SSHCZO -- Groundwater Temperatures, Stream Water Temperatures -- Shale Hills -- (2015-2016)


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Owners: CZO Shale-HillsCZO National
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Created: Nov 19, 2019 at 6:47 a.m.
Last updated: Nov 21, 2019 at 8:07 p.m.
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Abstract

Streambed water temperature was monitored at 6 streambed piezometers at the Shale Hills Critical Zone Observatory since May 2015 at a 15-min interval. These are RAW data to estimate the groundwater seepage rates. Each piezometer has two thermal probes at about vertically 15-20cm apart. The daily seepage rate is inferred from the amplitude and phases differences between the two streambed temperature measurements (Hatch et al., 2006). The daily seepage rate at each streambed piezometer point is inferred from the amplitude and phase differences between a pair of water temperature measurements. The detailed method is available in Hatch et al. (2006). Matlab codes for the seepage rate computation are available (contact Tess Russo at russo@psu.edu)

Hatch C.E., Andrew T. Fisher, Revenaugh J. S., Constantz J., and Ruehl C. (2006) Quantifying surface water-groundwater interactions using time series analysis of streambed thermal records: Method development. Water Resources Research, 42, W10410. doi:10.1029/2005WR004787

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Susquehanna Shale Hills Critical Zone Observatory, Shale Hills
North Latitude
40.7116°
East Longitude
-77.8658°
South Latitude
40.6096°
West Longitude
-77.9799°

Temporal

Start Date: 07/02/2015
End Date: 07/26/2016
Leaflet Map data © OpenStreetMap contributors

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How to Cite

Russo, T., H. Kim (2019). SSHCZO -- Groundwater Temperatures, Stream Water Temperatures -- Shale Hills -- (2015-2016), HydroShare, http://www.hydroshare.org/resource/a868f9188e36478db40c02efab920281

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

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

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