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Data files for "Quantifying underflow in the river corridor of a headwater mountain stream"

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Type:	Resource
Storage:	The size of this resource is 13.6 MB
Created:	Feb 09, 2025 at 6:55 p.m. (UTC)
Last updated:	Jun 10, 2025 at 1:14 p.m. (UTC)
Published date:	Jun 10, 2025 at 1:14 p.m. (UTC)
DOI:	10.4211/hs.9be2a7c3bc19467fbfac7aa99ad61790
Citation:	See how to cite this resource

Sharing Status:	Published
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Abstract

Underflow, or the downstream flow of water in the shallow subsurface parallel to a stream, is important for the transport of water and solutes through river corridors and is driven by hydrostatic controls such as hydraulic conductivity and volumetric subsurface capacity. However, these controls rely on point measurements and thus the actual volume of underflow is difficult to quantify. In this study, we take advantage of bedrock outcrops paired with reach and segment scale water balances to quantify underflow. From the water balances, we learn that reach and segment scale balances can have differing interpretations due to the existence of underflow. Additionally, we suggest that fluxes, geometries, and timescales are important for fully understanding the role of underflow and present a high-level review of methods that can be used to address all three components to better quantify underflow in future studies.

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:

WGS 84 EPSG:4326

Coordinate Units:

Decimal degrees

Place/Area Name:

H. J. Andrews Experimental Forest

Longitude

-122.2602°

Latitude

44.2076°

Temporal

Start Date:
End Date:

Content

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How to Cite

Becker, P., A. S. Ward, S. P. Herzog, S. Wondzell (2025). Data files for "Quantifying underflow in the river corridor of a headwater mountain stream", HydroShare, https://doi.org/10.4211/hs.9be2a7c3bc19467fbfac7aa99ad61790

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

http://creativecommons.org/licenses/by/4.0/

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