Chemistry-climate model SOCOL: a validation of the present-day climatology
International audience In this paper we document "SOCOL", a new chemistry-climate model, which has been ported for regular PCs and shows good wall-clock performance. An extensive validation of the model results against present-day climate data obtained from observations and assimilation da...
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ftinsu:oai:HAL:hal-00295679v1 2023-11-12T04:24:55+01:00 Chemistry-climate model SOCOL: a validation of the present-day climatology Egorova, T. Rozanov, E. Zubov, V. Manzini, E. Schmutz, W. Peter, T. Physikalisch-Meteorologisches Observatorium Davos/World Radiation Center (PMOD/WRC) Institute for Atmospheric and Climate Science Zürich (IAC) Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich) Main Astronomical Observatory of NAS of Ukraine (MAO) National Academy of Sciences of Ukraine (NASU) Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Bologna (INGV) Istituto Nazionale di Geofisica e Vulcanologia 2005-06-21 https://hal.science/hal-00295679 https://hal.science/hal-00295679/document https://hal.science/hal-00295679/file/acp-5-1557-2005.pdf en eng HAL CCSD European Geosciences Union hal-00295679 https://hal.science/hal-00295679 https://hal.science/hal-00295679/document https://hal.science/hal-00295679/file/acp-5-1557-2005.pdf info:eu-repo/semantics/OpenAccess ISSN: 1680-7316 EISSN: 1680-7324 Atmospheric Chemistry and Physics https://hal.science/hal-00295679 Atmospheric Chemistry and Physics, 2005, 5 (6), pp.1557-1576 [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2005 ftinsu 2023-10-25T16:29:59Z International audience In this paper we document "SOCOL", a new chemistry-climate model, which has been ported for regular PCs and shows good wall-clock performance. An extensive validation of the model results against present-day climate data obtained from observations and assimilation data sets shows that the model describes the climatological state of the atmosphere for the late 1990s with reasonable accuracy. The model has a significant temperature bias only in the upper stratosphere and near the tropopause at high latitudes. The latter is the result of the rather low vertical resolution of the model near the tropopause. The former can be attributed to a crude representation of radiation heating in the middle atmosphere. A comparison of the simulated and observed link between the tropical stratospheric structure and the strength of the polar vortex shows that in general, both observations and simulations reveal a higher temperature and ozone mixing ratio in the lower tropical stratosphere for the case with stronger Polar night jet (PNJ) and slower Brewer-Dobson circulation as predicted by theoretical studies. Article in Journal/Newspaper polar night Institut national des sciences de l'Univers: HAL-INSU |
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Open Polar |
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Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere |
spellingShingle |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere Egorova, T. Rozanov, E. Zubov, V. Manzini, E. Schmutz, W. Peter, T. Chemistry-climate model SOCOL: a validation of the present-day climatology |
topic_facet |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere |
description |
International audience In this paper we document "SOCOL", a new chemistry-climate model, which has been ported for regular PCs and shows good wall-clock performance. An extensive validation of the model results against present-day climate data obtained from observations and assimilation data sets shows that the model describes the climatological state of the atmosphere for the late 1990s with reasonable accuracy. The model has a significant temperature bias only in the upper stratosphere and near the tropopause at high latitudes. The latter is the result of the rather low vertical resolution of the model near the tropopause. The former can be attributed to a crude representation of radiation heating in the middle atmosphere. A comparison of the simulated and observed link between the tropical stratospheric structure and the strength of the polar vortex shows that in general, both observations and simulations reveal a higher temperature and ozone mixing ratio in the lower tropical stratosphere for the case with stronger Polar night jet (PNJ) and slower Brewer-Dobson circulation as predicted by theoretical studies. |
author2 |
Physikalisch-Meteorologisches Observatorium Davos/World Radiation Center (PMOD/WRC) Institute for Atmospheric and Climate Science Zürich (IAC) Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich) Main Astronomical Observatory of NAS of Ukraine (MAO) National Academy of Sciences of Ukraine (NASU) Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Bologna (INGV) Istituto Nazionale di Geofisica e Vulcanologia |
format |
Article in Journal/Newspaper |
author |
Egorova, T. Rozanov, E. Zubov, V. Manzini, E. Schmutz, W. Peter, T. |
author_facet |
Egorova, T. Rozanov, E. Zubov, V. Manzini, E. Schmutz, W. Peter, T. |
author_sort |
Egorova, T. |
title |
Chemistry-climate model SOCOL: a validation of the present-day climatology |
title_short |
Chemistry-climate model SOCOL: a validation of the present-day climatology |
title_full |
Chemistry-climate model SOCOL: a validation of the present-day climatology |
title_fullStr |
Chemistry-climate model SOCOL: a validation of the present-day climatology |
title_full_unstemmed |
Chemistry-climate model SOCOL: a validation of the present-day climatology |
title_sort |
chemistry-climate model socol: a validation of the present-day climatology |
publisher |
HAL CCSD |
publishDate |
2005 |
url |
https://hal.science/hal-00295679 https://hal.science/hal-00295679/document https://hal.science/hal-00295679/file/acp-5-1557-2005.pdf |
genre |
polar night |
genre_facet |
polar night |
op_source |
ISSN: 1680-7316 EISSN: 1680-7324 Atmospheric Chemistry and Physics https://hal.science/hal-00295679 Atmospheric Chemistry and Physics, 2005, 5 (6), pp.1557-1576 |
op_relation |
hal-00295679 https://hal.science/hal-00295679 https://hal.science/hal-00295679/document https://hal.science/hal-00295679/file/acp-5-1557-2005.pdf |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1782339368063598592 |