Changes
On May 21, 2024 at 12:26:43 PM UTC, Michael Haugeneder:
-
Added resource t2_3m.zip to Turbulence in The Strongly Heterogeneous Near-Surface Boundary Layer over Patchy Snow
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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\": | ||
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25 | "license_title": "WSL Data Policy", | 25 | "license_title": "WSL Data Policy", | ||
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n | 33 | "metadata_modified": "2024-05-21T12:25:58.988669", | n | 33 | "metadata_modified": "2024-05-21T12:26:43.093455", |
34 | "name": "turbulence-patchy-snow-cover", | 34 | "name": "turbulence-patchy-snow-cover", | ||
35 | "notes": "This dataset contains the raw data that is analyzed in the | 35 | "notes": "This dataset contains the raw data that is analyzed in the | ||
36 | publication entitled \"Turbulence in The Strongly Heterogeneous | 36 | publication entitled \"Turbulence in The Strongly Heterogeneous | ||
37 | Near-Surface Boundary Layer over Patchy Snow\". Please find | 37 | Near-Surface Boundary Layer over Patchy Snow\". Please find | ||
38 | information on the individual data files in the description of the | 38 | information on the individual data files in the description of the | ||
39 | files.", | 39 | files.", | ||
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44 | "created": "2021-08-23T15:25:48.676190", | 44 | "created": "2021-08-23T15:25:48.676190", | ||
45 | "description": "The research group \u00abSnow Hydrology\u00bb | 45 | "description": "The research group \u00abSnow Hydrology\u00bb | ||
46 | investigates snow as a component of the hydrological cycle. In the | 46 | investigates snow as a component of the hydrological cycle. In the | ||
47 | Alps a significant percentage of precipitation comes in the form of | 47 | Alps a significant percentage of precipitation comes in the form of | ||
48 | 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 | ||
49 | runoff from alpine watersheds. Of particular interest for our research | 49 | runoff from alpine watersheds. Of particular interest for our research | ||
50 | is to enhance estimations of snow water resources and subsequent melt | 50 | is to enhance estimations of snow water resources and subsequent melt | ||
51 | 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 | ||
52 | projects and methods. The latest measuring techniques are used to | 52 | projects and methods. The latest measuring techniques are used to | ||
53 | investigate snow distribution patterns in alpine terrain, e.g. laser | 53 | investigate snow distribution patterns in alpine terrain, e.g. laser | ||
54 | scanning or radar technology. We use different types of numerical | 54 | scanning or radar technology. We use different types of numerical | ||
55 | models to calculate snow water resources based on input data from | 55 | models to calculate snow water resources based on input data from | ||
56 | meteorological monitoring networks. These models are being used to | 56 | meteorological monitoring networks. These models are being used to | ||
57 | predict the consequences of climate change on the water balance of | 57 | predict the consequences of climate change on the water balance of | ||
58 | mountain watersheds. The models also constitute a valuable tool for | 58 | mountain watersheds. The models also constitute a valuable tool for | ||
59 | our operational services, such as periodic snow hydrological | 59 | our operational services, such as periodic snow hydrological | ||
60 | bulletins, which contribute to the federal flood prevention and | 60 | bulletins, which contribute to the federal flood prevention and | ||
61 | forecasting system.\r\n\r\nThe research group \u00abSnow | 61 | forecasting system.\r\n\r\nThe research group \u00abSnow | ||
62 | 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 | ||
63 | Davosian research groups and the research unit \u201dMountain | 63 | Davosian research groups and the research unit \u201dMountain | ||
64 | Hydrology and Mass Movements\u201d in Birmensdorf.", | 64 | Hydrology and Mass Movements\u201d in Birmensdorf.", | ||
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70 | "title": "Snow Hydrology", | 70 | "title": "Snow Hydrology", | ||
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239 | {\"level\":\"public\",\"allowed_users\":\"\",\"shared_secret\":\"\"}", | ||||
240 | "size": 906522928, | ||||
241 | "state": "active", | ||||
242 | "url": | ||||
243 | c67/resource/a850ebcc-a124-4e27-8c90-8781e10522ae/download/t2_3m.zip", | ||||
244 | "url_type": "upload" | ||||
219 | } | 245 | } | ||
220 | ], | 246 | ], | ||
221 | "spatial": | 247 | "spatial": | ||
222 | \":\"Point\",\"coordinates\":[9.922499656677246,46.719613134706506]}", | 248 | \":\"Point\",\"coordinates\":[9.922499656677246,46.719613134706506]}", | ||
223 | "spatial_info": "Switzerland", | 249 | "spatial_info": "Switzerland", | ||
224 | "state": "active", | 250 | "state": "active", | ||
225 | "subtitle": "", | 251 | "subtitle": "", | ||
226 | "tags": [ | 252 | "tags": [ | ||
227 | { | 253 | { | ||
228 | "display_name": "ATMOSPHERIC TURBULENCE", | 254 | "display_name": "ATMOSPHERIC TURBULENCE", | ||
229 | "id": "33a2c66c-7196-447c-ae3c-603212e9492d", | 255 | "id": "33a2c66c-7196-447c-ae3c-603212e9492d", | ||
230 | "name": "ATMOSPHERIC TURBULENCE", | 256 | "name": "ATMOSPHERIC TURBULENCE", | ||
231 | "state": "active", | 257 | "state": "active", | ||
232 | "vocabulary_id": null | 258 | "vocabulary_id": null | ||
233 | }, | 259 | }, | ||
234 | { | 260 | { | ||
235 | "display_name": "EDDY-COVARIANCE MEASUREMENTS", | 261 | "display_name": "EDDY-COVARIANCE MEASUREMENTS", | ||
236 | "id": "3d92ab0f-64bb-4f23-a670-1d676d15f858", | 262 | "id": "3d92ab0f-64bb-4f23-a670-1d676d15f858", | ||
237 | "name": "EDDY-COVARIANCE MEASUREMENTS", | 263 | "name": "EDDY-COVARIANCE MEASUREMENTS", | ||
238 | "state": "active", | 264 | "state": "active", | ||
239 | "vocabulary_id": null | 265 | "vocabulary_id": null | ||
240 | }, | 266 | }, | ||
241 | { | 267 | { | ||
242 | "display_name": "PATCHY SNOW COVER", | 268 | "display_name": "PATCHY SNOW COVER", | ||
243 | "id": "61d8a21a-8ef9-4900-8050-bf3e84c05fc5", | 269 | "id": "61d8a21a-8ef9-4900-8050-bf3e84c05fc5", | ||
244 | "name": "PATCHY SNOW COVER", | 270 | "name": "PATCHY SNOW COVER", | ||
245 | "state": "active", | 271 | "state": "active", | ||
246 | "vocabulary_id": null | 272 | "vocabulary_id": null | ||
247 | }, | 273 | }, | ||
248 | { | 274 | { | ||
249 | "display_name": "SNOW MELT", | 275 | "display_name": "SNOW MELT", | ||
250 | "id": "4452e5c9-c707-4c61-bd1c-28816181a043", | 276 | "id": "4452e5c9-c707-4c61-bd1c-28816181a043", | ||
251 | "name": "SNOW MELT", | 277 | "name": "SNOW MELT", | ||
252 | "state": "active", | 278 | "state": "active", | ||
253 | "vocabulary_id": null | 279 | "vocabulary_id": null | ||
254 | }, | 280 | }, | ||
255 | { | 281 | { | ||
256 | "display_name": "SURFACE HEAT EXCHANGE", | 282 | "display_name": "SURFACE HEAT EXCHANGE", | ||
257 | "id": "cb61d6bd-bf4d-4fd6-a8e2-8dbbbd90d418", | 283 | "id": "cb61d6bd-bf4d-4fd6-a8e2-8dbbbd90d418", | ||
258 | "name": "SURFACE HEAT EXCHANGE", | 284 | "name": "SURFACE HEAT EXCHANGE", | ||
259 | "state": "active", | 285 | "state": "active", | ||
260 | "vocabulary_id": null | 286 | "vocabulary_id": null | ||
261 | } | 287 | } | ||
262 | ], | 288 | ], | ||
263 | "title": "Turbulence in The Strongly Heterogeneous Near-Surface | 289 | "title": "Turbulence in The Strongly Heterogeneous Near-Surface | ||
264 | Boundary Layer over Patchy Snow", | 290 | Boundary Layer over Patchy Snow", | ||
265 | "type": "dataset", | 291 | "type": "dataset", | ||
266 | "url": null, | 292 | "url": null, | ||
267 | "version": "1.0" | 293 | "version": "1.0" | ||
268 | } | 294 | } |