Assessment of the Version 1.3 ILAS-II ozone data quality in the high latitude lower stratosphere
dc.contributor.author | Sugita, T. | |
dc.contributor.author | Kanzawa, H. | |
dc.contributor.author | Nakajima, H. | |
dc.contributor.author | Yokota, T. | |
dc.contributor.author | Gernandt, H. | |
dc.contributor.author | Herber, A. | |
dc.contributor.author | von der Gathen, P. | |
dc.contributor.author | König-langlo, G. | |
dc.contributor.author | Murayama, Y. | |
dc.contributor.author | Sato, K. | |
dc.contributor.author | Yushov, V.A. | |
dc.contributor.author | Dorokhov, V. | |
dc.contributor.author | Allaart, M. | |
dc.contributor.author | Litynska, Z. | |
dc.contributor.author | Braathen, G.O. | |
dc.contributor.author | Kyrö, E. | |
dc.contributor.author | De Backer, H. | |
dc.contributor.author | Yela, M. | |
dc.contributor.author | Klekociuk, A. | |
dc.contributor.author | Goutail, F. l | |
dc.contributor.author | Godin-Beekmann, S. | |
dc.contributor.author | Taalas, P. | |
dc.contributor.author | Deshler, T. | |
dc.contributor.author | Roscoe, H.K. | |
dc.contributor.author | Oltmans, S.J. | |
dc.contributor.author | Johnson, B. | |
dc.contributor.author | Koayashi, H. | |
dc.contributor.author | Sasano, Y. | |
dc.coverage.temporal | 21st century | |
dc.date | 2004 | |
dc.date.accessioned | 2016-03-07T16:16:44Z | |
dc.date.accessioned | 2021-12-09T09:56:53Z | |
dc.date.available | 2016-03-07T16:16:44Z | |
dc.date.available | 2021-12-09T09:56:53Z | |
dc.identifier | ISBN 960-630-103-6, ISBN 960-630-101-1, ISBN 960-630-105-2 | |
dc.identifier.uri | https://orfeo.belnet.be/handle/internal/9363 | |
dc.description | Vertical profiles of ozone in both of the highlatitudes were observed by Improved Limb Atmospheric Spectrometer (ILAS)-II from April through October 2003. The Version 1.3 ozone data are compared with data obtained by ozonesondes during the ILAS-II validation campaign, the project Quantitative Understanding of Ozone losses by Bipolar Investigations (QUOBI), and so on. A traditional correlative approach is used for searching for matching pairs that fulfill coincidence criteria of 500 km in distance and 12 hours in time difference. The ILAS-II ozone data generally agree with the ozonesonde data at altitudes between 15 and 30 km within ±10% and ±5% relative differences with 10-30% and 20-30% root mean square errors in the Northern Hemisphere and in the Antarctic, respectively. | |
dc.language | eng | |
dc.publisher | IRM | |
dc.publisher | KMI | |
dc.publisher | RMI | |
dc.relation.ispartofseries | Proceedings of the XX Quadrennial Ozone Symposium, 1-8 June 2004, Kos, Greece, Edt. C.S. Zerefos, | |
dc.title | Assessment of the Version 1.3 ILAS-II ozone data quality in the high latitude lower stratosphere | |
dc.type | Article | |
dc.subject.frascati | Earth and related Environmental sciences | |
dc.audience | General Public | |
dc.audience | Scientific | |
dc.subject.free | atmospheric spectrometer (ILAS) | |
dc.subject.free | Ozone | |
dc.subject.free | Ozone losses by Bipolar Investigations (QUOBI) | |
dc.source.issue | Proceedings of the XX Quadrennial Ozone Symposium, 1-8 June 2004, Kos, Greece, Edt. C.S. Zerefos, | |
dc.source.page | pp. 614-615 | |
Orfeo.peerreviewed | Not pertinent |
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