KENTUCKY RIVER

River Levels Streamflow Hydrology
November 21, 2024

TOTAL DISCHARGE (CFS)

SUMMARY

Last Updated 2024-11-20
Discharge Volume 40,483 ACRE-FT
Streamflow 20,410.0 cfs
+936.0 cfs (+4.81%)
Percent of Normal 47.56%
Maximum 893,000.0 cfs
2021-03-03
Seasonal Avg 42,914 cfs

Total streamflow across the Kentucky River was last observed at 20,410 cfs, and is expected to yield approximately 40,483 acre-ft of water today; about 48% of normal. River levels are low and may signify a drought. Average streamflow for this time of year is 42,914 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 12 Near Irvine reporting a streamflow rate of 8,300 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 12.82 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.

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
1200 cfs 10.17 ft 29.9
Kentucky River At Lock 10 Near Winchester
USGS 03284000
1590 cfs 10.98 ft 10.22
Kentucky River At Lock 11 Near College Hill
USGS 03282290
1260 cfs 11.84 ft 24.24
Kentucky River At Lock 12 Near Irvine
USGS 03282120
8300 cfs 10.11 ft -20.19
Kentucky River At Lock 9 At Valley View
USGS 03284230
1780 cfs 12.05 ft -6.15
Kentucky River At Lock 8 Near Camp Nelson
USGS 03284500
1820 cfs 12.82 ft -9.03
Kentucky River At Lock 6 Near Salvisa
USGS 03287000
1830 cfs 10.68 ft -5.02
Kentucky River At Lock 7 At Highbridge
USGS 03286500
4390 cfs 10.33 ft 24.01
Kentucky River At Lock 5 Near Tyrone
USGS 03287250
1820 cfs 9.84 ft 1.08
Kentucky River At Lock 4 At Frankfort
USGS 03287500
2060 cfs 7.58 ft 1.75
Kentucky River At Lock 3 At Gest
USGS 03290080
2440 cfs 8.54 ft 5.9
Kentucky River At Lock 2 At Lockport
USGS 03290500
2470 cfs 9.55 ft 17.05
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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Watershed River Levels

96

Cubic Feet Per Second

1

Cubic Feet Per Second

9

Cubic Feet Per Second

3

Cubic Feet Per Second