Changes
On May 21, 2024 at 12:25:52 PM UTC, Administrator:
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Updated description of Turbulence in The Strongly Heterogeneous Near-Surface Boundary Layer over Patchy Snow from
EnviDat Admin message: this dataset is being recreated, please have patience. Data and code for the publication. The data is raw data. Processed data can be obtained upon request.
toThis dataset contains the raw data that is analyzed in the publication entitled "Turbulence in The Strongly Heterogeneous Near-Surface Boundary Layer over Patchy Snow". Please find information on the individual data files in the description of the files.
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Changed value of field
related_publications
tohttps://www.dora.lib4ri.ch/wsl/islandora/object/wsl:35982
in Turbulence in The Strongly Heterogeneous Near-Surface Boundary Layer over Patchy Snow -
Added resource t2_2m.zip to Turbulence in The Strongly Heterogeneous Near-Surface Boundary Layer over Patchy Snow
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Added resource aws.zip to Turbulence in The Strongly Heterogeneous Near-Surface Boundary Layer over Patchy Snow
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Deleted resource t2_2m.zip from Turbulence in The Strongly Heterogeneous Near-Surface Boundary Layer over Patchy Snow
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Deleted resource t2_3m.zip from Turbulence in The Strongly Heterogeneous Near-Surface Boundary Layer over Patchy Snow
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Deleted resource aws.zip from Turbulence in The Strongly Heterogeneous Near-Surface Boundary Layer over Patchy Snow
f | 1 | { | f | 1 | { |
2 | "author": "[{\"affiliation\": \"SLF\", \"affiliation_02\": \"\", | 2 | "author": "[{\"affiliation\": \"SLF\", \"affiliation_02\": \"\", | ||
3 | \"affiliation_03\": \"\", \"email\": \"michael.haugeneder@slf.ch\", | 3 | \"affiliation_03\": \"\", \"email\": \"michael.haugeneder@slf.ch\", | ||
4 | \"given_name\": \"Michael\", \"identifier\": \"0000-0003-3228-9868\", | 4 | \"given_name\": \"Michael\", \"identifier\": \"0000-0003-3228-9868\", | ||
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7 | \"lehning@slf.ch\", \"given_name\": \"Michael\", \"identifier\": | 7 | \"lehning@slf.ch\", \"given_name\": \"Michael\", \"identifier\": | ||
8 | \"0000-0002-8442-0875\", \"name\": \"Lehning\"}, {\"affiliation\": | 8 | \"0000-0002-8442-0875\", \"name\": \"Lehning\"}, {\"affiliation\": | ||
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10 | \"email\": \"mott@slf.ch\", \"given_name\": \"Rebecca\", | 10 | \"email\": \"mott@slf.ch\", \"given_name\": \"Rebecca\", | ||
11 | \"identifier\": \"\", \"name\": \"Mott\"}]", | 11 | \"identifier\": \"\", \"name\": \"Mott\"}]", | ||
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14 | "date": "[{\"date\": \"2021-05-21\", \"date_type\": \"collected\", | 14 | "date": "[{\"date\": \"2021-05-21\", \"date_type\": \"collected\", | ||
15 | \"end_date\": \"2021-06-11\"}]", | 15 | \"end_date\": \"2021-06-11\"}]", | ||
16 | "doi": "10.16904/envidat.399", | 16 | "doi": "10.16904/envidat.399", | ||
17 | "funding": "[{\"grant_number\": \"188554\", \"institution\": | 17 | "funding": "[{\"grant_number\": \"188554\", \"institution\": | ||
18 | \"SNF\", \"institution_url\": | 18 | \"SNF\", \"institution_url\": | ||
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25 | "license_title": "WSL Data Policy", | 25 | "license_title": "WSL Data Policy", | ||
26 | "license_url": | 26 | "license_url": | ||
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n | 33 | "metadata_modified": "2024-05-21T12:08:16.920601", | n | 33 | "metadata_modified": "2024-05-21T12:25:52.736451", |
34 | "name": "turbulence-patchy-snow-cover", | 34 | "name": "turbulence-patchy-snow-cover", | ||
n | 35 | "notes": "EnviDat Admin message: this dataset is being recreated, | n | 35 | "notes": "This dataset contains the raw data that is analyzed in the |
36 | please have patience.\r\n\r\nData and code for the publication. The | 36 | publication entitled \"Turbulence in The Strongly Heterogeneous | ||
37 | data is raw data. Processed data can be obtained upon request.", | 37 | Near-Surface Boundary Layer over Patchy Snow\". Please find | ||
38 | information on the individual data files in the description of the | ||||
39 | files.", | ||||
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42 | "created": "2021-08-23T15:25:48.676190", | 44 | "created": "2021-08-23T15:25:48.676190", | ||
43 | "description": "The research group \u00abSnow Hydrology\u00bb | 45 | "description": "The research group \u00abSnow Hydrology\u00bb | ||
44 | investigates snow as a component of the hydrological cycle. In the | 46 | investigates snow as a component of the hydrological cycle. In the | ||
45 | Alps a significant percentage of precipitation comes in the form of | 47 | Alps a significant percentage of precipitation comes in the form of | ||
46 | snow. The timing of snow melt thus influences the annual dynamics of | 48 | snow. The timing of snow melt thus influences the annual dynamics of | ||
47 | runoff from alpine watersheds. Of particular interest for our research | 49 | runoff from alpine watersheds. Of particular interest for our research | ||
48 | is to enhance estimations of snow water resources and subsequent melt | 50 | is to enhance estimations of snow water resources and subsequent melt | ||
49 | water discharge.\r\n\r\nThe research group covers a broad range of | 51 | water discharge.\r\n\r\nThe research group covers a broad range of | ||
50 | projects and methods. The latest measuring techniques are used to | 52 | projects and methods. The latest measuring techniques are used to | ||
51 | investigate snow distribution patterns in alpine terrain, e.g. laser | 53 | investigate snow distribution patterns in alpine terrain, e.g. laser | ||
52 | scanning or radar technology. We use different types of numerical | 54 | scanning or radar technology. We use different types of numerical | ||
53 | models to calculate snow water resources based on input data from | 55 | models to calculate snow water resources based on input data from | ||
54 | meteorological monitoring networks. These models are being used to | 56 | meteorological monitoring networks. These models are being used to | ||
55 | predict the consequences of climate change on the water balance of | 57 | predict the consequences of climate change on the water balance of | ||
56 | mountain watersheds. The models also constitute a valuable tool for | 58 | mountain watersheds. The models also constitute a valuable tool for | ||
57 | our operational services, such as periodic snow hydrological | 59 | our operational services, such as periodic snow hydrological | ||
58 | bulletins, which contribute to the federal flood prevention and | 60 | bulletins, which contribute to the federal flood prevention and | ||
59 | forecasting system.\r\n\r\nThe research group \u00abSnow | 61 | forecasting system.\r\n\r\nThe research group \u00abSnow | ||
60 | Hydrology\u00bb is based in Davos and ensures the link between other | 62 | Hydrology\u00bb is based in Davos and ensures the link between other | ||
61 | Davosian research groups and the research unit \u201dMountain | 63 | Davosian research groups and the research unit \u201dMountain | ||
62 | Hydrology and Mass Movements\u201d in Birmensdorf.", | 64 | Hydrology and Mass Movements\u201d in Birmensdorf.", | ||
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246 | "spatial_info": "Switzerland", | 222 | "spatial_info": "Switzerland", | ||
247 | "state": "active", | 223 | "state": "active", | ||
248 | "subtitle": "", | 224 | "subtitle": "", | ||
249 | "tags": [ | 225 | "tags": [ | ||
250 | { | 226 | { | ||
251 | "display_name": "ATMOSPHERIC TURBULENCE", | 227 | "display_name": "ATMOSPHERIC TURBULENCE", | ||
252 | "id": "33a2c66c-7196-447c-ae3c-603212e9492d", | 228 | "id": "33a2c66c-7196-447c-ae3c-603212e9492d", | ||
253 | "name": "ATMOSPHERIC TURBULENCE", | 229 | "name": "ATMOSPHERIC TURBULENCE", | ||
254 | "state": "active", | 230 | "state": "active", | ||
255 | "vocabulary_id": null | 231 | "vocabulary_id": null | ||
256 | }, | 232 | }, | ||
257 | { | 233 | { | ||
258 | "display_name": "EDDY-COVARIANCE MEASUREMENTS", | 234 | "display_name": "EDDY-COVARIANCE MEASUREMENTS", | ||
259 | "id": "3d92ab0f-64bb-4f23-a670-1d676d15f858", | 235 | "id": "3d92ab0f-64bb-4f23-a670-1d676d15f858", | ||
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262 | "vocabulary_id": null | 238 | "vocabulary_id": null | ||
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264 | { | 240 | { | ||
265 | "display_name": "PATCHY SNOW COVER", | 241 | "display_name": "PATCHY SNOW COVER", | ||
266 | "id": "61d8a21a-8ef9-4900-8050-bf3e84c05fc5", | 242 | "id": "61d8a21a-8ef9-4900-8050-bf3e84c05fc5", | ||
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269 | "vocabulary_id": null | 245 | "vocabulary_id": null | ||
270 | }, | 246 | }, | ||
271 | { | 247 | { | ||
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273 | "id": "4452e5c9-c707-4c61-bd1c-28816181a043", | 249 | "id": "4452e5c9-c707-4c61-bd1c-28816181a043", | ||
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276 | "vocabulary_id": null | 252 | "vocabulary_id": null | ||
277 | }, | 253 | }, | ||
278 | { | 254 | { | ||
279 | "display_name": "SURFACE HEAT EXCHANGE", | 255 | "display_name": "SURFACE HEAT EXCHANGE", | ||
280 | "id": "cb61d6bd-bf4d-4fd6-a8e2-8dbbbd90d418", | 256 | "id": "cb61d6bd-bf4d-4fd6-a8e2-8dbbbd90d418", | ||
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282 | "state": "active", | 258 | "state": "active", | ||
283 | "vocabulary_id": null | 259 | "vocabulary_id": null | ||
284 | } | 260 | } | ||
285 | ], | 261 | ], | ||
286 | "title": "Turbulence in The Strongly Heterogeneous Near-Surface | 262 | "title": "Turbulence in The Strongly Heterogeneous Near-Surface | ||
287 | Boundary Layer over Patchy Snow", | 263 | Boundary Layer over Patchy Snow", | ||
288 | "type": "dataset", | 264 | "type": "dataset", | ||
289 | "url": null, | 265 | "url": null, | ||
290 | "version": "1.0" | 266 | "version": "1.0" | ||
291 | } | 267 | } |