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| Authors: |  | |
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| Owners: |  | This resource does not have an owner who is an active HydroShare user. Contact CUAHSI (help@cuahsi.org) for information on this resource. | 
| Type: | Resource | |
| Storage: | The size of this resource is 886.5 MB | |
| Created: | Jan 26, 2022 at 1:56 p.m. (UTC) | |
| Last updated: | Feb 18, 2022 at 5:47 p.m. (UTC) (Metadata update) | |
| Published date: | Feb 18, 2022 at 5:47 p.m. (UTC) | |
| DOI: | 10.4211/hs.4b940b8593a4416e954a47bbbc58c568 | |
| Citation: | See how to cite this resource | 
| Sharing Status: | Published | 
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| Views: | 2779 | 
| Downloads: | 13 | 
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| Comments: | No comments (yet) | 
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.
Subject Keywords
Coverage
Spatial
Temporal
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Content
Related Resources
| 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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