Esko Kyrö, Florence Goutail, Manuel Gil, Valery Dorokhov, G. Held, P. Eriksen, R. Evans, François Hendrick, Dmitry V. Ionov, Andrea Pazmino, M. Van Roozendael, Jean-Pierre Pommereau, Belgian Inst Space Aeron BIRA IASB, CNRS, Univ Versailles St Quentin, Natl Ocean & Atmospher Adm NOAA, St Petersburg State Univ, Finnish Meteorol Inst FMI, Universidade Estadual Paulista (Unesp), Danish Meteorol Inst, Cent Aerol Observ, Inst Tecn Aerospacial INTA, Belgian Institute for Space Aeronomy / Institut d'Aéronomie Spatiale de Belgique (BIRA-IASB), STRATO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), NOAA Earth System Research Laboratory (ESRL), National Oceanic and Atmospheric Administration (NOAA), V.A. Fock Institute of Physics (NIF), St Petersburg State University (SPbU), Finnish Meteorological Institute (FMI), Instituto de Pesquisas Meteorológicas (IPMet), Universidade Estadual Paulista Júlio de Mesquita Filho = São Paulo State University (UNESP), Danish Meteorological Institute (DMI), Central Aerological Observatory (CAO), Russian Federal Service for Hydrometeorology and Environmental Monitoring (Roshydromet), and Instituto Nacional de Técnica Aeroespacial (INTA)
Made available in DSpace on 2013-08-28T14:11:56Z (GMT). No. of bitstreams: 1 WOS000292183400004.pdf: 4179321 bytes, checksum: 4244a6184542ca360e9f7148b60e061e (MD5) Made available in DSpace on 2013-09-30T19:23:07Z (GMT). No. of bitstreams: 2 WOS000292183400004.pdf: 4179321 bytes, checksum: 4244a6184542ca360e9f7148b60e061e (MD5) WOS000292183400004.pdf.txt: 99323 bytes, checksum: 83dfb242aa73c3c29d166c8d826e9aca (MD5) Previous issue date: 2011-01-01 Submitted by Vitor Silverio Rodrigues (vitorsrodrigues@reitoria.unesp.br) on 2014-05-20T15:34:05Z No. of bitstreams: 2 WOS000292183400004.pdf: 4179321 bytes, checksum: 4244a6184542ca360e9f7148b60e061e (MD5) WOS000292183400004.pdf.txt: 99323 bytes, checksum: 83dfb242aa73c3c29d166c8d826e9aca (MD5) Made available in DSpace on 2014-05-20T15:34:05Z (GMT). No. of bitstreams: 2 WOS000292183400004.pdf: 4179321 bytes, checksum: 4244a6184542ca360e9f7148b60e061e (MD5) WOS000292183400004.pdf.txt: 99323 bytes, checksum: 83dfb242aa73c3c29d166c8d826e9aca (MD5) Previous issue date: 2011-01-01 ESA Multi-Taste EC GEOmon Belgian PRODEX SECPEA projects Accurate long-term monitoring of total ozone is one of the most important requirements for identifying possible natural or anthropogenic changes in the composition of the stratosphere. For this purpose, the NDACC (Network for the Detection of Atmospheric Composition Change) UV-visible Working Group has made recommendations for improving and homogenizing the retrieval of total ozone columns from twilight zenith-sky visible spectrometers. These instruments, deployed all over the world in about 35 stations, allow measuring total ozone twice daily with limited sensitivity to stratospheric temperature and cloud cover. The NDACC recommendations address both the DOAS spectral parameters and the calculation of air mass factors (AMF) needed for the conversion of O-3 slant column densities into vertical column amounts. The most important improvement is the use of O-3 AMF look-up tables calculated using the TOMS V8 (TV8) O-3 profile climatology, that allows accounting for the dependence of the O-3 AMF on the seasonal and latitudinal variations of the O-3 vertical distribution. To investigate their impact on the retrieved ozone columns, the recommendations have been applied to measurements from the NDACC/SAOZ (Systeme d'Analyse par Observation Zenithale) network. The revised SAOZ ozone data from eight stations deployed at all latitudes have been compared to TOMS, GOMEGDP4, SCIAMACHY-TOSOMI, SCIAMACHY-OL3, OMI-TOMS, and OMI-DOAS satellite overpass observations, as well as to those of collocated Dobson and Brewer instruments at Observatoire de Haute Provence (44 degrees N, 5.5 degrees E) and Sodankyla (67 degrees N, 27 degrees E), respectively. A significantly better agreement is obtained between SAOZ and correlative reference ground-based measurements after applying the new O-3 AMFs. However, systematic seasonal differences between SAOZ and satellite instruments remain. These are shown to mainly originate from (i) a possible problem in the satellite retrieval algorithms in dealing with the temperature dependence of the ozone cross-sections in the UV and the solar zenith angle (SZA) dependence, (ii) zonal modulations and seasonal variations of tropospheric ozone columns not accounted for in the TV8 profile climatology, and (iii) uncertainty on the stratospheric ozone profiles at high latitude in the winter in the TV8 climatology. For those measurements mostly sensitive to stratospheric temperature like TOMS, OMI-TOMS, Dobson and Brewer, or to SZA like SCIAMACHY-TOSOMI, the application of temperature and SZA corrections results in the almost complete removal of the seasonal difference with SAOZ, improving significantly the consistency between all ground-based and satellite total ozone observations. Belgian Inst Space Aeron BIRA IASB, Brussels, Belgium CNRS, LATMOS, Guyancourt, France Univ Versailles St Quentin, Guyancourt, France Natl Ocean & Atmospher Adm NOAA, Global Monitoring Div, Earth Syst Res Lab, Boulder, CO USA St Petersburg State Univ, Inst Phys Res, Dept Atmospher Phys, St Petersburg, Russia Finnish Meteorol Inst FMI, Arctic Res Ctr, Sodankyla, Finland Univ Estadual Paulista, Meteorol Res Inst, Bauru, SP, Brazil Danish Meteorol Inst, Copenhagen, Denmark Cent Aerol Observ, Moscow, Russia Inst Tecn Aerospacial INTA, Torrejon de Ardoz, Spain Univ Estadual Paulista, Meteorol Res Inst, Bauru, SP, Brazil