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Dataset for 'Towards the closure of mass and energy budgets at the watershed scale: the Wahoo Creek Case' article
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| Type: | Resource | |
| Storage: | The size of this resource is 1.1 MB | |
| Created: | Oct 26, 2021 at 12:25 p.m. (UTC) | |
| Last updated: | Nov 10, 2021 at 6:07 p.m. (UTC) (Metadata update) | |
| Published date: | Nov 10, 2021 at 6:07 p.m. (UTC) | |
| DOI: | 10.4211/hs.89478d0a27c646e3b6a92c2483c0174d | |
| Citation: | See how to cite this resource | |
| Content types: | Geographic Feature Content |
| Sharing Status: | Published |
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| Views: | 2382 |
| Downloads: | 52 |
| +1 Votes: | Be the first one to this. |
| Comments: | No comments (yet) |
Abstract
This dataset is part of the article entitled 'Towards the closure of mass and energy budgets at the watershed scale: the Wahoo Creek Case' from Hoeltgebaum and Dias, submitted to the Water Resources Research journal in November 2021.
This dataset contains processed data from 6 rain gauges, 10 snowboard measurement points, 2 discharge gages, measurements of latent heat flux and soil moisture (at 4 depths) for 3 AmeriFlux stations, and remote sensing data over 2 basins, such as NDVI, land surface radiation, and soil moisture. Estimates of storage and evapotranspiration over the basins are also included. More detail on the processing of data and methods of calculations can be seen in the article 'Towards the closure of mass and energy budgets at the watershed scale: the Wahoo Creek Case'.
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Related Resources
| The content of this resource is derived from | NCDC - National Climatic Data Center |
| The content of this resource is derived from | AmeriFlux |
| The content of this resource is derived from | USGS - United States Geological Survey |
| The content of this resource is derived from | ORNL DAAC - Distributed Active Archive Center |
| The content of this resource is derived from | NASA NSIDC - National Snow and Ice Data Center |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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