Changes
On April 4, 2023 at 9:39:04 AM UTC, Administrator:
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Added the following fields to resource Alpine3D output Dischma in Influence of slope-scale snowmelt on catchment response simulated with the Alpine3D model
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resource_size with value
publication_state with value
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Changed value of field
restricted
of resource Alpine3D output Dischma to{"allowed_users": "", "level": "public", "shared_secret": ""}
(previously{"allowed_users": "", "level": "same_organization"}
) in Influence of slope-scale snowmelt on catchment response simulated with the Alpine3D model
f | 1 | { | f | 1 | { |
2 | "author": "[{\"affiliation\": \"EPFL\", \"affiliation_02\": \"\", | 2 | "author": "[{\"affiliation\": \"EPFL\", \"affiliation_02\": \"\", | ||
3 | \"affiliation_03\": \"\", \"email\": | 3 | \"affiliation_03\": \"\", \"email\": | ||
4 | \"tristan.brauchli@alumni.epfl.ch\", \"given_name\": \"Tristan\", | 4 | \"tristan.brauchli@alumni.epfl.ch\", \"given_name\": \"Tristan\", | ||
5 | \"identifier\": \"0000-0003-3332-4995\", \"name\": \"Brauchli\"}]", | 5 | \"identifier\": \"0000-0003-3332-4995\", \"name\": \"Brauchli\"}]", | ||
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8 | "date": "[{\"date\": \"2017-12-07\", \"date_type\": \"created\", | 8 | "date": "[{\"date\": \"2017-12-07\", \"date_type\": \"created\", | ||
9 | \"end_date\": \"\"}]", | 9 | \"end_date\": \"\"}]", | ||
10 | "doi": "10.16904/envidat.24", | 10 | "doi": "10.16904/envidat.24", | ||
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24 | "license_title": "WSL Data Policy", | 24 | "license_title": "WSL Data Policy", | ||
25 | "license_url": | 25 | "license_url": | ||
26 | ps://www.wsl.ch/en/about-wsl/programmes-and-initiatives/envidat.html", | 26 | ps://www.wsl.ch/en/about-wsl/programmes-and-initiatives/envidat.html", | ||
27 | "maintainer": "{\"affiliation\": \"CREALP\", \"email\": | 27 | "maintainer": "{\"affiliation\": \"CREALP\", \"email\": | ||
28 | \"tristan.brauchli@crealp.vs.ch\", \"given_name\": \"Tristan\", | 28 | \"tristan.brauchli@crealp.vs.ch\", \"given_name\": \"Tristan\", | ||
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30 | "maintainer_email": null, | 30 | "maintainer_email": null, | ||
31 | "metadata_created": "2017-10-26T14:33:36.796092", | 31 | "metadata_created": "2017-10-26T14:33:36.796092", | ||
n | 32 | "metadata_modified": "2022-05-31T13:45:58.069717", | n | 32 | "metadata_modified": "2023-04-04T09:39:04.838254", |
33 | "name": "10-16904-envidat-24", | 33 | "name": "10-16904-envidat-24", | ||
34 | "notes": "# Abstract\r\nSnow and hydrological modeling in alpine | 34 | "notes": "# Abstract\r\nSnow and hydrological modeling in alpine | ||
35 | environments remains a challenge because of the complexity of the | 35 | environments remains a challenge because of the complexity of the | ||
36 | processes complexity affecting the mass and energy balance. This study | 36 | processes complexity affecting the mass and energy balance. This study | ||
37 | examines the influence of snowmelt on the hydrological response of a | 37 | examines the influence of snowmelt on the hydrological response of a | ||
38 | high-alpine catchment of 43.2 km2 in the Swiss Alps during the water | 38 | high-alpine catchment of 43.2 km2 in the Swiss Alps during the water | ||
39 | year 2014-2015. Based on recent advances in Alpine3D, we examine how | 39 | year 2014-2015. Based on recent advances in Alpine3D, we examine how | ||
40 | modeled snow distributions, and modeled liquid water transport within | 40 | modeled snow distributions, and modeled liquid water transport within | ||
41 | the snowpack influence runoff dynamics. By combining these results | 41 | the snowpack influence runoff dynamics. By combining these results | ||
42 | with multi-scale field data (snow lysimeter data, distributed snow | 42 | with multi-scale field data (snow lysimeter data, distributed snow | ||
43 | depths and streamflow), we demonstrate the added value of a more | 43 | depths and streamflow), we demonstrate the added value of a more | ||
44 | realistic representation of snow distribution at the onset of melt | 44 | realistic representation of snow distribution at the onset of melt | ||
45 | season. At the site scale, snowpack runoff is well simulated when the | 45 | season. At the site scale, snowpack runoff is well simulated when the | ||
46 | snowpack mass balance errors are corrected (R2 = 0.95 vs. R2 = 0.61). | 46 | snowpack mass balance errors are corrected (R2 = 0.95 vs. R2 = 0.61). | ||
47 | At the sub-basin scale, a more heterogeneous snowpack leads to a more | 47 | At the sub-basin scale, a more heterogeneous snowpack leads to a more | ||
48 | rapid runoff pulse originated in the shallower areas while an extended | 48 | rapid runoff pulse originated in the shallower areas while an extended | ||
49 | melting period (by more than a month) is caused by slower snowmelt | 49 | melting period (by more than a month) is caused by slower snowmelt | ||
50 | from deeper areas. This result is a marked improvement over results | 50 | from deeper areas. This result is a marked improvement over results | ||
51 | obtained using a less heterogeneous snow distribution (i.e., | 51 | obtained using a less heterogeneous snow distribution (i.e., | ||
52 | traditional precipitation interpolation method). Catchment | 52 | traditional precipitation interpolation method). Catchment | ||
53 | hydrological response is also improved by the more realistic | 53 | hydrological response is also improved by the more realistic | ||
54 | representation of snowpack heterogeneity (Nash coefficient of 0.85 vs. | 54 | representation of snowpack heterogeneity (Nash coefficient of 0.85 vs. | ||
55 | 0.74), even though the calibration process smoothens out the | 55 | 0.74), even though the calibration process smoothens out the | ||
56 | differences. \r\nThe added value of a more complex liquid water | 56 | differences. \r\nThe added value of a more complex liquid water | ||
57 | transport scheme is obvious at the site scale but decreases at the | 57 | transport scheme is obvious at the site scale but decreases at the | ||
58 | sub-basin and basin scales. Our results highlight not only the | 58 | sub-basin and basin scales. Our results highlight not only the | ||
59 | importance but also the difficulty of getting a realistic snowpack | 59 | importance but also the difficulty of getting a realistic snowpack | ||
60 | distribution even in a well-instrumented area and present a model | 60 | distribution even in a well-instrumented area and present a model | ||
61 | validation from multi-scale experimental datasets.", | 61 | validation from multi-scale experimental datasets.", | ||
62 | "num_resources": 1, | 62 | "num_resources": 1, | ||
63 | "num_tags": 5, | 63 | "num_tags": 5, | ||
64 | "organization": { | 64 | "organization": { | ||
65 | "approval_status": "approved", | 65 | "approval_status": "approved", | ||
66 | "created": "2016-11-17T12:24:20.447699", | 66 | "created": "2016-11-17T12:24:20.447699", | ||
67 | "description": "CRYOS is the EPFL laboratory of the WSL/SLF - EPFL | 67 | "description": "CRYOS is the EPFL laboratory of the WSL/SLF - EPFL | ||
68 | joint appointment for Prof. Michael Lehning. At his WSL side, Prof. | 68 | joint appointment for Prof. Michael Lehning. At his WSL side, Prof. | ||
69 | Michael Lehning is head of the research unit \"Snow and Permafrost\" | 69 | Michael Lehning is head of the research unit \"Snow and Permafrost\" | ||
70 | at SLF in Davos.\r\n \r\n###General Mission\r\nThe laboratory of | 70 | at SLF in Davos.\r\n \r\n###General Mission\r\nThe laboratory of | ||
71 | cryospheric sciences investigates the processes that shape snow and | 71 | cryospheric sciences investigates the processes that shape snow and | ||
72 | ice in mountains and polar regions. In particular, snow cover | 72 | ice in mountains and polar regions. In particular, snow cover | ||
73 | processes, snow-atmosphere interactions and mountain hydrology are in | 73 | processes, snow-atmosphere interactions and mountain hydrology are in | ||
74 | the focus of current research. This includes a strive for deeper | 74 | the focus of current research. This includes a strive for deeper | ||
75 | understanding of the complicated mass and energy exchange processes | 75 | understanding of the complicated mass and energy exchange processes | ||
76 | within, above and below a snow cover but also predictions of future | 76 | within, above and below a snow cover but also predictions of future | ||
77 | snow and ice in mountains and high latitudes. A newer work area is the | 77 | snow and ice in mountains and high latitudes. A newer work area is the | ||
78 | risk management and optimization in the field of renewable energy | 78 | risk management and optimization in the field of renewable energy | ||
79 | production based on our detailed understanding of water, wind and | 79 | production based on our detailed understanding of water, wind and | ||
80 | radiation processes in mountains.\r\n\r\nMore information: | 80 | radiation processes in mountains.\r\n\r\nMore information: | ||
81 | http://cryos.epfl.ch/", | 81 | http://cryos.epfl.ch/", | ||
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83 | "image_url": "2019-03-26-151807.125593CRYOSLogoFinal.jpg", | 83 | "image_url": "2019-03-26-151807.125593CRYOSLogoFinal.jpg", | ||
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85 | "name": "cryos", | 85 | "name": "cryos", | ||
86 | "state": "active", | 86 | "state": "active", | ||
87 | "title": "CRYOS", | 87 | "title": "CRYOS", | ||
88 | "type": "organization" | 88 | "type": "organization" | ||
89 | }, | 89 | }, | ||
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92 | "publication": "{\"publication_year\": \"2017\", \"publisher\": | 92 | "publication": "{\"publication_year\": \"2017\", \"publisher\": | ||
93 | \"EnviDat\"}", | 93 | \"EnviDat\"}", | ||
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175 | } | 178 | } | ||
176 | ], | 179 | ], | ||
177 | "title": "Influence of slope-scale snowmelt on catchment response | 180 | "title": "Influence of slope-scale snowmelt on catchment response | ||
178 | simulated with the Alpine3D model", | 181 | simulated with the Alpine3D model", | ||
179 | "type": "dataset", | 182 | "type": "dataset", | ||
180 | "url": null, | 183 | "url": null, | ||
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