Результаты исследований: Научные публикации в периодических изданиях › статья
Spectroscopic measurements of O3 and NO2 atmospheric content: Correction of ground-based method and comparison with satellite data. / Ionov, D.V.; Timofeyev, Y.M.; Poberovskii, A.V.
в: Atmospheric and Oceanic Optics, № 6, 2015, стр. 526-532.Результаты исследований: Научные публикации в периодических изданиях › статья
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TY - JOUR
T1 - Spectroscopic measurements of O3 and NO2 atmospheric content: Correction of ground-based method and comparison with satellite data
AU - Ionov, D.V.
AU - Timofeyev, Y.M.
AU - Poberovskii, A.V.
PY - 2015
Y1 - 2015
N2 - © 2015, Pleiades Publishing, Ltd.The results of daily observations of O3 and NO2 atmospheric total content near St. Petersburg retrieved from the automated ground-based measurements of zenith-sky scattered visible solar radiation are presented. The measurements of 2009–2013 are compared with the data of satellite measurements with the GOME (ERS-2), SCIAMACHY (ENVISAT), and OMI (AURA) satellite spectrometers. The analysis of differences revealed between the data of satellite and ground-based measurements allowed us to improve the ground-based method (DOAS technique) and decrease the average difference down to ~2 and ~20% for O3 and NO2, respectively. Remaining differences may be further decreased if the seasonal variability of air mass factors calculated is taken into account in the ground-based method.
AB - © 2015, Pleiades Publishing, Ltd.The results of daily observations of O3 and NO2 atmospheric total content near St. Petersburg retrieved from the automated ground-based measurements of zenith-sky scattered visible solar radiation are presented. The measurements of 2009–2013 are compared with the data of satellite measurements with the GOME (ERS-2), SCIAMACHY (ENVISAT), and OMI (AURA) satellite spectrometers. The analysis of differences revealed between the data of satellite and ground-based measurements allowed us to improve the ground-based method (DOAS technique) and decrease the average difference down to ~2 and ~20% for O3 and NO2, respectively. Remaining differences may be further decreased if the seasonal variability of air mass factors calculated is taken into account in the ground-based method.
U2 - 10.1134/S1024856015060068
DO - 10.1134/S1024856015060068
M3 - Article
SP - 526
EP - 532
JO - Atmospheric and Oceanic Optics
JF - Atmospheric and Oceanic Optics
SN - 1024-8560
IS - 6
ER -
ID: 4003923