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| Created: | Nov 19, 2019 at 6:47 a.m. (UTC) | |
| Last updated: | Nov 21, 2019 at 8:07 p.m. (UTC) | |
| Citation: | See how to cite this resource | |
| Content types: | Single File Content |
| Sharing Status: | Public |
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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
Subject Keywords
Coverage
Spatial
Temporal
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Content
Additional Metadata
| Name | Value |
|---|---|
| czos | Shale Hills |
| czo_id | 5285 |
| citation | The following acknowledgment should accompany any publication or citation of these data: Logistical support and/or data were provided by the NSF-supported Susquehanna Shale Hills Critical Zone Observatory. |
| keywords | streambed temperature, seepage rate |
| subtitle | Level 1 - Quality Controlled Data |
| variables | TmStamp (YYYY-MM-DD hh:mm:ss), CZ_20, CZ_21, CZ_35, CZ_36, CZ_22, CZ_23, CZ_24, CZ_25, CZ_26, CZ_27, CZ_28, CZ_29 |
| disciplines | Hydrology |
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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