"Ozone loss form quasi-conservative coordinate mapping during the 1999-2000 SOLVE/THESEO campaign"
dc.contributor.author | Lait, L.R. | |
dc.contributor.author | Schoeberl, M.R. | |
dc.contributor.author | Newman, P.A. | |
dc.contributor.author | McGee, T. | |
dc.contributor.author | Burris, J. | |
dc.contributor.author | Browell, E.V. | |
dc.contributor.author | Richard, E. | |
dc.contributor.author | Braathen, G. O. | |
dc.contributor.author | Bojkov, B.R. | |
dc.contributor.author | Goutail, F. | |
dc.contributor.author | von der Gathen, P. | |
dc.contributor.author | Kyrö, E. | |
dc.contributor.author | Vaughan, G. | |
dc.contributor.author | Kelder, H. | |
dc.contributor.author | Kirkwood, S. | |
dc.contributor.author | Woods, P. | |
dc.contributor.author | Dorokhov,V. | |
dc.contributor.author | Zaitcec, I. | |
dc.contributor.author | Lytinska, Z. | |
dc.contributor.author | Benesova, A. | |
dc.contributor.author | Srivankova, P. | |
dc.contributor.author | De Backer, H. | |
dc.contributor.author | Davies, J. | |
dc.contributor.author | Jorgensen, T. | |
dc.contributor.author | Mikkelsen, I.S. | |
dc.coverage.temporal | 1999-2000 | |
dc.date | 2002 | |
dc.date.accessioned | 2016-03-07T16:16:38Z | |
dc.date.accessioned | 2021-12-09T09:53:48Z | |
dc.date.available | 2016-03-07T16:16:38Z | |
dc.date.available | 2021-12-09T09:53:48Z | |
dc.identifier.uri | https://orfeo.belnet.be/handle/internal/8752 | |
dc.description | Ozone observations made by the Airborne Raman Ozone, Temperature, and Aerosol Lidar (AROTEL) and Differential Absorption Lidar (DIAL) on board the NASA DC-8 aircraft, the NOAA in situ instrument on board the NASA ER-2 aircraft, and Third European Stratospheric Experiment on Ozone 2000 (THESEO 2000) ozonesondes are analyzed by applying a quasi-conservative coordinate mapping technique. Measurements from the late winter/early spring SAGE III Ozone Loss and Validation Experiment (SOLVE) period (January through March 2000) are incorporated into a time-varying composite field in a potential vorticity-potential temperature coordinate space; ozone loss rates are calculated both with and without diabatic effects. The average loss rate from mid-January to mid-March near the 450 K isentropic surface in the polar vortex is found to be approximately 0.03 ppmv/d. | |
dc.language | eng | |
dc.publisher | IRM | |
dc.publisher | KMI | |
dc.publisher | RMI | |
dc.relation.ispartofseries | J. Geophys. Res. | |
dc.title | "Ozone loss form quasi-conservative coordinate mapping during the 1999-2000 SOLVE/THESEO campaign" | |
dc.type | Article | |
dc.subject.frascati | Earth and related Environmental sciences | |
dc.audience | General Public | |
dc.audience | Scientific | |
dc.subject.free | Ozone loss | |
dc.subject.free | 1999-200 | |
dc.subject.free | SOLVE/THESEO | |
dc.subject.free | lidar | |
dc.source.issue | J. Geophys. Res. | |
Orfeo.peerreviewed | Not pertinent | |
dc.identifier.doi | DOI 10.1029/2001JD000988 |
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