Résumé
We give the first demonstration that humidity has indirect effects on atmospheric spectra near 4 μm, through the influence of collisions with H2O on both the collision-induced band of N2 and the wings of the CO2 lines. This is shown by comparing computed and measured values of atmospheric transmissions and outgoing radiances. The usual assumption that collisions with H2O and dry air have equal effect on the N2 and CO2 absorptions leads to significantly underestimated absorptions for humid atmospheres. This bias is considerably reduced when the influences of H2O on the N2 and CO2 contributions to the spectra are taken into account using proper spectroscopic models. This opens perspectives of increased accuracy near 4 μm where the atmosphere is relatively transparent, for astronomical observations of outer objects from ground as well as for retrievals of the Earth land/sea surface temperatures from radiances recorded from space.
| langue originale | Anglais |
|---|---|
| Pages (de - à) | 12,593-12,601 |
| journal | Geophysical Research Letters |
| Volume | 45 |
| Numéro de publication | 22 |
| Les DOIs | |
| état | Publié - 28 nov. 2018 |
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