loading page

Investigating the role of the Cuvette Centrale in the hydrology of the Congo
  • +5
  • PANKYES DATOK,
  • Clément Fabre,
  • Sabine Sauvage,
  • Moukandi N'kaya,
  • Adrien Paris,
  • Vanessa Dos-Santos,
  • Alain Laraque,
  • José-Miguel Sanchez -Perez
PANKYES DATOK
Université de Toulouse

Corresponding Author:[email protected]

Author Profile
Clément Fabre
Université de Toulouse
Author Profile
Sabine Sauvage
Université de Toulouse
Author Profile
Moukandi N'kaya
Université Marien Ngouabi
Author Profile
Adrien Paris
Ocean Next, Grenoble
Author Profile
Vanessa Dos-Santos
Université de Toulouse
Author Profile
Alain Laraque
Institut de Recherche pour le Développment, Toulouse
Author Profile
José-Miguel Sanchez -Perez
Université de Toulouse
Author Profile

Abstract

15 The increasing pressure on wetland resources continues to threaten the role wetlands play in 16 maintaining the ecological balance of watersheds. The Cuvette Centrale of the Congo is the 17 greatest intertropical peatland in the world. To fully understand its role in water resources and 18 ecological services linked to the quality of water and life in the basin, we first need to quantify 19 its role in the hydrological dynamics. To achieve this aim, we used the Soil and Water 20 Assessment Tool model (SWAT)-modified for tropical environments-in combination with 21 monthly discharge data. We analyzed water fluxes entering and flowing out of the Cuvette 22 Centrale of the Congo River Basin on a monthly time scale for the 2000-2012 period. The 23 model was calibrated, validated, and compared with discharge from gauging stations and 24 surface water elevation from radar altimetry. Results showed that upland runoff from the 25 Congo River was the highest contributor to the Cuvette Centrale (33 percent) followed closely 26 by efficient precipitation inside the Cuvette Centrale (31 percent) with right bank and left bank 27 tributaries contributing 25 percent and 11 percent respectively. We simulated monthly mean 28 interannual inflows of approximately 34,150 m 3 s-1 (88 billion m 3) with the main flood peaking 29 in November (45,310 m 3 s-1) and total outflows averaging around 39,860 m 3 s-1 (100 billion 30 m 3) peaking at 52,430 m 3 s-1 in December for the simulation period. We subsequently estimated 31 a negative monthly mean interannual variation of storage in the Cuvette Centrale wetlands in 32 the order of 5,700 m 3 s-1 suggesting that the Cuvette Centrale supplies the river during low 33 water periods. This highlights the important regulatory function of the Cuvette Centrale and 34 the need for protection of groundwater resources in order to maintain wetland water quantities 35 and quality. 36
25 Feb 2022Published in Congo Basin Hydrology, Climate, and Biogeochemistry on pages 247-273. https://doi.org/10.1002/9781119657002.ch14