TOTAL DISCHARGE (CFS)
SUMMARY
| Last Updated | 2024-11-20 |
| Discharge Volume | 14,182 ACRE-FT |
| Streamflow |
7,150.1 cfs
+1232.2 cfs (+20.82%) |
| Percent of Normal | 98.43% |
| Maximum |
215,320.0 cfs
2024-09-29 |
| Seasonal Avg | 7,264 cfs |
Total streamflow across the
Catawba River
was last observed at
7,150
cfs, and is expected to yield approximately
14,182
acre-ft of water today; about 98%
of normal.
Average streamflow for this time of year is
7,264 cfs,
with recent peaks last observed
on
2024-09-29 when daily discharge volume was observed at
215,320 cfs.
Maximum discharge along the river is currently at the
Catawba River Below Catawba
reporting a streamflow rate of 6,030 cfs.
This is also the highest stage along the Catawba River, with a gauge stage of
7.75 ft at this location.
This river is monitored from 3 different streamgauging stations along the Catawba River, the highest being situated at an altitude of 1,235 ft, the
Catawba R Nr Pleasant Gardens.
The Catawba River is a 220-mile long river that flows through western North Carolina and South Carolina. It was historically significant to Native American tribes such as the Catawba and Cherokee. Today, it provides approximately 1.7 million people with drinking water and powers several hydroelectric power plants. The river has several reservoirs and dams, including the Lake James Dam, the Lake Hickory Dam, and the Mountain Island Lake Dam. These provide flood control, water supply, and recreational opportunities such as fishing, boating, and swimming. The Catawba River also supports agricultural uses, particularly for irrigation and livestock watering, and is home to a diverse array of wildlife, including fish, birds, and mammals.
YEAR OVER YEAR DISCHARGE (CFS)
Streamflow Conditions
| Streamgauge | Streamflow | Gauge Stage | 24hr Change (%) | % Normal | Minimum (cfs) | Maximum (cfs) | Air Temp | Elevation |
|---|---|---|---|---|---|---|---|---|
|
Catawba R Nr Pleasant Gardens
USGS 02137727 |
74 cfs | 1.49 ft | 3.8 | |||||
|
Catawba River Near Rockhill
USGS 02146000 |
1630 cfs | 3.78 ft | 1.25 | |||||
|
Catawba River Below Catawba
USGS 02147020 |
6030 cfs | 7.75 ft | 28.4 |
History of the River
The Catawba River (named after the Native American tribes that first settled on the banks) originates in Western North Carolina and the name of the river changes to the Wateree River in South Carolina. The river is approximately 220 miles (350 km) long. It rises in the Appalachian Mountains and drains into the Piedmont, where it has been impounded through a series of reservoirs for flood control and generation of hydroelectricity. The river is named after the Catawba tribe of Native Americans. In their Siouan language, they identified as the Kawahcatawbas, "the people of the river".
It rises in the Blue Ridge Mountains in western McDowell County, North Carolina, approximately 20 miles (30 km) east of Asheville. It flows ENE, forming, along with the Linville River, Lake James. It passes north of Morganton, then southeast through Lake Hickory just north of Hickory, NC, and into the Lake Norman reservoir. From Lake Norman it flows south, passing west of Charlotte, then flowing through the Mountain Island Lake and Lake Wylie reservoirs, where it forms approximately 10 miles (15 km) of the border between North Carolina and South Carolina. The confluence of the South Fork Catawba River and Catawba River is submerged by Lake Wylie near the NC/SC state line.
It flows into northern South Carolina, passing Rock Hill, through Fishing Creek Reservoir near Great Falls, and into the Lake Wateree reservoir, approximately 30 miles (50 km) northeast of Columbia. At the now-submerged confluence with Wateree Creek, it becomes known as the Wateree River.
