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VLIYANIE AEROZOLYA NA FORMIROVANIE UKHODYASHCHEGO TEPLOVOGO IZLUCHENIYA. / Timofeev, Yu M.; Obraztsov, S. P.

In: Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana, Vol. 20, No. 10, 01.10.1984, p. 947-956.

Research output: Contribution to journal › Article › peer-review

Harvard

Timofeev, YM & Obraztsov, SP 1984, 'VLIYANIE AEROZOLYA NA FORMIROVANIE UKHODYASHCHEGO TEPLOVOGO IZLUCHENIYA.', Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana, vol. 20, no. 10, pp. 947-956.

APA

Timofeev, Y. M., & Obraztsov, S. P. (1984). VLIYANIE AEROZOLYA NA FORMIROVANIE UKHODYASHCHEGO TEPLOVOGO IZLUCHENIYA. Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana, 20(10), 947-956.

Vancouver

Timofeev YM, Obraztsov SP. VLIYANIE AEROZOLYA NA FORMIROVANIE UKHODYASHCHEGO TEPLOVOGO IZLUCHENIYA. Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana. 1984 Oct 1;20(10):947-956.

Author

Timofeev, Yu M. ; Obraztsov, S. P. / VLIYANIE AEROZOLYA NA FORMIROVANIE UKHODYASHCHEGO TEPLOVOGO IZLUCHENIYA. In: Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana. 1984 ; Vol. 20, No. 10. pp. 947-956.

BibTeX

@article{47682fed32a546ddbd732ec33a068258,
title = "VLIYANIE AEROZOLYA NA FORMIROVANIE UKHODYASHCHEGO TEPLOVOGO IZLUCHENIYA.",
abstract = "On the basis of a solution of the integrodifferential equation for radiation transport, a study is made of the effect of aerosol on the formation of outgoing thermal radiation in the 400-2685 cm** minus **1 range for aerosol models of various shapes. It is shown that the effect of the aerosol on the brightness temperature of radiation can amount to 0. 1-0. 4 K for a pure atmosphere and to 2-4 K for a turbid atmosphere. The contribution of aerosol scattering to the formation of outgoing thermal radiation can amount to 5-10%. An approximate method of taking the effect of aerosol into account is proposed.",
author = "Timofeev, {Yu M.} and Obraztsov, {S. P.}",
year = "1984",
month = oct,
day = "1",
language = "русский",
volume = "20",
pages = "947--956",
journal = "Izvestiya - Atmospheric and Oceanic Physics",
issn = "0001-4338",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "10",

}

RIS

TY - JOUR

T1 - VLIYANIE AEROZOLYA NA FORMIROVANIE UKHODYASHCHEGO TEPLOVOGO IZLUCHENIYA.

AU - Timofeev, Yu M.

AU - Obraztsov, S. P.

PY - 1984/10/1

Y1 - 1984/10/1

N2 - On the basis of a solution of the integrodifferential equation for radiation transport, a study is made of the effect of aerosol on the formation of outgoing thermal radiation in the 400-2685 cm** minus **1 range for aerosol models of various shapes. It is shown that the effect of the aerosol on the brightness temperature of radiation can amount to 0. 1-0. 4 K for a pure atmosphere and to 2-4 K for a turbid atmosphere. The contribution of aerosol scattering to the formation of outgoing thermal radiation can amount to 5-10%. An approximate method of taking the effect of aerosol into account is proposed.

AB - On the basis of a solution of the integrodifferential equation for radiation transport, a study is made of the effect of aerosol on the formation of outgoing thermal radiation in the 400-2685 cm** minus **1 range for aerosol models of various shapes. It is shown that the effect of the aerosol on the brightness temperature of radiation can amount to 0. 1-0. 4 K for a pure atmosphere and to 2-4 K for a turbid atmosphere. The contribution of aerosol scattering to the formation of outgoing thermal radiation can amount to 5-10%. An approximate method of taking the effect of aerosol into account is proposed.

UR - http://www.scopus.com/inward/record.url?scp=0021507280&partnerID=8YFLogxK

M3 - статья

AN - SCOPUS:0021507280

VL - 20

SP - 947

EP - 956

JO - Izvestiya - Atmospheric and Oceanic Physics

JF - Izvestiya - Atmospheric and Oceanic Physics

SN - 0001-4338

IS - 10

ER -

ID: 51564571