Changes
On June 19, 2023 at 9:06:34 PM UTC, Michael Haugeneder:
-
Updated description of resource kaijo.zip in Turbulence in The Strongly Heterogeneous Near-Surface Boundary Layer over Patchy Snow from
IR-data that is visualized in the video
toRaw eddy covariance data from the short-path ultrasonic ("Kaijo") at 0.3m above the snow
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34 | "notes": "Data and code for the publication. The data is raw data. | 34 | "notes": "Data and code for the publication. The data is raw data. | ||
35 | Processed data can be obtained upon request.", | 35 | Processed data can be obtained upon request.", | ||
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41 | "description": "The research group \u00abSnow Hydrology\u00bb | 41 | "description": "The research group \u00abSnow Hydrology\u00bb | ||
42 | investigates snow as a component of the hydrological cycle. In the | 42 | investigates snow as a component of the hydrological cycle. In the | ||
43 | Alps a significant percentage of precipitation comes in the form of | 43 | Alps a significant percentage of precipitation comes in the form of | ||
44 | snow. The timing of snow melt thus influences the annual dynamics of | 44 | snow. The timing of snow melt thus influences the annual dynamics of | ||
45 | runoff from alpine watersheds. Of particular interest for our research | 45 | runoff from alpine watersheds. Of particular interest for our research | ||
46 | is to enhance estimations of snow water resources and subsequent melt | 46 | is to enhance estimations of snow water resources and subsequent melt | ||
47 | water discharge.\r\n\r\nThe research group covers a broad range of | 47 | water discharge.\r\n\r\nThe research group covers a broad range of | ||
48 | projects and methods. The latest measuring techniques are used to | 48 | projects and methods. The latest measuring techniques are used to | ||
49 | investigate snow distribution patterns in alpine terrain, e.g. laser | 49 | investigate snow distribution patterns in alpine terrain, e.g. laser | ||
50 | scanning or radar technology. We use different types of numerical | 50 | scanning or radar technology. We use different types of numerical | ||
51 | models to calculate snow water resources based on input data from | 51 | models to calculate snow water resources based on input data from | ||
52 | meteorological monitoring networks. These models are being used to | 52 | meteorological monitoring networks. These models are being used to | ||
53 | predict the consequences of climate change on the water balance of | 53 | predict the consequences of climate change on the water balance of | ||
54 | mountain watersheds. The models also constitute a valuable tool for | 54 | mountain watersheds. The models also constitute a valuable tool for | ||
55 | our operational services, such as periodic snow hydrological | 55 | our operational services, such as periodic snow hydrological | ||
56 | bulletins, which contribute to the federal flood prevention and | 56 | bulletins, which contribute to the federal flood prevention and | ||
57 | forecasting system.\r\n\r\nThe research group \u00abSnow | 57 | forecasting system.\r\n\r\nThe research group \u00abSnow | ||
58 | Hydrology\u00bb is based in Davos and ensures the link between other | 58 | Hydrology\u00bb is based in Davos and ensures the link between other | ||
59 | Davosian research groups and the research unit \u201dMountain | 59 | Davosian research groups and the research unit \u201dMountain | ||
60 | Hydrology and Mass Movements\u201d in Birmensdorf.", | 60 | Hydrology and Mass Movements\u201d in Birmensdorf.", | ||
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