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Type: | Resource | |
Storage: | The size of this resource is 886.5 MB | |
Created: | Jan 26, 2022 at 1:56 p.m. | |
Last updated: | Feb 18, 2022 at 5:47 p.m. (Metadata update) | |
Published date: | Feb 18, 2022 at 5:47 p.m. | |
DOI: | 10.4211/hs.4b940b8593a4416e954a47bbbc58c568 | |
Citation: | See how to cite this resource |
Sharing Status: | Published |
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Views: | 1598 |
Downloads: | 9 |
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Abstract
April 1 SWE is used across the western USA as a predictor of spring streamflow. Here, we use SNODAS data (https://nsidc.org/data/g02158) to map 10, 25, 50, 75, and 90th percentiles of April 1 SWE across the contiguous USA. This data is part of the data supplement for Lapides et al., 20XX.
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The content of this resource is derived from | https://nsidc.org/data/g02158 |
This resource is referenced by | Lapides, DA, Hahm, WJ, Rempe, DM, Dralle, DN. "Root zone storage deficits mediate the generation of streamflow from snowmelt". In Preparation. |
How to Cite
This resource is shared under the Creative Commons Attribution-NoCommercial-ShareAlike CC BY-NC-SA.
http://creativecommons.org/licenses/by-nc-sa/4.0/
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