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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
ReadMe.md
SSHCZO -- Groundwater Temperatures, Stream Water Temperatures -- Shale Hills -- (2015-2016)
OVERVIEW
Description/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
Creator/Author
Russo, Tess|Kim, Hyojin
CZOs
Shale Hills
Contact
Dr. Tess A. Russo – Assistant Professor, Department of Geosciences, 310 Deike Building, Pennsylvania State University, University Park, PA 16802 russo@psu.edu (814)865-7389
Subtitle
Level 1 - Quality Controlled Data
SUBJECTS
Disciplines
Hydrology
Topics
Groundwater Temperatures|Stream Water Temperatures
Keywords
streambed temperature|seepage rate
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
Variables ODM2
Temperature|Water temperature|Groundwater temperature
TEMPORAL
Date Start
2015-07-02
Date End
2016-07-26
SPATIAL
Field Areas
Susquehanna Shale Hills Critical Zone Observatory
Location
Shale Hills
North latitude
40.7116043893
South latitude
40.6096426283
West longitude
-77.97987827760001
East longitude
-77.86579982239999
REFERENCE
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.
CZO ID
5285
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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