ANSON — On Monday, January eighth, a robust storm swept by the southeastern United States, bringing heavy rains, wind gusts, and excessive sustained winds from as far south as Atlanta, GA, to as far north as Norfolk, VA.
The Pee Dee River, an important waterway within the area, was one of many beneficiaries of the substantial rainfall, resulting in important modifications in water ranges and the encompassing panorama.
The Pee Dee River originates within the Appalachian Mountains of North Carolina, the place its higher course, above the Uwharrie River, is named the Yadkin River. The river’s identify modifications to the Pee Dee at its merger with the Uwharrie River. It travels southward, ultimately merging with the Waccamaw River to type the Winyah Bay that empties into the Atlantic Ocean close to Georgetown, SC.
This 232-mile-long river often known as the Nice Pee Dee performs a vital position within the area’s ecosystem and financial system because it winds its solution to the Atlantic Ocean.
As rain falls all through the river basin, numerous creeks, branches and tributaries channel rainwater from its touchdown spot into the Pee Dee.
The Nationwide Oceanic and Atmospheric Administration (NOAA), a US Commerce Division tracks climate and rainfall by its Nationwide Climate Service (NWS).
The NWS gives climate and local weather forecasts and warnings for america, its territories, adjoining waters and ocean areas, for the safety of life and property and the enhancement of the nationwide financial system.
The widespread rain fall from Sunday, January 7th and Monday, January 8th induced the Pee Dee to swell. In keeping with information of the NWS, rain fell from a excessive of two.14” in Albemarle, NC to 1.5” in different areas of the Yadkin Pee Dee River basin.
The heavy rain fall result in elevated water ranges, inflicting flooding in low-lying areas alongside the riverbanks. Grassy Island Highway in Anson County (often known as County Highway 1634) that’s lower than 5 hundred yards from the Pee Dee in some areas in Anson County skilled some flooding from the Pee Dee. Whereas many different low-lying bridges and roadways in Anson County skilled some flooding it could not have been a direct results of the upper water stage of the Pee Dee. Conversely, these increased water ranges most probably flowed into the Pee Dee.
Usually the chemical high quality of the floor waters within the Yadkin-Pee Dee River basin is sweet. The floor waters are low in mineral matter though a number of the floor water incorporates extreme portions of iron.
Blewett Falls Lake borders Anson and Richmond counties and close by Lake Tillery borders Montgomery and Stanly counties.
Lake Tillery in North Carolina has a median depth of 32 toes and a most depth of 72 toes. The lake is 29.934 miles lengthy, has 104 miles of shoreline, and is 278 toes in elevation.
Lake Tillery is a artifical lake that was created in 1928 by damming the Yadkin and Pee Dee Rivers. The lake is a well-liked vacation spot for fishing tournaments, water sports activities, and swimming. The lake is house to many fish species, together with bass, catfish, crappie, and bream.
Blewett Falls Lake is a 2560-acre between Wadesboro, NC and Rockingham, NC. The lake is the storage reservoir for the Blewett Falls Hydroelectric Dam and is situated at roughly mile 195 on the Pee Dee River between Anson and Richmond counties. The dam has a most peak of about 50-feet above the river mattress.
The Blewett Falls growth started operation in 1912 and is owned and operated by Progress Vitality. The floor space of Blewett Falls Lake covers about 2560 acres on the regular full pool elevation of 178 toes above imply sea stage. At full pool elevation, the lake incorporates roughly 34 linear miles of shoreline.
There are six giant hydroelectric dams alongside the Pee Dee River. The uppermost reservoir is W. Kerr Scott Dam and Reservoir. The opposite reservoirs are: Excessive Rock Dam and Lake, Tuckertown Dam and Reservoir, Narrows Dam and Badin Lake, the Tillery Hydroelectric Plant Dam and Lake Tillery and The Blewett Falls Dam and Blewett Falls Lake.
The current storm and heavy rainfall have highlighted the dynamic relationship between climate patterns and the Pee Dee River’s conduct. As communities alongside the riverbanks navigate the challenges posed by elevated water ranges and flooding, it underscores the significance of monitoring and managing these waterways. The Pee Dee River and its surrounding lakes proceed to be integral to the area’s surroundings, financial system, and recreation, showcasing the resilience and adaptableness of communities within the face of pure forces.