Stratospheric water vapor from high resolution infrared spectra
dc.contributor.author | Ackerman, M. | |
dc.date | 1974 | |
dc.date.accessioned | 2017-08-30T13:27:26Z | |
dc.date.available | 2017-08-30T13:27:26Z | |
dc.identifier.uri | https://orfeo.belnet.be/handle/internal/6048 | |
dc.description | A volume of mixing ratio equal to (3·4 ± 0.7) × 10-6 is deduced for the stratospheric water vapour from 20 to 37 km. The results have been obtained by absorptiometry from a balloon platform at 40 km. | |
dc.language | eng | |
dc.title | Stratospheric water vapor from high resolution infrared spectra | |
dc.type | Article | |
dc.subject.frascati | Earth and related Environmental sciences | |
dc.audience | Scientific | |
dc.source.title | Planetary and Space Science | |
dc.source.volume | 22 | |
dc.source.issue | 8 | |
dc.source.page | 1265-1267 | |
Orfeo.peerreviewed | Yes | |
dc.identifier.doi | 10.1016/0032-0633(74)90009-9 | |
dc.identifier.scopus | 2-s2.0-49549158877 |