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SSHCZO -- Streamflow / Discharge, Air Temperature, Stream Water Temperatures -- Garner Run Outlet -- (2014-2016)
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Type: | Resource | |
Storage: | The size of this resource is 321 bytes | |
Created: | Nov 19, 2019 at 6:48 a.m. | |
Last updated: | Nov 21, 2019 at 8:07 p.m. | |
Citation: | See how to cite this resource | |
Content types: | Single File Content |
Sharing Status: | Public |
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Views: | 1949 |
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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
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Content
Additional Metadata
Name | Value |
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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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