Spatial and temporal variations of dissolved CO2, CH4 and N2O in Lakes Edward and George (East Africa)

We report dissolved CO2, CH4 and N2O concentrations in two large East African lakes, Edward (surface area 2,325 km2, average depth of 37 m) and George (surface area 273 km2, average depth of 2 m). Lake George showed modest seasonal and spatial variations, and lower partial pressure of CO2 (pCO2) (26 & PLUSMN; 16 ppm, mean & PLUSMN; standard deviation), CH4 (234 & PLUSMN; 208 nmol/L) and N2O saturation levels (%N2O) (80 & PLUSMN; 9 %) than Lake Edward (404 & PLUSMN; 145 ppm, 357 & PLUSMN; 483 nmol/L, 139 & PLUSMN; 222 %). Surface waters in both lakes were over-saturated in CH4, and Lake George was under-saturated in CO2 while Lake Edward was slightly over-saturated in CO2. This difference was related to higher phytoplankton biomass in Lake George than Lake Edward, with average chlorophyll-a concentrations of 177 & PLUSMN; 125 and 18 & PLUSMN; 25 lg/L, respectively. Permanent high cyanobacterial biomass in Lake George led to uniform dissolved CO2, CH4 and N2O concentrations. In surface waters of Lake Edward, spatial variations of pCO2, CH4 and N2O were related to bottom depth, and locally (in particular in Katwe Bay) also related to the inputs of water from Lake George via the Kazinga Channel, a 40-km natural channel connecting the lakes. Short-term mixing events related to storms increased CO2, CH4 and N2O content in surface waters, in particular for CH4 and N2O. This indicates that mixing events in response to storms can create 'hot moments' for CH4 and N2O emissions to the atmosphere in tropical lakes, given the weaker vertical density gradients compared to higher latitude systems.& COPY; 2022 International Association for Great Lakes Research. Published by Elsevier B.V. All rights reserved.

Automated summary

We report the concentrations of dissolved CO2, CH4, and N2O in two large East African lakes, Edward and George. Lake George has lower levels of CO2, CH4, and N2O compared to Lake Edward, primarily due to higher phytoplankton biomass. Spatial variations in the concentrations of these gases are related to bottom depth and inputs from Lake George via the Kazinga Channel. Mixing events caused by storms can lead to increased emissions of CH4 and N2O in surface waters.