Kuparuk River 1985 summer temperature and discharge calculated from state height.

Abstract: 

Stream temperature and discharge each summer, water temperature and stream discharge are determined for the Kuparuk River. In many years, temperature and stream height were recorded manually each day. In recent years, data loggers have measured stream temperature and stream height at regular intervals. The Kuparuk River data is maintained by Dough Kane on the Water and Environmental Research Center at UAF (http://www.uaf.edu/water/projects/NorthSlope/upper_kuparuk/uk_river/uk_r...) Stream height is converted into stream discharge based on a rating curve calculated from manual discharge measurements throughout the season. The principal investigator in charge of the temperature and discharge measurements is Dr. Breck Bowden.

Project Keywords: 

Data set ID: 

10504

EML revision ID: 

4
Published on EDI/LTER Data Portal

Citation Suggestion: 

Bowden, W. 1987. Kuparuk River 1985 summer temperature and discharge calculated from state height. Environmental Data Initiative. http://dx.doi.org/10.6073/pasta/092ce9d56166a5928ba1b8d0ee3502c1
People
Dates

Date Range: 

Thursday, June 27, 1985 to Wednesday, August 14, 1985

Publication Date: 

1987

Purpose: 

Longterm monitoring and experimentation

Methods: 

Discharge measurements were taken daily 1 km upstream of the Kuparuk River crossing at the Dalton Highway. Measurements were taken manually. It is unknown what type of sensor was used. It is also unknown what type of flow meter was used.

Some temperature data is available for this year. However, not all sampling days have temperature measurements.
Arctic LTER Streams Protocol, updated 2010 by EBS

http://ecosystems.mbl.edu/ARC/streams/protocol2.html

Version Changes: 

annual data updated to new file
7/23/13: EJE organized metadata and data into this file.
Version 2: Checked keywords, file ready for online (JD-Jan2014)
Version 3: Changed Distrubution URL since the LTER network DAS system is being discontinued. JimL 9Apr2015

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