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Supporting data for "Active layer groundwater flow: the interrelated effects of stratigraphy, thaw, and topography"


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Type: Resource
Storage: The size of this resource is 589.5 KB
Created: Jul 08, 2019 at 4:49 p.m.
Last updated: Jul 31, 2019 at 6:48 p.m.
DOI: 10.4211/hs.938ea95c2fe3498a9a893cf4e63f8b3b
Citation: See how to cite this resource
Sharing Status: Published
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Abstract

Data pertaining to the following publication:

"O'Connor, M., Cardenas, M., Neilson, B., Nicholaides, K., and Kling, G. (2019). Active layer groundwater flow: the interrelated effects of stratigraphy, thaw, and topography. Water Resources Research, DOI:10.1029/2018WR024636"

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Imnavait Creek Watershed
North Latitude
68.6150°
East Longitude
-149.2900°
South Latitude
68.6050°
West Longitude
-149.3250°

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
National Science Foundation ARC 1204220
National Science Foundation DEB 1026843
National Science Foundation OPP 1107593
National Science Foundation DEB 0639805
National Science Foundation PLR 1504006

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
Bethany Neilson Utah State University UT, US
M. Bayani Cardenas University of Texas at Austin
Kindra Nicholaides
George W. Kling University of Michigan

How to Cite

O'Connor, M. T. (2019). Supporting data for "Active layer groundwater flow: the interrelated effects of stratigraphy, thaw, and topography", HydroShare, https://doi.org/10.4211/hs.938ea95c2fe3498a9a893cf4e63f8b3b

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

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

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