http://www.cnr.it/ontology/cnr/individuo/prodotto/ID173263
Geophysical validation of temperature retrieved by the ESA Level 2 processor from MIPAS/ENVISAT measurements (Contributo in atti di convegno)
- Type
- Label
- Geophysical validation of temperature retrieved by the ESA Level 2 processor from MIPAS/ENVISAT measurements (Contributo in atti di convegno) (literal)
- Anno
- 2006-01-01T00:00:00+01:00 (literal)
- Alternative label
M. Ridolfi, U. Blum, B. Carli, V. Catoire, S. Ceccherini, C. Cornacchia, C.De Clercq, K. H. Fricke, M. Iarlori, B. Kerridge, M. Kiefer, J.-C. Lambert, Y. Meijer, L. Mona, H. Oelhaf, G. Pappalardo, C. Piccolo, M. Pirre, P.Raspollini, V. Rizi, et al. (2006)
Geophysical validation of temperature retrieved by the ESA Level 2 processor from MIPAS/ENVISAT measurements
in Atmospheric Science Conference, Frascati, 8-12 maggio 2006
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- M. Ridolfi, U. Blum, B. Carli, V. Catoire, S. Ceccherini, C. Cornacchia, C.De Clercq, K. H. Fricke, M. Iarlori, B. Kerridge, M. Kiefer, J.-C. Lambert, Y. Meijer, L. Mona, H. Oelhaf, G. Pappalardo, C. Piccolo, M. Pirre, P.Raspollini, V. Rizi, et al. (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#titoloVolume
- Proceedings of the First Conference on Atmospheric Science (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#volumeInCollana
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#note
- Proceedings di Atmospheric Science Conference, ESA-ESRIN Frascati, Italy, 8-12 Maggio 2006,SP-628 (July 2006). (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Dipartimento di Chimica Fisica e Inorganica, Università di Bologna, Italy
Fraunhofer-Institut für Naturwissenschaftlich-Technische Trendanalysen, Euskirchen, Germany
Istituto di Fisica Applicata \"Nello Carrara\", CNR, Firenze (Italy)
Laboratoire de Physique et Chimie de l'Environnement, CNRS Université d'Orleans, Orleans, France
DWD, Observatory Hohenpeissenberg, Germany
Institut d'Aéronomie Spatiale de Belgique, Bruxelles, Belgique
Physikalisches Institut, Universität Bonn, Bonn, Germany
Dipartimento di Fisica, Università de L'Aquila, L'aquila, Italy
Service d'Aeronomie Institut Pierre Simon Laplace/UVSQ, Verrieres-Le-Buisson, France
Earth Observation and Atmospheric Science, Space Science and Technology Department, RAL, Oxfordshire, UK
National Institute for Public Health and the Environment, RIVM LVM, Bilthoven, The Netherlands
Istituto di Metodologie per lAnalisi Ambientale, CNR, Tito Scalo, Potenza, Italy
Forschungszentrum Karlsruhe, IMK, Germany (literal)
- Titolo
- Geophysical validation of temperature retrieved by the ESA Level 2 processor from MIPAS/ENVISAT measurements (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#isbn
- Abstract
- The Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) is operating on the ESA ENVIronmental
SATellite since March 2002. The high resolution (0.025 cm-1) limb-emission measurements acquired by MIPAS in the
first two years of operations constitute a self-consistent set of data with very good geographical and time coverage.
These measurements have been re-processed by ESA up to Level 2, with the most recent versions of both Level 1b and
Level 2 algorithms. The products of the ESA Level 2 algorithm are geolocated profiles of temperature and of volume
mixing ratio of six key atmospheric constituents: H2O, O3, HNO3, CH4, N2O and NO2. As for all the measurements
made with innovative instruments and techniques, this data set requires a thorough validation.
During the last year, a large team of scientists spent great efforts in the validation of this data set. In particular, the
authors of this paper have focused their activities on the validation of temperature. The validation was carried-out by
comparing MIPAS retrieved temperature with correlative measurements made by radiosondes, lidars, in-situ and remote
sensors operated either from stratospheric balloons or satellites. Preliminary results show that MIPAS profiles are
affected by a bias generally consistent with their a-priori estimated systematic error component. This bias is usually
localized at the edges of the altitude range covered by the MIPAS scan (6 - 68 km). (literal)
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