Table 3.
Overall lake stability (S) and CO2 content in Lake Nyos and Lake Monoun
| Date | Lake | S, Joule/m2 | Total CO2† | CO2 at depth‡ |
|---|---|---|---|---|
| March–April 1992 | Nyos | 65,570 | 1.343 | 1.325 |
| May 1998 | Nyos | 69,720 | 1.375 ± 0.021 | 1.355 ± 0.023 |
| Nov. 1999 | Nyos | 75,250 | 1.438 ± 0.014 | 1.410 ± 0.010 |
| Jan. 2001 | Nyos | 71,970 | 1.504 ± 0.061 | 1.452 ± 0.064 |
| Jan. 2003 | Nyos | 71,110 | 1.390 ± 0.001 | 1.362 ± 0.036 |
| Jan. 2004 | Nyos | 67,980 | 1.305 ± 0.009 | 1.302 ± 0.009 |
| March–April 1992 | Monoun | 6,500 | 5.362 | 5.328 |
| Nov. 1999 | Monoun | 6,700 | 5.849 ± 0.114 | 5.831 ± 0.115 |
| Jan. 2003 | Monoun | 6,420 | 6.284 ± 0.011 | 6.250 ± 0.020 |
| Jan. 2004 | Monoun | 7,130 | 5.393 ± 0.065 | 5.365 ± 0.066 |
CO2 content is in mol × 1010 for Lake Nyos and mol × 108 for Lake Monoun (main basin only)
CO2 at depth gives content from 50- to 210-m depth (Nyos) and 20- to 100-m depth (Monoun). CO2 content of surface waters is equal to (total CO2 – CO2 at depth), and changes over time of this difference indicate surface water losses of CO2