http://www.cnr.it/ontology/cnr/individuo/prodotto/ID45460
Stratospheric NO2 trends over the high mountain Ottavio Vittori station, Italy (Articolo in rivista)
- Type
- Label
- Stratospheric NO2 trends over the high mountain Ottavio Vittori station, Italy (Articolo in rivista) (literal)
- Anno
- 2011-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1080/01431161.2010.517799 (literal)
- Alternative label
Kostadinov, I., A. Petritoli, G. Giovanelli, M. Premuda, D. Bortoli, S. Masieri, F. Ravegnani (2011)
Stratospheric NO2 trends over the high mountain Ottavio Vittori station, Italy
in International journal of remote sensing (Print); Taylor & Francis Group, London (Regno Unito)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Kostadinov, I., A. Petritoli, G. Giovanelli, M. Premuda, D. Bortoli, S. Masieri, F. Ravegnani (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#url
- http://dx.doi.org/10.1080/01431161.2010.517799 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Note
- ISI Web of Science (WOS) (literal)
- Scopus (literal)
- Elsevier (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Istituto di Scienze dell'Atmosfera e del Clima
University of Évora, Évora, Portugal (literal)
- Titolo
- Stratospheric NO2 trends over the high mountain Ottavio Vittori station, Italy (literal)
- Abstract
- This paper presents an evaluation of the nitrogen dioxide (NO 2 ) trend
inferred from UV-visible zenith-sky measurements performed at the 'Ottavio
Vittori' ground-based research station (www.isac.cnr.it/cimone) at Monte Cimone
(44.18 o N, 10.7 o E, 2165 m above sea level (a.s.l.)). Experimental data series are
obtained from the measured spectra adopting a retrieval procedure according to
differential optical absorption spectroscopy (DOAS) methodology. Data series
cover the period from 1993 to 2009, with limited interruptions due to technical
maintenance of the instrument or poor meteorological conditions. The NO 2
trends are calculated with a linear regression model considering different factors
assumed to contribute to NO 2 atmospheric content. Before running the model,
a procedure for data quality control was applied to reduce or exclude the influence
of measurements affected by poor meteorological conditions or the vertical
transport of polluted air masses from the lower troposphere. The negative trends
obtained for sunrise (a.m.) and sunset (p.m.) NO 2 measurements are in good agreement
with previous studies accomplished for ground-based stations in the northern
hemisphere. (literal)
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