Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › Research › peer-review
Assessment of the ozone and temperature variability during 1979-1993 with the chemistry-climate model SOCOL. / Rozanov, E; Schraner, M; Schnadt, C; Wild, M; Ohmura, A; Schmutz, W; Peter, T; Зубов, Владимир Аркадьевич.
GREENHOUSE GASES, OZONE, AND ELECTRODYNAMICS; THEIR CHANGES IN THE MIDDLE ATMOSPHERE AND LOWER THERMOSPHERE. ed. / DK Chakrabarty; SP Gupta. Elsevier, 2005. p. 1375-1384 (ADVANCES IN SPACE RESEARCH-SERIES; Vol. 35).Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › Research › peer-review
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TY - GEN
T1 - Assessment of the ozone and temperature variability during 1979-1993 with the chemistry-climate model SOCOL
AU - Rozanov, E
AU - Schraner, M
AU - Schnadt, C
AU - Wild, M
AU - Ohmura, A
AU - Schmutz, W
AU - Peter, T
AU - Зубов, Владимир Аркадьевич
PY - 2005
Y1 - 2005
N2 - The chemistry-climate model SOCOL has been applied for the study of ozone and temperature anomalies during 1979-1993. Temperature and ozone anomalies have been obtained for a set of model runs forced by all major stratospheric forcing mechanisms. Forcings have been prescribed separately and together to assess their individual influence oil stratospheric ozone and temperature. The results of these simulations have been compared to available satellite data. The model captures well ozone depletion and cooling in the upper stratosphere due to increases in the abundance of greenhouse gases and ozone depleting substances in the atmosphere. In the lower stratosphere, the model reproduces the warming over tropical and middle latitudes caused by the El-Chichon and Pinatubo eruptions. However, the simulated ozone response is overestimated in comparison with SAGE data. The best agreement with observations has been obtained for the run with all forcings included. This emphasizes the importance of the volcanic and solar forcings for the correct reproduction of observed trends. Comparison of near-global total ozone anomalies confirms an overestimation of ozone depletion just after volcanic eruptions, while the overall agreement with the model is fairly good. (c) 2005 COSPAR. Published by Elsevier Ltd. All rights reserved.
AB - The chemistry-climate model SOCOL has been applied for the study of ozone and temperature anomalies during 1979-1993. Temperature and ozone anomalies have been obtained for a set of model runs forced by all major stratospheric forcing mechanisms. Forcings have been prescribed separately and together to assess their individual influence oil stratospheric ozone and temperature. The results of these simulations have been compared to available satellite data. The model captures well ozone depletion and cooling in the upper stratosphere due to increases in the abundance of greenhouse gases and ozone depleting substances in the atmosphere. In the lower stratosphere, the model reproduces the warming over tropical and middle latitudes caused by the El-Chichon and Pinatubo eruptions. However, the simulated ozone response is overestimated in comparison with SAGE data. The best agreement with observations has been obtained for the run with all forcings included. This emphasizes the importance of the volcanic and solar forcings for the correct reproduction of observed trends. Comparison of near-global total ozone anomalies confirms an overestimation of ozone depletion just after volcanic eruptions, while the overall agreement with the model is fairly good. (c) 2005 COSPAR. Published by Elsevier Ltd. All rights reserved.
KW - ozone
KW - temperature
KW - stratosphere
KW - variability
KW - modeling
KW - DOPPLER-SPREAD PARAMETERIZATION
KW - WAVE MOMENTUM DEPOSITION
KW - MIDDLE-ATMOSPHERE
KW - TRENDS
KW - SIMULATION
KW - DEPLETION
U2 - 10.1016/j.asr.2005.05.003
DO - 10.1016/j.asr.2005.05.003
M3 - статья в сборнике материалов конференции
SN - *************
T3 - ADVANCES IN SPACE RESEARCH-SERIES
SP - 1375
EP - 1384
BT - GREENHOUSE GASES, OZONE, AND ELECTRODYNAMICS; THEIR CHANGES IN THE MIDDLE ATMOSPHERE AND LOWER THERMOSPHERE
A2 - Chakrabarty, DK
A2 - Gupta, SP
PB - Elsevier
Y2 - 18 July 2004 through 25 July 2004
ER -
ID: 121595511