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SSHCZO -- Streamflow / Discharge, Groundwater Temperatures, Electrical Conductivity -- Shale Hills -- (2015-2018)
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Abstract
A 2.5 foot fiberglass H-flume with 7’ 6” 3D approach section, 10” diameter stilling well, and dual scale staff gauge is located at the outlet of the stream Shale Hills Susquehanna Critical Zone Observatory Stream (40.664848, -77.907245, elevation 259.08 m) is used to monitor stream discharge accurately during high and low flows. Water depths are measured using a Decagon CTD-10 sensor recording in one-minute intervals, integrated to 10 minute values and converted to discharge using a rating curve developed by Open Channel Flow for the specific flume dimensions. An offset of 54 mm has been entered in the Campbell Science CR1000 data-logger program to account for the difference between the pressure sensor spacing and distance from bottom of stilling well to flume.
Date Range Comments: 2015 2015-11-03 to 2015-11-19: no flow and building up ice 2015-11-20 to 2015-12-01: ice 2016 2016-12-15 : ice 2016-12-20 to 2016-12-25 : ice 2016-01-05 to 2016-01-08: ice 2016-01-09 to 2016-01-10: ice 2016-01-13 to 2016-01-14: ice 2016-01-18 to 2016-01-31: ice 2016-02-11 to 2016-02-21: ice 2016-04-20: debris buildup 2016-06-10 to 2016-11-30: no flow – summer was dry 2017 2017-01-07 to 2017-01-12: ice 2017-05-03: debris buildup 2017-05-17 to 2017-05-29: debris buildup 2017-06-08 to 2017-06-16: debris buildup 2017-06-29 to 2017-07-11: debris buildup 2017-10-17: erroneous data spikes 2017-11-20 to 2017-11-21: ice 2017-12-13 to 2018-01-01: ice
Subject Keywords
Coverage
Spatial
Temporal
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Content
ReadMe.md
SSHCZO -- Streamflow / Discharge, Groundwater Temperatures, Electrical Conductivity -- Shale Hills -- (2015-2018)
OVERVIEW
Description/Abstract
A 2.5 foot fiberglass H-flume with 7’ 6” 3D approach section, 10” diameter stilling well, and dual scale staff gauge is located at the outlet of the stream Shale Hills Susquehanna Critical Zone Observatory Stream (40.664848, -77.907245, elevation 259.08 m) is used to monitor stream discharge accurately during high and low flows. Water depths are measured using a Decagon CTD-10 sensor recording in one-minute intervals, integrated to 10 minute values and converted to discharge using a rating curve developed by Open Channel Flow for the specific flume dimensions. An offset of 54 mm has been entered in the Campbell Science CR1000 data-logger program to account for the difference between the pressure sensor spacing and distance from bottom of stilling well to flume.
Creator/Author
Brantley, Susan L.
CZOs
Shale Hills
Contact
Dr. Susan Brantley, Professor of Geosciences, The Pennsylvania State University, 2217 Earth and Environmental Systems Institute, University Park, PA, 16802, 814.865.1619, sxb7@psu.edu.
Subtitle
Shale Hills Stream Discharge, Water Temperature, and Conductivity Data - Level 1
SUBJECTS
Disciplines
Hydrology
Topics
Streamflow / Discharge|Groundwater Temperatures|Electrical Conductivity
Keywords
hydrology|stream flow|water|discharge|stage|conductivity|specific conductivity|stream water temperature
Variables
TmStamp_UTC|Stage_m|Water_TempC|Cond (conductivity)|spc_cond (specific conductivity)|dischg_m3s_m3s (discharge in cubic meters per second)|dischg_cfs (discharge in cubic feet per second)
Variables ODM2
Electrical conductivity|Discharge|Specific conductance|Water depth|Temperature
TEMPORAL
Date Start
2015-10-22
Date End
2018-08-07
Date Range Comments
2015 2015-11-03 to 2015-11-19: no flow and building up ice 2015-11-20 to 2015-12-01: ice 2016 2016-12-15 : ice 2016-12-20 to 2016-12-25 : ice 2016-01-05 to 2016-01-08: ice 2016-01-09 to 2016-01-10: ice 2016-01-13 to 2016-01-14: ice 2016-01-18 to 2016-01-31: ice 2016-02-11 to 2016-02-21: ice 2016-04-20: debris buildup 2016-06-10 to 2016-11-30: no flow – summer was dry 2017 2017-01-07 to 2017-01-12: ice 2017-05-03: debris buildup 2017-05-17 to 2017-05-29: debris buildup 2017-06-08 to 2017-06-16: debris buildup 2017-06-29 to 2017-07-11: debris buildup 2017-10-17: erroneous data spikes 2017-11-20 to 2017-11-21: ice 2017-12-13 to 2018-01-01: ice
SPATIAL
Field Areas
Susquehanna Shale Hills Critical Zone Observatory
Location
Shale Hills
North latitude
40.664848799999994
South latitude
40.664848799999994
West longitude
-77.9072458
East longitude
-77.9072458
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 Shale Hills Susquehanna Critical Zone Observatory.
CZO ID
6786
Additional Metadata
| Name | Value |
|---|---|
| czos | Shale Hills |
| czo_id | 6786 |
| citation | The following acknowledgment should accompany any publication or citation of these data: Logistical support and/or data were provided by the NSF-supported Shale Hills Susquehanna Critical Zone Observatory. |
| keywords | hydrology, stream flow, water, discharge, stage, conductivity, specific conductivity, stream water temperature |
| subtitle | Shale Hills Stream Discharge, Water Temperature, and Conductivity Data - Level 1 |
| variables | TmStamp_UTC, Stage_m, Water_TempC, Cond (conductivity), spc_cond (specific conductivity), dischg_m3s_m3s (discharge in cubic meters per second), dischg_cfs (discharge in cubic feet per second) |
| disciplines | Hydrology |
| date_range_comments | 2015 2015-11-03 to 2015-11-19: no flow and building up ice 2015-11-20 to 2015-12-01: ice 2016 2016-12-15 : ice 2016-12-20 to 2016-12-25 : ice 2016-01-05 to 2016-01-08: ice 2016-01-09 to 2016-01-10: ice 2016-01-13 to 2016-01-14: ice 2016-01-18 to 2016-01-31: ice 2016-02-11 to 2016-02-21: ice 2016-04-20: debris buildup 2016-06-10 to 2016-11-30: no flow – summer was dry 2017 2017-01-07 to 2017-01-12: ice 2017-05-03: debris buildup 2017-05-17 to 2017-05-29: debris buildup 2017-06-08 to 2017-06-16: debris buildup 2017-06-29 to 2017-07-11: debris buildup 2017-10-17: erroneous data spikes 2017-11-20 to 2017-11-21: ice 2017-12-13 to 2018-01-01: ice |
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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