Research output: Contribution to journal › Article
Ground-Based Measurements of Total Ozone Content by the Infrared Method. / Virolainen, Ya. A.; Timofeev, Yu. M.; Ionov, D. V.; Poberovskii, A. V.; Shalamyanskii, A. M.
In: IZVESTIYA. ATMOSPHERIC AND OCEANIC PHYSICS, Vol. 47, No. 4, 2011, p. 480-490.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Ground-Based Measurements of Total Ozone Content by the Infrared Method
AU - Virolainen, Ya. A.
AU - Timofeev, Yu. M.
AU - Ionov, D. V.
AU - Poberovskii, A. V.
AU - Shalamyanskii, A. M.
PY - 2011
Y1 - 2011
N2 - To interpret the ground-based measurements of the spectra of direct solar infrared radiation with the help of a Brucker Fourier-spectrometer, a technique for determining the total ozone content (TOC) was developed and implemented. The TOC was determined using six spectral intervals of an ozone-absorption band of 9.6 m and the shortwave panel of a carbon-dioxide-absorption band of 15 m, where the impact of other atmospheric parameters on the measured solar radiation was reduced to a minimum. The potential errors of the infrared method for determining the TOC for the chosen spectral scheme with the influence of measurement errors and vertical profiles of temperature are less than 1% for different signal-to-noise ratios and zenith angles of the sun. We analyzed 269 high-resolution (0.005–0.008 cm–1) spectra of solar infrared radiation measured in Peterhof over 52 days from March to November, 2009. The resulting values of TOC were compared with the results of independent ground-based TOC measurements in
AB - To interpret the ground-based measurements of the spectra of direct solar infrared radiation with the help of a Brucker Fourier-spectrometer, a technique for determining the total ozone content (TOC) was developed and implemented. The TOC was determined using six spectral intervals of an ozone-absorption band of 9.6 m and the shortwave panel of a carbon-dioxide-absorption band of 15 m, where the impact of other atmospheric parameters on the measured solar radiation was reduced to a minimum. The potential errors of the infrared method for determining the TOC for the chosen spectral scheme with the influence of measurement errors and vertical profiles of temperature are less than 1% for different signal-to-noise ratios and zenith angles of the sun. We analyzed 269 high-resolution (0.005–0.008 cm–1) spectra of solar infrared radiation measured in Peterhof over 52 days from March to November, 2009. The resulting values of TOC were compared with the results of independent ground-based TOC measurements in
KW - ozonometry
KW - spectroscopic measurements
KW - remote sensing
KW - atmosphere.
U2 - DOI: 10.1134/S0001433811040104
DO - DOI: 10.1134/S0001433811040104
M3 - статья
VL - 47
SP - 480
EP - 490
JO - Izvestiya - Atmospheric and Oceanic Physics
JF - Izvestiya - Atmospheric and Oceanic Physics
SN - 0001-4338
IS - 4
ER -
ID: 5196892