KENTUCKY RIVER

RIVER LEVELS
December 21, 2024
38.68, -85.19


TOTAL RIVER DISCHARGE

Total streamflow across the Kentucky River was last observed at 194,780 cfs, and is expected to yield approximately 386,341 acre-ft of water today; about 226% of normal. River levels are high. Average streamflow for this time of year is 86,224 cfs, with recent peaks last observed on 2021-03-03 when daily discharge volume was observed at 893,000 cfs.

Maximum discharge along the river is currently at the Kentucky River At Lock 3 At Gest reporting a streamflow rate of 25,400 cfs. However, the streamgauge with the highest stage along the river is the Kentucky River At Lock 8 Near Camp Nelson with a gauge stage of 18.87 ft. This river is monitored from 12 different streamgauging stations along the Kentucky River, the highest being situated at an altitude of 630 ft, the Kentucky River At Lock 14 At Heidelberg.

The Kentucky River is a tributary of the Ohio River, covering a total length of 259 miles. It has a significant history in the state of Kentucky, as it was a vital transportation route for early settlers and served as a source of power for mills and factories in the 19th century. The river's hydrology includes multiple tributaries, with some of the major ones being the North Fork, Middle Fork, and South Fork. The river is impounded by several dams, including the Lock and Dam 11, which creates the reservoir known as the Kentucky River Lake. Other recreational areas around the river include the Kentucky River Palisades and the Clifty Wilderness Area. The Kentucky River is used for agricultural purposes, including irrigation and livestock watering.

Last Updated 2024-12-21
Discharge Volume 386,341 ACRE-FT
Streamflow 194,780.0 cfs
-61720.0 cfs (-24.06%)
Percent of Normal 225.9%
Maximum 893,000.0 cfs
2021-03-03
Seasonal Avg 86,224 cfs

YEAR OVER YEAR DISCHARGE (CFS)

Streamflow Conditions
Streamgauge Streamflow Gauge Stage 24hr Change (%) % Normal Minimum (cfs) Maximum (cfs) Air Temp Elevation
Kentucky River At Lock 14 At Heidelberg
USGS 03282000
8780 cfs 13.92 ft -26.83
Kentucky River At Lock 10 Near Winchester
USGS 03284000
14300 cfs 15.91 ft -29.9
Kentucky River At Lock 11 Near College Hill
USGS 03282290
10900 cfs 16.72 ft -24.31
Kentucky River At Lock 12 Near Irvine
USGS 03282120
8300 cfs 14.82 ft -20.19
Kentucky River At Lock 9 At Valley View
USGS 03284230
14500 cfs 16.77 ft -28.57
Kentucky River At Lock 8 Near Camp Nelson
USGS 03284500
16700 cfs 18.87 ft -29.54
Kentucky River At Lock 6 Near Salvisa
USGS 03287000
19700 cfs 15.68 ft -22.13
Kentucky River At Lock 7 At Highbridge
USGS 03286500
18700 cfs 15.75 ft -24.9
Kentucky River At Lock 5 Near Tyrone
USGS 03287250
21000 cfs 14.2 ft -21.93
Kentucky River At Lock 4 At Frankfort
USGS 03287500
20200 cfs 11.61 ft -21.09
Kentucky River At Lock 3 At Gest
USGS 03290080
25400 cfs 18.04 ft -20.13
Kentucky River At Lock 2 At Lockport
USGS 03290500
24600 cfs 15.8 ft -21.15
History of the River

The Kentucky River is a tributary of the Ohio River, 260 miles (418 km) long, in the U.S. Commonwealth of Kentucky. The river and its tributaries drain much of the central region of the state, with its upper course passing through the coal-mining regions of the Cumberland Mountains, and its lower course passing through the Bluegrass region in the north central part of the state. Its watershed encompasses about 7,000 square miles (18,000 km2). It supplies drinking water to about one-sixth of the population of the Commonwealth of Kentucky.
The river is no longer navigable above Lock 4 at Frankfort. Concrete bulkheads have been poured behind the upper lock gates of Locks 5-14 to strengthen the weakest link in the dam structures. All 14 dams are now under the management of the state-run Kentucky River Authority. The primary importance of the locks today is to maintain a pool that allows the city of Lexington to draw its drinking water from the river. Despite the fact that the Lexington area receives well over 40 inches (1,000 mm) of precipitation annually, the limestone, karst geology of that area means that surprisingly little natural surface water is found in the region.
Winchester, Beattyville, Irvine, Richmond, Lancaster, Nicholasville, Harrodsburg, Wilmore, Versailles, Lawrenceburg, and Frankfort also draw water from the river for their municipal water supplies. It is estimated that over 700,000 people depend on the river for water.

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