windows_atmos3::CO (No. 5)
Links:
| Window ID | Central Freq (cm-1) | Full Width (cm-1) | No. Lines | E" (cm-1) | Altitude Range (km) | Rating | Remarks | |
|---|---|---|---|---|---|---|---|---|
| 1 | 1 | 2045.78 | 1 | 0 | 0 | 10 - 40 | 1 | H2O CO2 |
| 1 | 2 | 2111.54 | 0.8 | 0 | 0 | 30 - 99 | 1 | CO2 O3 |
| 1 | 3 | 2135.54 | 0.7 | 0 | 0 | 20 - 99 | 1 | O3 |
| 1 | 4 | 2139.43 | 1 | 0 | 0 | 20 - 99 | 1 | H2O CO2 O3 N2O |
| 1 | 5 | 2144.03 | 1 | 0 | 0 | 0 - 30 | 1 | H2O CO2 O3 CH4 |
| 1 | 6 | 2147.08 | 0.8 | 0 | 0 | 20 - 99 | 1 | H2O O3 |
| 1 | 7 | 2156.51 | 1 | 0 | 0 | 0 - 20 | 1 | H2O CO2 O3 |
| 1 | 8 | 2158.3 | 1 | 0 | 0 | 20 - 99 | 1 | O3 N2O |
| 1 | 9 | 2183.2 | 0.4 | 0 | 0 | 20 - 99 | 1 | O3 N2O |
| 1 | 10 | 2186.64 | 0.4 | 0 | 0 | 20 - 99 | 1 | O3 N2O |
| 1 | 11 | 2189.9 | 0.4 | 0 | 0 | 20 - 99 | 1 | O3 N2O |
| 1 | 12 | 4180.28 | 0.26 | 0 | 0 | 0 - 25 | 1 | H2O HDO |
| 1 | 13 | 4190.24 | 0.16 | 0 | 0 | 0 - 25 | 1 | H2O CH4 HDO |
| 1 | 14 | 4199.93 | 0.5 | 0 | 0 | 0 - 50 | 1 | H2O CH4 |
| 1 | 15 | 4231.68 | 0.5 | 0 | 0 | 0 - 99 | 1 | H2O CH4 HDO |
| 1 | 16 | 4236 | 0.5 | 0 | 0 | 0 - 85 | 1 | H2O CH4 HDO |
| 1 | 17 | 4248.32 | 0.5 | 0 | 0 | 0 - 90 | 1 | H2O CH4 HDO |
| 1 | 18 | 4274.74 | 0.35 | 0 | 0 | 0 - 80 | 1 | CH4 HDO |
| 1 | 19 | 4285.01 | 0.22 | 0 | 0 | 0 - 90 | 1 | CH4 |
| 1 | 20 | 4300.66 | 0.35 | 0 | 0 | 0 - 85 | 1 | CH4 |
Remarks:
- (0) Lack of good lines for the 15-50 km altitude range necessitates extrapolation down to tropopause, of lines being significantly saturated.
- (0) Below 30 km or so, DS fitting may be useful or required.
- (0) If ODS does not handle 40 cm-1 wide windows, these should be sliced into 2 X 20 cm-1.
- (0) CPRs microwindows incorporated
References:
- (0) Gunson, M.R. et al. , Measurements of CH4, N2O, CO, H2O, and O3 in the middle atmosphere by the Atmospheric Trace Molecule Spectroscopy experiment on Spacelab 3, J. Geophys. Res., 95, 13,867-13,882, 1990