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Feedbacks in one-dimensional climatic models with cloud formation block. / Kostsov, V. S.; Rozanov, V. V.; Rozanov, Y. V.; Selyakov, T. I.

In: Izvestiya - Atmospheric and Oceanic Physics, Vol. 30, No. 4, 01.12.1995, p. 541-546.

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

Harvard

Kostsov, VS, Rozanov, VV, Rozanov, YV & Selyakov, TI 1995, 'Feedbacks in one-dimensional climatic models with cloud formation block', Izvestiya - Atmospheric and Oceanic Physics, vol. 30, no. 4, pp. 541-546.

APA

Kostsov, V. S., Rozanov, V. V., Rozanov, Y. V., & Selyakov, T. I. (1995). Feedbacks in one-dimensional climatic models with cloud formation block. Izvestiya - Atmospheric and Oceanic Physics, 30(4), 541-546.

Vancouver

Kostsov VS, Rozanov VV, Rozanov YV, Selyakov TI. Feedbacks in one-dimensional climatic models with cloud formation block. Izvestiya - Atmospheric and Oceanic Physics. 1995 Dec 1;30(4):541-546.

Author

Kostsov, V. S. ; Rozanov, V. V. ; Rozanov, Y. V. ; Selyakov, T. I. / Feedbacks in one-dimensional climatic models with cloud formation block. In: Izvestiya - Atmospheric and Oceanic Physics. 1995 ; Vol. 30, No. 4. pp. 541-546.

BibTeX

@article{20fb6d29634b40d4b1c3aca3b1cf0b47,
title = "Feedbacks in one-dimensional climatic models with cloud formation block",
abstract = "The study of feedback mechanisms caused by changes in the water vapor, the lapse rate in the troposphere, and cloudiness is carried out with the aid of the 1D radiative-dynamic climate model. The climate warming due to doubling of the CO2 and a 2% rise in the solar constant is calculated with use of this model. The resulting values of underlying surface heating do not exceed 1.0 K, which is much smaller than those obtained in the framework of the standard 1D radiative-convective models. The results also demonstrate a decrease in the vertical size and the liquid-water content for clouds of the lower layer and, therefore, a decrease in their optical thickness.",
author = "Kostsov, {V. S.} and Rozanov, {V. V.} and Rozanov, {Y. V.} and Selyakov, {T. I.}",
year = "1995",
month = dec,
day = "1",
language = "English",
volume = "30",
pages = "541--546",
journal = "Izvestiya, Atmospheric and Oceanic Physics",
issn = "0001-4338",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "4",

}

RIS

TY - JOUR

T1 - Feedbacks in one-dimensional climatic models with cloud formation block

AU - Kostsov, V. S.

AU - Rozanov, V. V.

AU - Rozanov, Y. V.

AU - Selyakov, T. I.

PY - 1995/12/1

Y1 - 1995/12/1

N2 - The study of feedback mechanisms caused by changes in the water vapor, the lapse rate in the troposphere, and cloudiness is carried out with the aid of the 1D radiative-dynamic climate model. The climate warming due to doubling of the CO2 and a 2% rise in the solar constant is calculated with use of this model. The resulting values of underlying surface heating do not exceed 1.0 K, which is much smaller than those obtained in the framework of the standard 1D radiative-convective models. The results also demonstrate a decrease in the vertical size and the liquid-water content for clouds of the lower layer and, therefore, a decrease in their optical thickness.

AB - The study of feedback mechanisms caused by changes in the water vapor, the lapse rate in the troposphere, and cloudiness is carried out with the aid of the 1D radiative-dynamic climate model. The climate warming due to doubling of the CO2 and a 2% rise in the solar constant is calculated with use of this model. The resulting values of underlying surface heating do not exceed 1.0 K, which is much smaller than those obtained in the framework of the standard 1D radiative-convective models. The results also demonstrate a decrease in the vertical size and the liquid-water content for clouds of the lower layer and, therefore, a decrease in their optical thickness.

UR - http://www.scopus.com/inward/record.url?scp=0029433132&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0029433132

VL - 30

SP - 541

EP - 546

JO - Izvestiya, Atmospheric and Oceanic Physics

JF - Izvestiya, Atmospheric and Oceanic Physics

SN - 0001-4338

IS - 4

ER -

ID: 34928931