017-07-19T11:00:32.955353",
            
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      "description": "Eddy-covariance measurement with an ultrasonic 
125
      "description": "Eddy-covariance measurement with an ultrasonic 
            
126
anemometer (CSAT3, Campbell Scientific, Inc.) in 2.6 m.",
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anemometer (CSAT3, Campbell Scientific, Inc.) in 2.6 m.",
            
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      "name": "S1 2014",
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      "size": 725025,
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      "created": "2017-07-19T12:00:49.356035",
            
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      "description": "Eddy-covariance measurement with an ultrasonic 
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      "description": "Eddy-covariance measurement with an ultrasonic 
            
155
anemometer (CSAT3, Campbell Scientific, Inc.) in 2.6 m.",
155
anemometer (CSAT3, Campbell Scientific, Inc.) in 2.6 m.",
            
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      "doi": "",
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      "doi": "",
            
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swisstopo (JD100042)",
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(2094 m asl) in the upper Dischma valley, Davos, Switzerland. Swiss 
577
(2094 m asl) in the upper Dischma valley, Davos, Switzerland. Swiss 
            
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  "tags": [
            
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    {
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    {
            
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      "display_name": "DISCHMEX",
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      "display_name": "DISCHMEX",
            
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      "display_name": "PATCHY SNOW COVERS",
            
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      "name": "PATCHY SNOW COVERS",
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      "name": "PATCHY SNOW COVERS",
            
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      "id": "b2b233ee-7728-4219-85b5-3cd3bca463cd",
            
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      "name": "SNOW PATCH",
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      "name": "SNOW PATCH",
            
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      "state": "active",
            
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    {
610
    {
            
609
      "display_name": "TURBULENT SENSIBLE HEAT FLUXES",
611
      "display_name": "TURBULENT SENSIBLE HEAT FLUXES",
            
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      "name": "TURBULENT SENSIBLE HEAT FLUXES",
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      "name": "TURBULENT SENSIBLE HEAT FLUXES",
            
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    }
            
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  ],
617
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616
  "title": "DISCHMEX - Impact of extreme land-surface heterogeneity on 
618
  "title": "DISCHMEX - Impact of extreme land-surface heterogeneity on 
            
617
micrometeorology over spring snow-cover",
619
micrometeorology over spring snow-cover",
            
618
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620
  "type": "dataset",
            
619
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621
  "url": null,
            
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622
  "version": "1.0"
            
621
}
623
}