Formation of solid particles in synoptic-scale Arctic PSCs in early winter 2002/2003
International audience Polar stratospheric clouds (PSC) have been observed in early winter (December 2002) during the SOLVE II/Vintresol campaign, both from balloons carrying comprehensive instrumentation for measurements of chemical composition, size distributions, and optical properties of the par...
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Other Authors: | , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2004
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Online Access: | https://hal.archives-ouvertes.fr/hal-00327870 https://hal.archives-ouvertes.fr/hal-00327870/document https://hal.archives-ouvertes.fr/hal-00327870/file/acpd-4-2485-2004.pdf |
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ftccsdartic:oai:HAL:hal-00327870v1 |
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Open Polar |
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Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere |
spellingShingle |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere Larsen, N. Knudsen, B. M. Svendsen, S. H. Deshler, T. Rosen, J. M. Kivi, R. Weisser, C. Schreiner, J. Mauerberger, K. Cairo, F. Ovarlez, J. Oelhaf, H. Spang, R. Formation of solid particles in synoptic-scale Arctic PSCs in early winter 2002/2003 |
topic_facet |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere |
description |
International audience Polar stratospheric clouds (PSC) have been observed in early winter (December 2002) during the SOLVE II/Vintresol campaign, both from balloons carrying comprehensive instrumentation for measurements of chemical composition, size distributions, and optical properties of the particles, as well as from individual backscatter soundings from Esrange and Sodankylä. The observations are unique in the sense that the PSC particles seem to have formed in the early winter under synoptic temperature conditions and not being influenced by mountain lee waves. A sequence of measurements during a 5-days period shows a gradual change between liquid and solid type PSCs with the development of a well-known sandwich structure. It appears that all PSC observations show the presence of a background population of solid particles, occasionally mixed in with more dominating liquid particles. The measurements have been compared with results from a detailed microphysical and optical simulation of the formation processes. Calculated extinction(indices) are in good agreement with SAGE-III measurements from the same period. Apparently the solid particles are controlled by the synoptic temperature history while the presence of liquid particles is controlled by the local temperatures at the time of observation. The temperature histories indicate that the solid particles are nucleated above the ice frost point, and a surface freezing mechanism for this is included in the model. Reducing the calculated freezing rates by a factor 10–20, the model is able to simulate the observed particle size distributions and reproduce observed HNO 3 gas phase concentrations. |
author2 |
Danish Meteorological Institute (DMI) University of Wyoming (UW) Finnish Meteorological Institute (FMI) Max-Planck-Institut für Kernphysik (MPIK) Max-Planck-Gesellschaft Istituto di Scienze dell'Atmosfera e del Clima (ISAC) Consiglio Nazionale delle Ricerche Roma (CNR) Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-École des Ponts ParisTech (ENPC)-École polytechnique (X)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC) Institute for Meteorology and Climate Research (IMK) Karlsruhe Institute of Technology (KIT) Institut für Chemie und Dynamik der Geosphäre - Stratosphäre (ICG-1) Forschungszentrum Jülich GmbH Helmholtz-Gemeinschaft = Helmholtz Association-Helmholtz-Gemeinschaft = Helmholtz Association |
format |
Article in Journal/Newspaper |
author |
Larsen, N. Knudsen, B. M. Svendsen, S. H. Deshler, T. Rosen, J. M. Kivi, R. Weisser, C. Schreiner, J. Mauerberger, K. Cairo, F. Ovarlez, J. Oelhaf, H. Spang, R. |
author_facet |
Larsen, N. Knudsen, B. M. Svendsen, S. H. Deshler, T. Rosen, J. M. Kivi, R. Weisser, C. Schreiner, J. Mauerberger, K. Cairo, F. Ovarlez, J. Oelhaf, H. Spang, R. |
author_sort |
Larsen, N. |
title |
Formation of solid particles in synoptic-scale Arctic PSCs in early winter 2002/2003 |
title_short |
Formation of solid particles in synoptic-scale Arctic PSCs in early winter 2002/2003 |
title_full |
Formation of solid particles in synoptic-scale Arctic PSCs in early winter 2002/2003 |
title_fullStr |
Formation of solid particles in synoptic-scale Arctic PSCs in early winter 2002/2003 |
title_full_unstemmed |
Formation of solid particles in synoptic-scale Arctic PSCs in early winter 2002/2003 |
title_sort |
formation of solid particles in synoptic-scale arctic pscs in early winter 2002/2003 |
publisher |
HAL CCSD |
publishDate |
2004 |
url |
https://hal.archives-ouvertes.fr/hal-00327870 https://hal.archives-ouvertes.fr/hal-00327870/document https://hal.archives-ouvertes.fr/hal-00327870/file/acpd-4-2485-2004.pdf |
long_lat |
ENVELOPE(21.117,21.117,67.883,67.883) ENVELOPE(26.600,26.600,67.417,67.417) |
geographic |
Arctic Esrange Sodankylä |
geographic_facet |
Arctic Esrange Sodankylä |
genre |
Arctic Sodankylä |
genre_facet |
Arctic Sodankylä |
op_source |
ISSN: 1680-7367 EISSN: 1680-7375 Atmospheric Chemistry and Physics Discussions https://hal.archives-ouvertes.fr/hal-00327870 Atmospheric Chemistry and Physics Discussions, European Geosciences Union, 2004, 4 (3), pp.2485-2512 |
op_relation |
hal-00327870 https://hal.archives-ouvertes.fr/hal-00327870 https://hal.archives-ouvertes.fr/hal-00327870/document https://hal.archives-ouvertes.fr/hal-00327870/file/acpd-4-2485-2004.pdf |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1766341452363726848 |
spelling |
ftccsdartic:oai:HAL:hal-00327870v1 2023-05-15T15:10:25+02:00 Formation of solid particles in synoptic-scale Arctic PSCs in early winter 2002/2003 Larsen, N. Knudsen, B. M. Svendsen, S. H. Deshler, T. Rosen, J. M. Kivi, R. Weisser, C. Schreiner, J. Mauerberger, K. Cairo, F. Ovarlez, J. Oelhaf, H. Spang, R. Danish Meteorological Institute (DMI) University of Wyoming (UW) Finnish Meteorological Institute (FMI) Max-Planck-Institut für Kernphysik (MPIK) Max-Planck-Gesellschaft Istituto di Scienze dell'Atmosfera e del Clima (ISAC) Consiglio Nazionale delle Ricerche Roma (CNR) Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-École des Ponts ParisTech (ENPC)-École polytechnique (X)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC) Institute for Meteorology and Climate Research (IMK) Karlsruhe Institute of Technology (KIT) Institut für Chemie und Dynamik der Geosphäre - Stratosphäre (ICG-1) Forschungszentrum Jülich GmbH Helmholtz-Gemeinschaft = Helmholtz Association-Helmholtz-Gemeinschaft = Helmholtz Association 2004-05-12 https://hal.archives-ouvertes.fr/hal-00327870 https://hal.archives-ouvertes.fr/hal-00327870/document https://hal.archives-ouvertes.fr/hal-00327870/file/acpd-4-2485-2004.pdf en eng HAL CCSD European Geosciences Union hal-00327870 https://hal.archives-ouvertes.fr/hal-00327870 https://hal.archives-ouvertes.fr/hal-00327870/document https://hal.archives-ouvertes.fr/hal-00327870/file/acpd-4-2485-2004.pdf info:eu-repo/semantics/OpenAccess ISSN: 1680-7367 EISSN: 1680-7375 Atmospheric Chemistry and Physics Discussions https://hal.archives-ouvertes.fr/hal-00327870 Atmospheric Chemistry and Physics Discussions, European Geosciences Union, 2004, 4 (3), pp.2485-2512 [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2004 ftccsdartic 2021-12-19T04:09:18Z International audience Polar stratospheric clouds (PSC) have been observed in early winter (December 2002) during the SOLVE II/Vintresol campaign, both from balloons carrying comprehensive instrumentation for measurements of chemical composition, size distributions, and optical properties of the particles, as well as from individual backscatter soundings from Esrange and Sodankylä. The observations are unique in the sense that the PSC particles seem to have formed in the early winter under synoptic temperature conditions and not being influenced by mountain lee waves. A sequence of measurements during a 5-days period shows a gradual change between liquid and solid type PSCs with the development of a well-known sandwich structure. It appears that all PSC observations show the presence of a background population of solid particles, occasionally mixed in with more dominating liquid particles. The measurements have been compared with results from a detailed microphysical and optical simulation of the formation processes. Calculated extinction(indices) are in good agreement with SAGE-III measurements from the same period. Apparently the solid particles are controlled by the synoptic temperature history while the presence of liquid particles is controlled by the local temperatures at the time of observation. The temperature histories indicate that the solid particles are nucleated above the ice frost point, and a surface freezing mechanism for this is included in the model. Reducing the calculated freezing rates by a factor 10–20, the model is able to simulate the observed particle size distributions and reproduce observed HNO 3 gas phase concentrations. Article in Journal/Newspaper Arctic Sodankylä Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Arctic Esrange ENVELOPE(21.117,21.117,67.883,67.883) Sodankylä ENVELOPE(26.600,26.600,67.417,67.417) |