Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Possibilities for determining the vertical structure of ozone content from ground-based measurements of IR radiation. / Virolainen, Ya A.; Polyakov, A. V.; Timofeev, Yu M.
в: Izvestiya - Atmospheric and Ocean Physics, Том 33, № 4, 01.12.1997, стр. 427-430.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Possibilities for determining the vertical structure of ozone content from ground-based measurements of IR radiation
AU - Virolainen, Ya A.
AU - Polyakov, A. V.
AU - Timofeev, Yu M.
PY - 1997/12/1
Y1 - 1997/12/1
N2 - A possibility for determining the ozone vertical distribution in the earth's atmosphere from groundbased measurements of downward atmospheric radiation in the spectral region of the 9.6-nm ozone absorption band is studied. A measuring instrument of the Fourier-interferometer type with a spectral resolution of about 0.2-0.5 cm-1 is considered. It is shown that satisfactory estimates of the potential accuracy of determination of the ozone content in the troposphere and the stratosphere can be obtained with the known profiles of atmospheric temperature and moisture content. The error in determination of the total ozone content is found to be 4-5% in the troposphere, 2-3% in the stratosphere, and 2-3% in the entire atmosphere.
AB - A possibility for determining the ozone vertical distribution in the earth's atmosphere from groundbased measurements of downward atmospheric radiation in the spectral region of the 9.6-nm ozone absorption band is studied. A measuring instrument of the Fourier-interferometer type with a spectral resolution of about 0.2-0.5 cm-1 is considered. It is shown that satisfactory estimates of the potential accuracy of determination of the ozone content in the troposphere and the stratosphere can be obtained with the known profiles of atmospheric temperature and moisture content. The error in determination of the total ozone content is found to be 4-5% in the troposphere, 2-3% in the stratosphere, and 2-3% in the entire atmosphere.
UR - http://www.scopus.com/inward/record.url?scp=0002978706&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:0002978706
VL - 33
SP - 427
EP - 430
JO - Izvestiya, Atmospheric and Oceanic Physics
JF - Izvestiya, Atmospheric and Oceanic Physics
SN - 0001-4338
IS - 4
ER -
ID: 36157229