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| Type: | Resource | |
| Storage: | The size of this resource is 1.6 MB | |
| Created: | Sep 07, 2022 at 7 p.m. (UTC) | |
| Last updated: | Sep 07, 2022 at 7:59 p.m. (UTC) (Metadata update) | |
| Published date: | Sep 07, 2022 at 7:59 p.m. (UTC) | |
| DOI: | 10.4211/hs.143291acae574aaeb3b9acbbd6ca118c | |
| Citation: | See how to cite this resource |
| Sharing Status: | Published |
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| Views: | 1535 |
| Downloads: | 10 |
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| Comments: | No comments (yet) |
Abstract
Raw Electrical Resistivity Tomography data, Seismic Refraction first arrival times, top boundary condition forcing data, Hydra sensor data, and groundwater well data for a forested mountainous hillslope in the NoName zero-order catchment, Snowy Range, Wyoming, U.S.A. used for a coupled hydrogeophysical inversion study.
Subject Keywords
Coverage
Spatial
Temporal
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Content
Credits
Funding Agencies
This resource was created using funding from the following sources:
| Agency Name | Award Title | Award Number |
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| NSF | Subsurface Structure and Flow Regime for Rocky Mountain Hillslopes with Different Geologies | 1818550 |
Contributors
People or Organizations that contributed technically, materially, financially, or provided general support for the creation of the resource's content but are not considered authors.
| Name | Organization | Address | Phone | Author Identifiers |
|---|---|---|---|---|
| Mark S Pleasants | University of Wyoming | Wyoming, US | ORCID | |
| Andrew Parsekian | University of Wyoming | Wyoming, US | ||
| Matt Covalt |
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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