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CNPPID Reservoir Elevation
& Platte River Flow Data
(Unofficial data subject to revision)

 

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Elevation in Feet Above Mean Sea Level
 
Today
May 21  (7 am)
Week
Ago
Month
Ago
Year
Ago
Lake McConaughy
(Historical graph -- Last 12 months graph -- 1-Month graph)

3240.6
Vol.= 1,100,300 acre-feet
%Max*63.1

3240.3
Vol.= 1,095,900 a-f
%Max* = 62.9
3240.6
Vol.= 1,100,300 a-f
%Max* = 63.1

3254.0
Vol.= 1,430,100 a-f
%Max* = 82.0

Jeffrey Lake
(30-day graph)
2758.3
2757.3
2757.6
2758.0
Johnson Lake
(30-day graph)
2617.6
2617.6
2617.0
2618.1
Elwood Reservoir
(Current water year graph -- Last 5 years)
(Max. elev. = 2607.0; Min. elev. = 2568.8)
2602.5

2600.9

2592.6
2605.9
 
Stream flow in cubic feet per second (cfs). Spot reading for current day; daily average for week, month, and year ago.
 
 Today (7 a.m.)
Week Ago
Month Ago
Year Ago
Inflows to Lake McConaughy
(Current, Average & Median Inflow graph)
634
686
1,241
628
Total Lake McConaughy Outflow 
950
764
1,491
1,352
North Platte below Keystone Dam 
255
178
10
648
Keystone Dam Diversion
714
442
1,702
554
North Platte at North Platte
539
298
448
964
South Platte at Roscoe***
N/A
N/A N/A
N/A
South Platte at North Platte
329
306 263 195
Diversion to CNPPID Supply Canal
950
865 2,105 1,097
Platte River at Overton
400
471
2,276
208
Platte River at Kearney
249
486 2,233 300
Platte River at Grand Island
359
502 2,374
587

* Percent of capacity is dependent upon maximum elevations/operating levels at different times of the year.  Lower maximum levels were established in 1974 after a 1972 storm caused damage to the dam's face.  The limits are in effect for periods when high winds and waves are most likely to occur.  (See Lake McConaughy Maximum Operating Levels table)
** Flow too low for gauge to measure
*** River gauge for South Platte at Roscoe is out of use due to budget cuts until further notice.

@ - Yesterday's average flow
# - Ice affecting stream gauges; readings may not be accurate
N/A - Data temporarily unavailable (data not reported from gauge)

Note: Flow records during winter months are often affected by ice conditions in the river(s). When ice forms, the river cross-section is constricted, resulting in a higher river stage for the amount of flow than exists during ice-free conditions. Therefore, the streamflow readings may be too high and freezing temperatures may also affect the gauging equipment, resulting in inaccurate data recording or no report from the gauge. Flows may be estimated under these circumstances. Equipment or communications problems also sometimes prevent transfer of river stage data during other times of the year, resulting in an N/A display in the table above.

 

Other Nebraska current stream flow conditions from U.S. Geologic Survey (USGS) gauging stations

 

National Water Conditions: Current daily stream flows in real time for all measuring gauges in U.S.A.

 

Department of Natural Resources: Tentative Apportionment of Flows (an analysis of flow between Kingsley Dam and Kearney, including storage water, natural flow and Environmental Account water)

 


The Central Nebraska Public Power and Irrigation District
415 Lincoln Street , P.O. Box 740
Holdrege, Nebraska 68949
Phone 308-995-8601
For additional information, contact: WebMaster

(Updated 5/21/13 )

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