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Chemical and dynamical response to the 11-year variability of the solar irradiance simulated with a chemistry-climate model. / Rozanov, E; Manzini, E; Haberreiter, M; Schmutz, W; Peter, T; Зубов, Владимир Аркадьевич; Egorova, Tatiana.

In: Geophysical Research Letters, Vol. 31, No. 6, 06119, 24.03.2004.

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

Harvard

Rozanov, E, Manzini, E, Haberreiter, M, Schmutz, W, Peter, T, Зубов, ВА & Egorova, T 2004, 'Chemical and dynamical response to the 11-year variability of the solar irradiance simulated with a chemistry-climate model', Geophysical Research Letters, vol. 31, no. 6, 06119. https://doi.org/10.1029/2003GL019294

APA

Rozanov, E., Manzini, E., Haberreiter, M., Schmutz, W., Peter, T., Зубов, В. А., & Egorova, T. (2004). Chemical and dynamical response to the 11-year variability of the solar irradiance simulated with a chemistry-climate model. Geophysical Research Letters, 31(6), [06119]. https://doi.org/10.1029/2003GL019294

Vancouver

Rozanov E, Manzini E, Haberreiter M, Schmutz W, Peter T, Зубов ВА et al. Chemical and dynamical response to the 11-year variability of the solar irradiance simulated with a chemistry-climate model. Geophysical Research Letters. 2004 Mar 24;31(6). 06119. https://doi.org/10.1029/2003GL019294

Author

Rozanov, E ; Manzini, E ; Haberreiter, M ; Schmutz, W ; Peter, T ; Зубов, Владимир Аркадьевич ; Egorova, Tatiana. / Chemical and dynamical response to the 11-year variability of the solar irradiance simulated with a chemistry-climate model. In: Geophysical Research Letters. 2004 ; Vol. 31, No. 6.

BibTeX

@article{48bdba38385c497dafbbf62580ee6ec6,
title = "Chemical and dynamical response to the 11-year variability of the solar irradiance simulated with a chemistry-climate model",
abstract = "Atmospheric effects of the solar irradiance variations during 11-year solar cycle are investigated using a chemistry-climate model. The model is enhanced by a more detailed parameterization of the oxygen and ozone UV heating rates. The simulated ozone response to the imposed solar forcing shows a positive correlation in the tropical stratosphere and a negative correlation in the tropical mesosphere, in agreement with theoretical expectation. The model suggests an acceleration of the polar night jets in both hemispheres and a dipole structure in the temperature changes at high latitudes. The model results also show an alteration of the tropospheric circulation air resulting in a statistically significant warming of 1 K in the annual mean surface air temperature over North America and Siberia. This supports the idea of a solar-climate connection.",
keywords = "TROPOSPHERIC RESPONSE, CYCLE, PARAMETERIZATION, OSCILLATION, SIGNAL, IMPACT",
author = "E Rozanov and E Manzini and M Haberreiter and W Schmutz and T Peter and Зубов, {Владимир Аркадьевич} and Tatiana Egorova",
year = "2004",
month = mar,
day = "24",
doi = "10.1029/2003GL019294",
language = "Английский",
volume = "31",
journal = "Geophysical Research Letters",
issn = "0094-8276",
publisher = "American Geophysical Union",
number = "6",

}

RIS

TY - JOUR

T1 - Chemical and dynamical response to the 11-year variability of the solar irradiance simulated with a chemistry-climate model

AU - Rozanov, E

AU - Manzini, E

AU - Haberreiter, M

AU - Schmutz, W

AU - Peter, T

AU - Зубов, Владимир Аркадьевич

AU - Egorova, Tatiana

PY - 2004/3/24

Y1 - 2004/3/24

N2 - Atmospheric effects of the solar irradiance variations during 11-year solar cycle are investigated using a chemistry-climate model. The model is enhanced by a more detailed parameterization of the oxygen and ozone UV heating rates. The simulated ozone response to the imposed solar forcing shows a positive correlation in the tropical stratosphere and a negative correlation in the tropical mesosphere, in agreement with theoretical expectation. The model suggests an acceleration of the polar night jets in both hemispheres and a dipole structure in the temperature changes at high latitudes. The model results also show an alteration of the tropospheric circulation air resulting in a statistically significant warming of 1 K in the annual mean surface air temperature over North America and Siberia. This supports the idea of a solar-climate connection.

AB - Atmospheric effects of the solar irradiance variations during 11-year solar cycle are investigated using a chemistry-climate model. The model is enhanced by a more detailed parameterization of the oxygen and ozone UV heating rates. The simulated ozone response to the imposed solar forcing shows a positive correlation in the tropical stratosphere and a negative correlation in the tropical mesosphere, in agreement with theoretical expectation. The model suggests an acceleration of the polar night jets in both hemispheres and a dipole structure in the temperature changes at high latitudes. The model results also show an alteration of the tropospheric circulation air resulting in a statistically significant warming of 1 K in the annual mean surface air temperature over North America and Siberia. This supports the idea of a solar-climate connection.

KW - TROPOSPHERIC RESPONSE

KW - CYCLE

KW - PARAMETERIZATION

KW - OSCILLATION

KW - SIGNAL

KW - IMPACT

U2 - 10.1029/2003GL019294

DO - 10.1029/2003GL019294

M3 - статья

VL - 31

JO - Geophysical Research Letters

JF - Geophysical Research Letters

SN - 0094-8276

IS - 6

M1 - 06119

ER -

ID: 121595739