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DESCRIPTION:

Latitude 40°58'30",   Longitude 102°15'05"   NAD27

Sedgwick County, Colorado, Hydrologic Unit 10190018

Drainage area: 22,824 square miles

Datum of gage: 3,449.80 feet above   NAVD88.

AVAILABLE DATA:

Data Type	Begin Date	End Date	Count
Daily Data
Temperature, water, degrees Celsius	1973-02-22	1979-10-15	6604
Discharge, cubic feet per second	1902-04-01	2018-09-30	41030
Specific conductance, water, unfiltered, microsiemens per centimeter at 25 degrees Celsius	1973-02-22	1979-10-15	2271
Daily Statistics
Temperature, water, degrees Celsius	1973-02-22	1979-10-15	2215
Discharge, cubic feet per second	1902-04-01	2018-09-30	41030
Specific conductance, water, unfiltered, microsiemens per centimeter at 25 degrees Celsius	1973-02-22	1979-10-15	2271
Monthly Statistics
Temperature, water, degrees Celsius	1973-02	1979-10
Discharge, cubic feet per second	1902-04	2018-09
Specific conductance, water, unfiltered, microsiemens per centimeter at 25 degrees Celsius	1973-02	1979-10
Annual Statistics
Temperature, water, degrees Celsius	1973	1980
Discharge, cubic feet per second	1902	2018
Specific conductance, water, unfiltered, microsiemens per centimeter at 25 degrees Celsius	1973	1980
Peak streamflow	1902-09-29	2018-05-23	114
Field measurements	1993-08-25	1993-08-25	1
Field/Lab water-quality samples	1900-03-30	2013-09-22	802
Water-Year Summary	2005	2018	14
Revisions	Loading...

OPERATION:

Record for this site is maintained by the USGS Colorado Water Science Center

Email questions about this site to Colorado Water Science Center Water-Data Inquiries

ADDITIONAL INFORMATION

This streamflow gaging station is operated by the Colorado Division of Water Resources (DWR). 
The USGS works cooperatively with the DWR to publish daily mean (and annual peak) discharge 
data for this station. These are the only streamflow data available in NWISWeb for this site. 
Current streamflow data (and other historical streamflow data) for this site are available on 
the DWR Colorado's Surface Water Conditions pages 
(channel #1 shown - due to the braided condition of the channel, flow may also occur in 
Channel #'s 2 and 4).