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Coupled Hydrogeophysical Inversion Study


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Created: Sep 07, 2022 at 7 p.m.
Last updated: Sep 07, 2022 at 7:59 p.m. (Metadata update)
Published date: Sep 07, 2022 at 7:59 p.m.
DOI: 10.4211/hs.143291acae574aaeb3b9acbbd6ca118c
Citation: See how to cite this resource
Sharing Status: Published
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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

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
NoName zero-order catchment, Snowy Range, Wyoming, U.S.A.
North Latitude
41.3475°
East Longitude
-106.2103°
South Latitude
41.3442°
West Longitude
-106.2167°

Temporal

Start Date:
End Date:

Content

Credits

Funding Agencies

This resource was created using funding from the following sources:
Agency Name Award Title Award Number
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

Kelleners, T. (2022). Coupled Hydrogeophysical Inversion Study, HydroShare, https://doi.org/10.4211/hs.143291acae574aaeb3b9acbbd6ca118c

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/
CC-BY

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