Mixing processes during the Antarctic vortex split in September-October 2002 as inferred from source gas and ozone distributions from ENVISAT-MIPAS

Norbert Glatthor, T. von Clarmann, H. Fischer, B. Funke, U. Grabowski, M. Höpfner, S. Kellmann, M. Kiefer, A. Linden, M. Milz, T. Steck, G. P. Stiller, G. Mengistu Tsidu, D. Y. Wang

Research output: Contribution to journalArticle

54 Citations (Scopus)

Abstract

In late September 2002, an Antarctic major stratospheric warming occurred, which led to a strong distortion of the southern polar vortex and to a split of its mid- and upper-stratospheric parts. Such an event had never before been observed since the beginning of regular Antarctic stratospheric temperature observations in the 1950s. The split is studied by means of nonoperational level-2 CH4, N 20, CFC-11, and O3 data, retrieved at the Institute for Meteorology and Climate Research Karlsruhe (IMK) from high-resolution atmospheric limb emission spectra from the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) on board the European research satellite, Environmental Satellite (ENVISAT). Retrieved horizontal and vertical distributions of CH4 and N 2O show good consistency with potential vorticity fields of the European Centre for Medium-Range Weather Forecasts (ECMWF) analysis for the entire period under investigation, even for fine structures such as vortex filaments. Tracer correlation analysis suggests that mixing into the vortex had already occurred before the major warming and that vortex fragments were transported into the surrounding air masses on potential temperature levels above 400 K during the split. Correlation analysis of ozone with the source gases indicates slight ongoing ozone destruction in the lower-stratospheric vortex (below ∼500 K) after the beginning of the warming event.

Original languageEnglish
Pages (from-to)787-800
Number of pages14
JournalJournal of the Atmospheric Sciences
Volume62
Issue number3
DOIs
Publication statusPublished - Mar 2005

Fingerprint

MIPAS
vortex
ozone
warming
gas
polar vortex
CFC
potential temperature
potential vorticity
meteorology
air mass
limb
vertical distribution
tracer
weather
distribution
climate
analysis
temperature

All Science Journal Classification (ASJC) codes

  • Atmospheric Science

Cite this

Glatthor, Norbert ; von Clarmann, T. ; Fischer, H. ; Funke, B. ; Grabowski, U. ; Höpfner, M. ; Kellmann, S. ; Kiefer, M. ; Linden, A. ; Milz, M. ; Steck, T. ; Stiller, G. P. ; Tsidu, G. Mengistu ; Wang, D. Y. / Mixing processes during the Antarctic vortex split in September-October 2002 as inferred from source gas and ozone distributions from ENVISAT-MIPAS. In: Journal of the Atmospheric Sciences. 2005 ; Vol. 62, No. 3. pp. 787-800.
@article{60ded9d10e7e4044949b55e8dd6f01a6,
title = "Mixing processes during the Antarctic vortex split in September-October 2002 as inferred from source gas and ozone distributions from ENVISAT-MIPAS",
abstract = "In late September 2002, an Antarctic major stratospheric warming occurred, which led to a strong distortion of the southern polar vortex and to a split of its mid- and upper-stratospheric parts. Such an event had never before been observed since the beginning of regular Antarctic stratospheric temperature observations in the 1950s. The split is studied by means of nonoperational level-2 CH4, N 20, CFC-11, and O3 data, retrieved at the Institute for Meteorology and Climate Research Karlsruhe (IMK) from high-resolution atmospheric limb emission spectra from the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) on board the European research satellite, Environmental Satellite (ENVISAT). Retrieved horizontal and vertical distributions of CH4 and N 2O show good consistency with potential vorticity fields of the European Centre for Medium-Range Weather Forecasts (ECMWF) analysis for the entire period under investigation, even for fine structures such as vortex filaments. Tracer correlation analysis suggests that mixing into the vortex had already occurred before the major warming and that vortex fragments were transported into the surrounding air masses on potential temperature levels above 400 K during the split. Correlation analysis of ozone with the source gases indicates slight ongoing ozone destruction in the lower-stratospheric vortex (below ∼500 K) after the beginning of the warming event.",
author = "Norbert Glatthor and {von Clarmann}, T. and H. Fischer and B. Funke and U. Grabowski and M. H{\"o}pfner and S. Kellmann and M. Kiefer and A. Linden and M. Milz and T. Steck and Stiller, {G. P.} and Tsidu, {G. Mengistu} and Wang, {D. Y.}",
year = "2005",
month = "3",
doi = "10.1175/JAS-3332.1",
language = "English",
volume = "62",
pages = "787--800",
journal = "Journals of the Atmospheric Sciences",
issn = "0022-4928",
publisher = "American Meteorological Society",
number = "3",

}

Glatthor, N, von Clarmann, T, Fischer, H, Funke, B, Grabowski, U, Höpfner, M, Kellmann, S, Kiefer, M, Linden, A, Milz, M, Steck, T, Stiller, GP, Tsidu, GM & Wang, DY 2005, 'Mixing processes during the Antarctic vortex split in September-October 2002 as inferred from source gas and ozone distributions from ENVISAT-MIPAS', Journal of the Atmospheric Sciences, vol. 62, no. 3, pp. 787-800. https://doi.org/10.1175/JAS-3332.1

Mixing processes during the Antarctic vortex split in September-October 2002 as inferred from source gas and ozone distributions from ENVISAT-MIPAS. / Glatthor, Norbert; von Clarmann, T.; Fischer, H.; Funke, B.; Grabowski, U.; Höpfner, M.; Kellmann, S.; Kiefer, M.; Linden, A.; Milz, M.; Steck, T.; Stiller, G. P.; Tsidu, G. Mengistu; Wang, D. Y.

In: Journal of the Atmospheric Sciences, Vol. 62, No. 3, 03.2005, p. 787-800.

Research output: Contribution to journalArticle

TY - JOUR

T1 - Mixing processes during the Antarctic vortex split in September-October 2002 as inferred from source gas and ozone distributions from ENVISAT-MIPAS

AU - Glatthor, Norbert

AU - von Clarmann, T.

AU - Fischer, H.

AU - Funke, B.

AU - Grabowski, U.

AU - Höpfner, M.

AU - Kellmann, S.

AU - Kiefer, M.

AU - Linden, A.

AU - Milz, M.

AU - Steck, T.

AU - Stiller, G. P.

AU - Tsidu, G. Mengistu

AU - Wang, D. Y.

PY - 2005/3

Y1 - 2005/3

N2 - In late September 2002, an Antarctic major stratospheric warming occurred, which led to a strong distortion of the southern polar vortex and to a split of its mid- and upper-stratospheric parts. Such an event had never before been observed since the beginning of regular Antarctic stratospheric temperature observations in the 1950s. The split is studied by means of nonoperational level-2 CH4, N 20, CFC-11, and O3 data, retrieved at the Institute for Meteorology and Climate Research Karlsruhe (IMK) from high-resolution atmospheric limb emission spectra from the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) on board the European research satellite, Environmental Satellite (ENVISAT). Retrieved horizontal and vertical distributions of CH4 and N 2O show good consistency with potential vorticity fields of the European Centre for Medium-Range Weather Forecasts (ECMWF) analysis for the entire period under investigation, even for fine structures such as vortex filaments. Tracer correlation analysis suggests that mixing into the vortex had already occurred before the major warming and that vortex fragments were transported into the surrounding air masses on potential temperature levels above 400 K during the split. Correlation analysis of ozone with the source gases indicates slight ongoing ozone destruction in the lower-stratospheric vortex (below ∼500 K) after the beginning of the warming event.

AB - In late September 2002, an Antarctic major stratospheric warming occurred, which led to a strong distortion of the southern polar vortex and to a split of its mid- and upper-stratospheric parts. Such an event had never before been observed since the beginning of regular Antarctic stratospheric temperature observations in the 1950s. The split is studied by means of nonoperational level-2 CH4, N 20, CFC-11, and O3 data, retrieved at the Institute for Meteorology and Climate Research Karlsruhe (IMK) from high-resolution atmospheric limb emission spectra from the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) on board the European research satellite, Environmental Satellite (ENVISAT). Retrieved horizontal and vertical distributions of CH4 and N 2O show good consistency with potential vorticity fields of the European Centre for Medium-Range Weather Forecasts (ECMWF) analysis for the entire period under investigation, even for fine structures such as vortex filaments. Tracer correlation analysis suggests that mixing into the vortex had already occurred before the major warming and that vortex fragments were transported into the surrounding air masses on potential temperature levels above 400 K during the split. Correlation analysis of ozone with the source gases indicates slight ongoing ozone destruction in the lower-stratospheric vortex (below ∼500 K) after the beginning of the warming event.

UR - http://www.scopus.com/inward/record.url?scp=20144389892&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=20144389892&partnerID=8YFLogxK

U2 - 10.1175/JAS-3332.1

DO - 10.1175/JAS-3332.1

M3 - Article

AN - SCOPUS:20144389892

VL - 62

SP - 787

EP - 800

JO - Journals of the Atmospheric Sciences

JF - Journals of the Atmospheric Sciences

SN - 0022-4928

IS - 3

ER -