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SSHCZO -- Streamflow / Discharge, Air Temperature, Stream Water Temperatures -- Garner Run Outlet -- (2014-2016)
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Created: | Nov 19, 2019 at 6:48 a.m. | |
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Abstract
Surface water discharge data for Garner Run stream (Sheet 1). Stage data was measured every 10 to15 min and a rating curve was built with manual measurements from a Parshall Flume. All data contributes to the goals of hypothesis six (H6), which focuses on concentration-discharge relationships spatially and temporally. Data spans from October 2014 to March 2016.
Discharge measurements were collected using a 9 inch flume monthly to bi-weekly and used to build a rating curve.
Stage was measured every 15 min in a pool ~20 m upstream of the flume using a HOBO pressure transducer. Surveys were conducted to compute elevation difference between Parshall Flume and HOBO pressure transducer. Discharge was calculated for each elevation compensated stage measurement based upon the rating curve.
Date Range Comments: Discharge values are computed based on rating developed with manual measurements.
Subject Keywords
Coverage
Spatial
Temporal
Start Date: | |
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End Date: |
Content
ReadMe.md
SSHCZO -- Streamflow / Discharge, Air Temperature, Stream Water Temperatures -- Garner Run Outlet -- (2014-2016)
OVERVIEW
Description/Abstract
Surface water discharge data for Garner Run stream (Sheet 1). Stage data was measured every 10 to15 min and a rating curve was built with manual measurements from a Parshall Flume. All data contributes to the goals of hypothesis six (H6), which focuses on concentration-discharge relationships spatially and temporally. Data spans from October 2014 to March 2016. Discharge measurements were collected using a 9 inch flume monthly to bi-weekly and used to build a rating curve.
Stage was measured every 15 min in a pool ~20 m upstream of the flume using a HOBO pressure transducer. Surveys were conducted to compute elevation difference between Parshall Flume and HOBO pressure transducer. Discharge was calculated for each elevation compensated stage measurement based upon the rating curve.
Creator/Author
Russo, Tess|Hoagland, Beth
CZOs
Shale Hills
Contact
Dr. Tess Russo, – Assistant Professor, Department of Geosciences, 310 Deike Building, Pennsylvania State University, University Park, PA 16802, russo@psu.edu, (814)865-7389 Beth Hoagland, neh137@psu.edu, Graduate Student, 502-432-0755
Subtitle
Level 2 - Derived Products
SUBJECTS
Disciplines
Hydrology
Topics
Streamflow / Discharge|Air Temperature|Stream Water Temperatures
Keywords
Hydrology|Stream discharge|rating curve
Variables
Time Stamp|baro|air_t|abs_press|w_temp|depth_m|stage_cm|stage_diff|discharge
Variables ODM2
Pressure, absolute|Temperature|Barometric pressure|Sensor depth|Discharge|Water depth
TEMPORAL
Date Start
2014-10-17
Date End
2016-03-08
Date Range Comments
Discharge values are computed based on rating developed with manual measurements.
SPATIAL
Field Areas
Garner Run - Sandstone Forested
Location
Garner Run Outlet
North latitude
40.692454
South latitude
40.692454
West longitude
-77.92773100000001
East longitude
-77.92773100000001
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
5324
Additional Metadata
Name | Value |
---|---|
czos | Shale Hills |
czo_id | 5324 |
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 | Hydrology, Stream discharge, rating curve |
subtitle | Level 2 - Derived Products |
variables | Time Stamp, baro, air_t, abs_press, w_temp, depth_m, stage_cm, stage_diff, discharge |
disciplines | Hydrology |
date_range_comments | Discharge values are computed based on rating developed with manual measurements. |
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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