Changes
On November 21, 2022 at 7:56:49 AM UTC, Michael Haugeneder:
-
Changed value of field
related_publications
toHaugeneder, M., Lehning, M., Reynolds, D. et al. A Novel Method to Quantify Near-Surface Boundary-Layer Dynamics at Ultra-High Spatio-Temporal Resolution. Boundary-Layer Meteorol (2022). https://doi.org/10.1007/s10546-022-00752-3
in Quantifying Surface Heat Exchange over Heterogeneous Land Surfaces at Ultra-High Spatio-Temporal Resolution
f | 1 | { | f | 1 | { |
2 | "author": "[{\"affiliation\": \"SLF\", \"affiliation_02\": \"EPFL\", | 2 | "author": "[{\"affiliation\": \"SLF\", \"affiliation_02\": \"EPFL\", | ||
3 | \"affiliation_03\": \"\", \"data_credit\": [\"collection\", | 3 | \"affiliation_03\": \"\", \"data_credit\": [\"collection\", | ||
4 | \"software\", \"publication\"], \"email\": | 4 | \"software\", \"publication\"], \"email\": | ||
5 | \"michael.haugeneder@slf.ch\", \"given_name\": \"Michael\", | 5 | \"michael.haugeneder@slf.ch\", \"given_name\": \"Michael\", | ||
6 | \"identifier\": \"0000-0003-3228-9868\", \"name\": \"Haugeneder\"}, | 6 | \"identifier\": \"0000-0003-3228-9868\", \"name\": \"Haugeneder\"}, | ||
7 | {\"affiliation\": \"SLF\", \"affiliation_02\": \"EPFL\", | 7 | {\"affiliation\": \"SLF\", \"affiliation_02\": \"EPFL\", | ||
8 | \"affiliation_03\": \"\", \"email\": \"lehning@slf.ch\", | 8 | \"affiliation_03\": \"\", \"email\": \"lehning@slf.ch\", | ||
9 | \"given_name\": \"Michael\", \"identifier\": \"\", \"name\": | 9 | \"given_name\": \"Michael\", \"identifier\": \"\", \"name\": | ||
10 | \"Lehning\"}, {\"affiliation\": \"SLF\", \"affiliation_02\": \"\", | 10 | \"Lehning\"}, {\"affiliation\": \"SLF\", \"affiliation_02\": \"\", | ||
11 | \"affiliation_03\": \"\", \"email\": \"jonas@slf.ch\", \"given_name\": | 11 | \"affiliation_03\": \"\", \"email\": \"jonas@slf.ch\", \"given_name\": | ||
12 | \"Tobias\", \"identifier\": \"\", \"name\": \"Jonas\"}, | 12 | \"Tobias\", \"identifier\": \"\", \"name\": \"Jonas\"}, | ||
13 | {\"affiliation\": \"SLF\", \"affiliation_02\": \"\", | 13 | {\"affiliation\": \"SLF\", \"affiliation_02\": \"\", | ||
14 | \"affiliation_03\": \"\", \"email\": \"mott@slf.ch\", \"given_name\": | 14 | \"affiliation_03\": \"\", \"email\": \"mott@slf.ch\", \"given_name\": | ||
15 | \"Rebecca\", \"identifier\": \"\", \"name\": \"Mott\"}]", | 15 | \"Rebecca\", \"identifier\": \"\", \"name\": \"Mott\"}]", | ||
16 | "author_email": null, | 16 | "author_email": null, | ||
17 | "creator_user_id": "ebd22060-c56d-419b-a56e-9e171f19e7e5", | 17 | "creator_user_id": "ebd22060-c56d-419b-a56e-9e171f19e7e5", | ||
18 | "date": "[{\"date\": \"2021-04-28\", \"date_type\": \"collected\", | 18 | "date": "[{\"date\": \"2021-04-28\", \"date_type\": \"collected\", | ||
19 | \"end_date\": \"\"}]", | 19 | \"end_date\": \"\"}]", | ||
20 | "doi": "10.16904/envidat.299", | 20 | "doi": "10.16904/envidat.299", | ||
21 | "funding": "[{\"grant_number\": \"\", \"institution\": \"SNF\", | 21 | "funding": "[{\"grant_number\": \"\", \"institution\": \"SNF\", | ||
22 | \"institution_url\": \"https://p3.snf.ch/project-188554\"}]", | 22 | \"institution_url\": \"https://p3.snf.ch/project-188554\"}]", | ||
23 | "groups": [], | 23 | "groups": [], | ||
24 | "id": "048b0129-b533-4310-8159-3c111b431fc7", | 24 | "id": "048b0129-b533-4310-8159-3c111b431fc7", | ||
25 | "isopen": false, | 25 | "isopen": false, | ||
26 | "language": "en", | 26 | "language": "en", | ||
27 | "license_id": "wsl-data", | 27 | "license_id": "wsl-data", | ||
28 | "license_title": "WSL Data Policy", | 28 | "license_title": "WSL Data Policy", | ||
29 | "license_url": | 29 | "license_url": | ||
30 | ps://www.wsl.ch/en/about-wsl/programmes-and-initiatives/envidat.html", | 30 | ps://www.wsl.ch/en/about-wsl/programmes-and-initiatives/envidat.html", | ||
31 | "maintainer": "{\"affiliation\": \"SLF\", \"email\": | 31 | "maintainer": "{\"affiliation\": \"SLF\", \"email\": | ||
32 | \"michael.haugeneder@slf.ch\", \"given_name\": \"Michael\", | 32 | \"michael.haugeneder@slf.ch\", \"given_name\": \"Michael\", | ||
33 | \"identifier\": \"0000-0003-3228-9868\", \"name\": \"Haugeneder\"}", | 33 | \"identifier\": \"0000-0003-3228-9868\", \"name\": \"Haugeneder\"}", | ||
34 | "maintainer_email": null, | 34 | "maintainer_email": null, | ||
35 | "metadata_created": "2022-02-24T16:15:53.573278", | 35 | "metadata_created": "2022-02-24T16:15:53.573278", | ||
n | 36 | "metadata_modified": "2022-10-04T07:05:00.002285", | n | 36 | "metadata_modified": "2022-11-21T07:56:49.683737", |
37 | "name": "weird", | 37 | "name": "weird", | ||
38 | "notes": "The lateral transport of heat above abrupt | 38 | "notes": "The lateral transport of heat above abrupt | ||
39 | (sub-)metre-scale steps in land surface temperature influences the | 39 | (sub-)metre-scale steps in land surface temperature influences the | ||
40 | local surface energy balance. We present a novel experimental method | 40 | local surface energy balance. We present a novel experimental method | ||
41 | to investigate the stratification and dynamics of the near-surface | 41 | to investigate the stratification and dynamics of the near-surface | ||
42 | atmospheric layer over a heterogeneous land surface. Using a high | 42 | atmospheric layer over a heterogeneous land surface. Using a high | ||
43 | resolution thermal infrared camera pointing at synthetic screens, a | 43 | resolution thermal infrared camera pointing at synthetic screens, a | ||
44 | 30Hz sequence of frames is recorded. The screens are deployed upright | 44 | 30Hz sequence of frames is recorded. The screens are deployed upright | ||
45 | and horizontally aligned with the prevailing wind direction. The | 45 | and horizontally aligned with the prevailing wind direction. The | ||
46 | screen\u2019s surface temperature serves as a proxy for the local air | 46 | screen\u2019s surface temperature serves as a proxy for the local air | ||
47 | temperature. We developed a method to estimate near-surface | 47 | temperature. We developed a method to estimate near-surface | ||
48 | two-dimensional wind fields at centimetre resolution from tracking the | 48 | two-dimensional wind fields at centimetre resolution from tracking the | ||
49 | air temperature pattern on the screens. Wind field estimations are | 49 | air temperature pattern on the screens. Wind field estimations are | ||
50 | validated with near-surface three-dimensional short-path ultrasonic | 50 | validated with near-surface three-dimensional short-path ultrasonic | ||
51 | data. To demonstrate the capabilities of the screen method, we present | 51 | data. To demonstrate the capabilities of the screen method, we present | ||
52 | results from a comprehensive field campaign at an alpine research site | 52 | results from a comprehensive field campaign at an alpine research site | ||
53 | during patchy snow cover conditions. The measurements reveal an | 53 | during patchy snow cover conditions. The measurements reveal an | ||
54 | extremely heterogeneous near-surface atmospheric layer. Vertical | 54 | extremely heterogeneous near-surface atmospheric layer. Vertical | ||
55 | profiles of horizontal and vertical wind speed reflect multiple layers | 55 | profiles of horizontal and vertical wind speed reflect multiple layers | ||
56 | of different static stability within 2m above the surface. A dynamic, | 56 | of different static stability within 2m above the surface. A dynamic, | ||
57 | thin stable internal boundary layer (SIBL) develops above the leading | 57 | thin stable internal boundary layer (SIBL) develops above the leading | ||
58 | edge of snow patches protecting the snow surface from warmer air | 58 | edge of snow patches protecting the snow surface from warmer air | ||
59 | above. During pronounced gusts the warm air from aloft entrains into | 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 | 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 | 61 | snow pack. Measured vertical turbulent sensible heat fluxes are shown | ||
62 | to be consistent with air temperature and wind speed profiles obtained | 62 | to be consistent with air temperature and wind speed profiles obtained | ||
63 | using the screen method and confirm its capabilities to investigate | 63 | using the screen method and confirm its capabilities to investigate | ||
64 | complex in situ near-surface heat exchange processes.\r\nHere you find | 64 | complex in situ near-surface heat exchange processes.\r\nHere you find | ||
65 | the data and the documented code used to create the plots in the | 65 | the data and the documented code used to create the plots in the | ||
66 | publication.", | 66 | publication.", | ||
67 | "num_resources": 3, | 67 | "num_resources": 3, | ||
68 | "num_tags": 8, | 68 | "num_tags": 8, | ||
69 | "organization": { | 69 | "organization": { | ||
70 | "approval_status": "approved", | 70 | "approval_status": "approved", | ||
71 | "created": "2021-08-23T15:25:48.676190", | 71 | "created": "2021-08-23T15:25:48.676190", | ||
72 | "description": "The research group \u00abSnow Hydrology\u00bb | 72 | "description": "The research group \u00abSnow Hydrology\u00bb | ||
73 | investigates snow as a component of the hydrological cycle. In the | 73 | investigates snow as a component of the hydrological cycle. In the | ||
74 | Alps a significant percentage of precipitation comes in the form of | 74 | Alps a significant percentage of precipitation comes in the form of | ||
75 | 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 | ||
76 | runoff from alpine watersheds. Of particular interest for our research | 76 | runoff from alpine watersheds. Of particular interest for our research | ||
77 | is to enhance estimations of snow water resources and subsequent melt | 77 | is to enhance estimations of snow water resources and subsequent melt | ||
78 | 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 | ||
79 | projects and methods. The latest measuring techniques are used to | 79 | projects and methods. The latest measuring techniques are used to | ||
80 | investigate snow distribution patterns in alpine terrain, e.g. laser | 80 | investigate snow distribution patterns in alpine terrain, e.g. laser | ||
81 | scanning or radar technology. We use different types of numerical | 81 | scanning or radar technology. We use different types of numerical | ||
82 | models to calculate snow water resources based on input data from | 82 | models to calculate snow water resources based on input data from | ||
83 | meteorological monitoring networks. These models are being used to | 83 | meteorological monitoring networks. These models are being used to | ||
84 | predict the consequences of climate change on the water balance of | 84 | predict the consequences of climate change on the water balance of | ||
85 | mountain watersheds. The models also constitute a valuable tool for | 85 | mountain watersheds. The models also constitute a valuable tool for | ||
86 | our operational services, such as periodic snow hydrological | 86 | our operational services, such as periodic snow hydrological | ||
87 | bulletins, which contribute to the federal flood prevention and | 87 | bulletins, which contribute to the federal flood prevention and | ||
88 | forecasting system.\r\n\r\nThe research group \u00abSnow | 88 | forecasting system.\r\n\r\nThe research group \u00abSnow | ||
89 | 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 | ||
90 | Davosian research groups and the research unit \u201dMountain | 90 | Davosian research groups and the research unit \u201dMountain | ||
91 | Hydrology and Mass Movements\u201d in Birmensdorf.", | 91 | Hydrology and Mass Movements\u201d in Birmensdorf.", | ||
92 | "id": "d66115d3-c4f9-4f6e-8ff1-5791549e0386", | 92 | "id": "d66115d3-c4f9-4f6e-8ff1-5791549e0386", | ||
93 | "image_url": "", | 93 | "image_url": "", | ||
94 | "is_organization": true, | 94 | "is_organization": true, | ||
95 | "name": "snow-hydrology", | 95 | "name": "snow-hydrology", | ||
96 | "state": "active", | 96 | "state": "active", | ||
97 | "title": "Snow Hydrology", | 97 | "title": "Snow Hydrology", | ||
98 | "type": "organization" | 98 | "type": "organization" | ||
99 | }, | 99 | }, | ||
100 | "owner_org": "d66115d3-c4f9-4f6e-8ff1-5791549e0386", | 100 | "owner_org": "d66115d3-c4f9-4f6e-8ff1-5791549e0386", | ||
101 | "private": false, | 101 | "private": false, | ||
102 | "publication": "{\"publication_year\": \"2022\", \"publisher\": | 102 | "publication": "{\"publication_year\": \"2022\", \"publisher\": | ||
103 | \"EnviDat\"}", | 103 | \"EnviDat\"}", | ||
104 | "publication_state": "published", | 104 | "publication_state": "published", | ||
105 | "related_datasets": "", | 105 | "related_datasets": "", | ||
t | 106 | "related_publications": "A Novel Method to Quantify Near-Surface | t | 106 | "related_publications": "Haugeneder, M., Lehning, M., Reynolds, D. |
107 | Boundary-Layer Dynamics at Ultra-High Spatio-Temporal Resolution; | 107 | et al. A Novel Method to Quantify Near-Surface Boundary-Layer Dynamics | ||
108 | accepted for publication in Boundary-Layer Meteorology", | 108 | at Ultra-High Spatio-Temporal Resolution. Boundary-Layer Meteorol | ||
109 | (2022). https://doi.org/10.1007/s10546-022-00752-3", | ||||
109 | "relationships_as_object": [], | 110 | "relationships_as_object": [], | ||
110 | "relationships_as_subject": [], | 111 | "relationships_as_subject": [], | ||
111 | "resource_type": "dataset", | 112 | "resource_type": "dataset", | ||
112 | "resource_type_general": "dataset", | 113 | "resource_type_general": "dataset", | ||
113 | "resources": [ | 114 | "resources": [ | ||
114 | { | 115 | { | ||
115 | "cache_last_updated": null, | 116 | "cache_last_updated": null, | ||
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117 | "created": "2022-02-24T16:22:51.056409", | 118 | "created": "2022-02-24T16:22:51.056409", | ||
118 | "description": "Data measured with a 3D short-path ultrasonic | 119 | "description": "Data measured with a 3D short-path ultrasonic | ||
119 | anemometer in close vicinity to the screens. Note that the time stamps | 120 | anemometer in close vicinity to the screens. Note that the time stamps | ||
120 | are in local time (GMT+2).", | 121 | are in local time (GMT+2).", | ||
121 | "doi": "", | 122 | "doi": "", | ||
122 | "format": "CSV", | 123 | "format": "CSV", | ||
123 | "hash": "", | 124 | "hash": "", | ||
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147 | "created": "2022-02-24T16:24:45.271824", | 148 | "created": "2022-02-24T16:24:45.271824", | ||
148 | "description": "folder containing the source code for the WEIRD | 149 | "description": "folder containing the source code for the WEIRD | ||
149 | method. Written in JULIA.", | 150 | method. Written in JULIA.", | ||
150 | "doi": "", | 151 | "doi": "", | ||
151 | "format": "*.zip", | 152 | "format": "*.zip", | ||
152 | "hash": "", | 153 | "hash": "", | ||
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176 | "created": "2022-02-24T16:54:09.616767", | 177 | "created": "2022-02-24T16:54:09.616767", | ||
177 | "description": "Sequence of 2700 frames recorded with the | 178 | "description": "Sequence of 2700 frames recorded with the | ||
178 | thermal IR cam. The data is stored as the variable 'irdata' in the .nc | 179 | thermal IR cam. The data is stored as the variable 'irdata' in the .nc | ||
179 | file.", | 180 | file.", | ||
180 | "doi": "", | 181 | "doi": "", | ||
181 | "format": "netcdf4", | 182 | "format": "netcdf4", | ||
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200 | esource/376ff6d3-b4a3-4dc8-b34b-8ba3c568b5cc/download/irdata_per3.nc", | 201 | esource/376ff6d3-b4a3-4dc8-b34b-8ba3c568b5cc/download/irdata_per3.nc", | ||
201 | "url_type": "upload" | 202 | "url_type": "upload" | ||
202 | } | 203 | } | ||
203 | ], | 204 | ], | ||
204 | "spatial": | 205 | "spatial": | ||
205 | e\":\"Point\",\"coordinates\":[9.948184490203857,46.85940286020026]}", | 206 | e\":\"Point\",\"coordinates\":[9.948184490203857,46.85940286020026]}", | ||
206 | "spatial_info": "Switzerland", | 207 | "spatial_info": "Switzerland", | ||
207 | "state": "active", | 208 | "state": "active", | ||
208 | "subtitle": "", | 209 | "subtitle": "", | ||
209 | "tags": [ | 210 | "tags": [ | ||
210 | { | 211 | { | ||
211 | "display_name": "2D TEMPERATURE FIELD", | 212 | "display_name": "2D TEMPERATURE FIELD", | ||
212 | "id": "d55ac0d2-0bc0-46a7-889c-1b926d075511", | 213 | "id": "d55ac0d2-0bc0-46a7-889c-1b926d075511", | ||
213 | "name": "2D TEMPERATURE FIELD", | 214 | "name": "2D TEMPERATURE FIELD", | ||
214 | "state": "active", | 215 | "state": "active", | ||
215 | "vocabulary_id": null | 216 | "vocabulary_id": null | ||
216 | }, | 217 | }, | ||
217 | { | 218 | { | ||
218 | "display_name": "2D WIND FIELD", | 219 | "display_name": "2D WIND FIELD", | ||
219 | "id": "660e5d4d-0c68-4484-a4f2-9d21b9029260", | 220 | "id": "660e5d4d-0c68-4484-a4f2-9d21b9029260", | ||
220 | "name": "2D WIND FIELD", | 221 | "name": "2D WIND FIELD", | ||
221 | "state": "active", | 222 | "state": "active", | ||
222 | "vocabulary_id": null | 223 | "vocabulary_id": null | ||
223 | }, | 224 | }, | ||
224 | { | 225 | { | ||
225 | "display_name": "INFRARED THERMOGRAPHY", | 226 | "display_name": "INFRARED THERMOGRAPHY", | ||
226 | "id": "3c841345-45cd-4a99-9c34-69a891d5ea38", | 227 | "id": "3c841345-45cd-4a99-9c34-69a891d5ea38", | ||
227 | "name": "INFRARED THERMOGRAPHY", | 228 | "name": "INFRARED THERMOGRAPHY", | ||
228 | "state": "active", | 229 | "state": "active", | ||
229 | "vocabulary_id": null | 230 | "vocabulary_id": null | ||
230 | }, | 231 | }, | ||
231 | { | 232 | { | ||
232 | "display_name": "NEAR-SURFACE ATMOSPHERIC LAYER", | 233 | "display_name": "NEAR-SURFACE ATMOSPHERIC LAYER", | ||
233 | "id": "93a597d5-cb9f-43d2-b7ca-dd50a368608b", | 234 | "id": "93a597d5-cb9f-43d2-b7ca-dd50a368608b", | ||
234 | "name": "NEAR-SURFACE ATMOSPHERIC LAYER", | 235 | "name": "NEAR-SURFACE ATMOSPHERIC LAYER", | ||
235 | "state": "active", | 236 | "state": "active", | ||
236 | "vocabulary_id": null | 237 | "vocabulary_id": null | ||
237 | }, | 238 | }, | ||
238 | { | 239 | { | ||
239 | "display_name": "PATCHY SNOW COVER", | 240 | "display_name": "PATCHY SNOW COVER", | ||
240 | "id": "61d8a21a-8ef9-4900-8050-bf3e84c05fc5", | 241 | "id": "61d8a21a-8ef9-4900-8050-bf3e84c05fc5", | ||
241 | "name": "PATCHY SNOW COVER", | 242 | "name": "PATCHY SNOW COVER", | ||
242 | "state": "active", | 243 | "state": "active", | ||
243 | "vocabulary_id": null | 244 | "vocabulary_id": null | ||
244 | }, | 245 | }, | ||
245 | { | 246 | { | ||
246 | "display_name": "SNOW MELT", | 247 | "display_name": "SNOW MELT", | ||
247 | "id": "4452e5c9-c707-4c61-bd1c-28816181a043", | 248 | "id": "4452e5c9-c707-4c61-bd1c-28816181a043", | ||
248 | "name": "SNOW MELT", | 249 | "name": "SNOW MELT", | ||
249 | "state": "active", | 250 | "state": "active", | ||
250 | "vocabulary_id": null | 251 | "vocabulary_id": null | ||
251 | }, | 252 | }, | ||
252 | { | 253 | { | ||
253 | "display_name": "SNOW-ATMOSPHERE INTERACTIONS", | 254 | "display_name": "SNOW-ATMOSPHERE INTERACTIONS", | ||
254 | "id": "9d4df93a-3291-49a2-8c72-565088f48c09", | 255 | "id": "9d4df93a-3291-49a2-8c72-565088f48c09", | ||
255 | "name": "SNOW-ATMOSPHERE INTERACTIONS", | 256 | "name": "SNOW-ATMOSPHERE INTERACTIONS", | ||
256 | "state": "active", | 257 | "state": "active", | ||
257 | "vocabulary_id": null | 258 | "vocabulary_id": null | ||
258 | }, | 259 | }, | ||
259 | { | 260 | { | ||
260 | "display_name": "SURFACE HEAT EXCHANGE", | 261 | "display_name": "SURFACE HEAT EXCHANGE", | ||
261 | "id": "cb61d6bd-bf4d-4fd6-a8e2-8dbbbd90d418", | 262 | "id": "cb61d6bd-bf4d-4fd6-a8e2-8dbbbd90d418", | ||
262 | "name": "SURFACE HEAT EXCHANGE", | 263 | "name": "SURFACE HEAT EXCHANGE", | ||
263 | "state": "active", | 264 | "state": "active", | ||
264 | "vocabulary_id": null | 265 | "vocabulary_id": null | ||
265 | } | 266 | } | ||
266 | ], | 267 | ], | ||
267 | "title": "Quantifying Surface Heat Exchange over Heterogeneous Land | 268 | "title": "Quantifying Surface Heat Exchange over Heterogeneous Land | ||
268 | Surfaces at Ultra-High Spatio-Temporal Resolution", | 269 | Surfaces at Ultra-High Spatio-Temporal Resolution", | ||
269 | "type": "dataset", | 270 | "type": "dataset", | ||
270 | "url": null, | 271 | "url": null, | ||
271 | "version": "1.0" | 272 | "version": "1.0" | ||
272 | } | 273 | } |