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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.

в: IZVESTIYA. ATMOSPHERIC AND OCEANIC PHYSICS, Том 47, № 4, 2011, стр. 480-490.

Результаты исследований: Научные публикации в периодических изданиях › статья

Harvard

Virolainen, YA, Timofeev, YM, Ionov, DV, Poberovskii, AV & Shalamyanskii, AM 2011, 'Ground-Based Measurements of Total Ozone Content by the Infrared Method', IZVESTIYA. ATMOSPHERIC AND OCEANIC PHYSICS, Том. 47, № 4, стр. 480-490. https://doi.org/DOI: 10.1134/S0001433811040104

APA

Virolainen, Y. A., Timofeev, Y. M., Ionov, D. V., Poberovskii, A. V., & Shalamyanskii, A. M. (2011). Ground-Based Measurements of Total Ozone Content by the Infrared Method. IZVESTIYA. ATMOSPHERIC AND OCEANIC PHYSICS, 47(4), 480-490. https://doi.org/DOI: 10.1134/S0001433811040104

Vancouver

Virolainen YA, Timofeev YM, Ionov DV, Poberovskii AV, Shalamyanskii AM. Ground-Based Measurements of Total Ozone Content by the Infrared Method. IZVESTIYA. ATMOSPHERIC AND OCEANIC PHYSICS. 2011;47(4):480-490. https://doi.org/DOI: 10.1134/S0001433811040104

Author

Virolainen, Ya. A. ; Timofeev, Yu. M. ; Ionov, D. V. ; Poberovskii, A. V. ; Shalamyanskii, A. M. / Ground-Based Measurements of Total Ozone Content by the Infrared Method. в: IZVESTIYA. ATMOSPHERIC AND OCEANIC PHYSICS. 2011 ; Том 47, № 4. стр. 480-490.

BibTeX

@article{adbb962278bb4f92b15b009bad67d03f,
title = "Ground-Based Measurements of Total Ozone Content by the Infrared Method",
abstract = "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",
keywords = "ozonometry, spectroscopic measurements, remote sensing, atmosphere.",
author = "Virolainen, {Ya. A.} and Timofeev, {Yu. M.} and Ionov, {D. V.} and Poberovskii, {A. V.} and Shalamyanskii, {A. M.}",
year = "2011",
doi = "DOI: 10.1134/S0001433811040104",
language = "не определен",
volume = "47",
pages = "480--490",
journal = "Izvestiya - Atmospheric and Oceanic Physics",
issn = "0001-4338",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "4",

}

RIS

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