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Logan River, flow, stage, and barometric pressure at Temple Fork Creek

Authors: Bethany Neilson
Owners: Bethany Neilson · iUTAH Data Manager
Resource type:Composite Resource
Created:Jan 28, 2018 at 8:56 p.m.
Last updated: Jun 28, 2018 at 10:47 p.m. by Bethany Neilson

Abstract

The QC0 file contains the raw pressure, temperature, and depth data collected by an in-situ AquaTroll. The QC1 file contains the quality-controlled depth data and the derived stage and discharge data. The depth data is a measure of the water surface elevation relative to the AquaTroll. The derived stage data is the water surface elevation relative to a benchmark at the site. The discharge data is calculated from the stage data using the relationship established from the site rating curve. The stage-discharge relationship was developed by making measurements of flow and stage under varying flow conditions and thus establishing a relationship between water depth and flow at the site. Flow measurements were made with a YSI Flowtracker handheld ADV using the velocity area method. The barometric pressure data was collected using an in-situ BaroTroll.

Subject Keywords

flow,barometric pressure,discharge,Logan River,iUTAH,water quantity,stage

How to cite

Neilson, B. (2018). Logan River, flow, stage, and barometric pressure at Temple Fork Creek, HydroShare, http://www.hydroshare.org/resource/5b5fef41619a435a9b51ef04e79831a0

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

  http://creativecommons.org/licenses/by/4.0/
CC-BY

Sharing status:

  • Public Resource  Public
  • Sharable Resource  Shareable

Content

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Authors

The people or organizations that created the intellectual content of the resource.

Name Organization Address Phone Author Identifiers
Bethany Neilson Utah State University

Credits

This resource was created using funding from the following sources:
Agency Name Award Title Award Number
National Science Foundation iUTAH-innovative Urban Transitions and Aridregion Hydro-sustainability NSF Award Number 1208732

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