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SSHCZO -- Streamflow / Discharge, Stream Suspended Sediment -- Shale Hills -- (2013-2016)

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Type:	Resource
Storage:	The size of this resource is 22.0 KB
Created:	Nov 19, 2019 at 6:29 a.m. (UTC)
Last updated:	Nov 21, 2019 at 8:05 p.m. (UTC)
Citation:	See how to cite this resource
Content types:	Single File Content

Sharing Status:	Public
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Abstract

Turbidity data collected upstream of Shale Hills weir. Use with caution, as the placement of probe was not ideal as it had to be in weir pond in order to obtain deep enough water to submerge probe. Stilling well installed with new flume in 2015 improved situation.
Date Range Comments: End Date should always be current day. Listed date is date of last update of this linking page only.

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Coverage

Spatial

Coordinate System/Geographic Projection:

WGS 84 EPSG:4326

Coordinate Units:

Decimal degrees

Place/Area Name:

Susquehanna Shale Hills Critical Zone Observatory, Shale Hills

Longitude

-77.9072°

Latitude

40.6649°

Temporal

Start Date:
End Date:

Content

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Additional Metadata

Name	Value
czos	Shale Hills
czo_id	4997
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	Turbidity, stream flow
subtitle	Level 0 - Raw Data
variables	Time Stamp, Record Number, Turbidity Maximum (NTU), Time of Turbidity Maximum within Last 15 Minutes, Turbidity Minimum (NTU), Time of Turbidity Minimum within Last 15 Minutes, Turbidity Average during Last 15 Minutes (NTU)
disciplines	Hydrology
date_range_comments	End Date should always be current day. Listed date is date of last update of this linking page only.

How to Cite

L., K. D. (2019). SSHCZO -- Streamflow / Discharge, Stream Suspended Sediment -- Shale Hills -- (2013-2016), HydroShare, http://www.hydroshare.org/resource/90aafb1028ec43dbb5b10a1302548c28

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/

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