PEARL RIVER

River Levels Streamflow Hydrology
November 21, 2024

TOTAL DISCHARGE (CFS)

SUMMARY

Last Updated 2024-11-20
Discharge Volume 45,019 ACRE-FT
Streamflow 22,697.0 cfs
+12198.0 cfs (+116.18%)
Percent of Normal 178.56%
Maximum 382,590.0 cfs
2020-02-22
Seasonal Avg 12,711 cfs

Total streamflow across the Pearl River was last observed at 22,697 cfs, and is expected to yield approximately 45,019 acre-ft of water today; about 179% of normal. River levels are high. Average streamflow for this time of year is 12,711 cfs, with recent peaks last observed on 2020-02-22 when daily discharge volume was observed at 382,590 cfs.

Maximum discharge along the river is currently at the Pearl River Nr Monticello reporting a streamflow rate of 7,530 cfs. However, the streamgauge with the highest stage along the river is the Pearl River Nr Rockport with a gauge stage of 14.1 ft. This river is monitored from 9 different streamgauging stations along the Pearl River, the highest being situated at an altitude of 382 ft, the Pearl River At Burnside.

The Pearl River is a major river system in the southeastern United States. The river flows for 485 miles through Mississippi and Louisiana, emptying into the Gulf of Mexico. The river has a rich history, playing a significant role in the Civil War and serving as a transportation route for Native American tribes.

The hydrology of the Pearl River is heavily influenced by several large reservoirs and dams, including the Ross Barnett Reservoir and the Bonnet Carré Spillway. These structures help manage flood control, water supply, and hydroelectric power generation.

Recreational activities along the Pearl River include fishing, boating, and camping. The river also supports agricultural activities, with farms and ranches along its banks producing crops such as cotton, soybeans, and rice. Despite its importance, the Pearl River faces threats from pollution and habitat destruction, highlighting the need for continued conservation efforts.

YEAR OVER YEAR DISCHARGE (CFS)

Streamflow Conditions
Streamgauge Streamflow Gauge Stage 24hr Change (%) % Normal Minimum (cfs) Maximum (cfs) Air Temp Elevation
Pearl River At Burnside
USGS 02481880
1000 cfs 9.17 ft -5.66
Pearl River At Edinburg
USGS 02482000
621 cfs 7.47 ft 352.63
Pearl River Nr Lena
USGS 02483500
2010 cfs 8.55 ft 154.13
Pearl River Nr Carthage
USGS 02482550
699 cfs 7.36 ft 159.34
Pearl River At Jackson
USGS 02486000
3220 cfs 9.96 ft 1648.82
Pearl River Nr Rockport
USGS 02488000
7020 cfs 14.1 ft 132.5
Pearl River Nr Monticello
USGS 02488500
7530 cfs 12.27 ft 212.09
Pearl River Nr Columbia
USGS 02489000
6330 cfs 5.21 ft 46.57
Pearl River Near Bogalusa
USGS 02489500
3940 cfs 9.17 ft -9.52
History of the River

The Pearl River Delta Metropolitan Region (PRD, Chinese: 珠江三角洲城市圈; pinyin: Zhūjiāng Sānjiǎozhōu Chéngshìquān) is the low-lying area surrounding the Pearl River estuary, where the Pearl River flows into the South China Sea. It is one of the most densely urbanized regions in the world, and is often considered as a megacity. It is now the wealthiest region in South China and one of the wealthiest in the whole of China along with Yangtze River Delta in East China and Jingjinji in North China. The region's economy is referred to as Pearl River Delta Economic Zone, it is also part of the Guangdong-Hong Kong-Macau Greater Bay Area.
The PRD is a megalopolis, with future development into a single mega metropolitan area, yet itself is at the southern end of a larger megalopolis running along the southern coast of China, which include metropolises such as Chaoshan, Zhangzhou-Xiamen, Quanzhou-Putian and Fuzhou. The nine largest cities of the PRD had a combined population of 57.15 million at the end of 2013, comprising 53.69% of the provincial population. According to the World Bank Group, the PRD has become the largest urban area in the world in both size and population.The west side of this region, along with Chaoshan, was also the source of much Chinese emigration from the 19th to the mid 20th centuries, including to the Western world, where they formed many Chinatowns. Today, much of the Chinese diaspora in the US, Canada, Australia, Latin America, and much of Southeast Asia traces their ancestry to the west side of this region. Its dominant language is Cantonese.

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