An algorithm to detect tropopause folds from ozone soundings

An algorithm has been developed to determine the occurrence of tropopause folds by an analysis of ozone soundings together with meteorological parameters, especially the potential vorticity. Tropopause folds transfer air and trace gases from the lower stratosphere into the troposphere. The algorithm...

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書目詳細資料
發表在:Meteorologische Zeitschrift
Main Authors: Susanne Blonsky, Peter Speth
格式: Article
語言:英语
出版: Borntraeger 1998-08-01
主題:
在線閱讀:http://dx.doi.org/10.1127/metz/7/1998/153
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author Susanne Blonsky
Peter Speth
author_facet Susanne Blonsky
Peter Speth
author_sort Susanne Blonsky
collection DOAJ
container_title Meteorologische Zeitschrift
description An algorithm has been developed to determine the occurrence of tropopause folds by an analysis of ozone soundings together with meteorological parameters, especially the potential vorticity. Tropopause folds transfer air and trace gases from the lower stratosphere into the troposphere. The algorithm detects folds by means of ozone anomalies in the troposphere, a simultaneous occurrence of low humidity and high values of potential vorticity. Furthermore the wind speed of the tropospheric wind profile has to exceed a jet stream velocity threshold of 30 m s-1. The application of the algorithm to the 2663 soundings taken at the sites Jülich, Uccle, Hohenpeißenberg and Payerne during six years (1989-1994) demonstrates that 46 tropopause folding events could be identified. The maximum of fold occurrence was found in March, and the minimum in April to June. The tropopause folded down to altitudes between 400 and 700 hPa during 75 % of the events.
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spelling doaj-art-5fbea1298d0f4a0cb4bd3b41bac23f212025-08-19T22:23:32ZengBorntraegerMeteorologische Zeitschrift0941-29481998-08-017415316210.1127/metz/7/1998/15389069An algorithm to detect tropopause folds from ozone soundingsSusanne BlonskyPeter SpethAn algorithm has been developed to determine the occurrence of tropopause folds by an analysis of ozone soundings together with meteorological parameters, especially the potential vorticity. Tropopause folds transfer air and trace gases from the lower stratosphere into the troposphere. The algorithm detects folds by means of ozone anomalies in the troposphere, a simultaneous occurrence of low humidity and high values of potential vorticity. Furthermore the wind speed of the tropospheric wind profile has to exceed a jet stream velocity threshold of 30 m s-1. The application of the algorithm to the 2663 soundings taken at the sites Jülich, Uccle, Hohenpeißenberg and Payerne during six years (1989-1994) demonstrates that 46 tropopause folding events could be identified. The maximum of fold occurrence was found in March, and the minimum in April to June. The tropopause folded down to altitudes between 400 and 700 hPa during 75 % of the events.http://dx.doi.org/10.1127/metz/7/1998/153tropopause foldsozone soundingsvorticitytropopausenfaltungenozonanomalien
spellingShingle Susanne Blonsky
Peter Speth
An algorithm to detect tropopause folds from ozone soundings
tropopause folds
ozone soundings
vorticity
tropopausenfaltungen
ozonanomalien
title An algorithm to detect tropopause folds from ozone soundings
title_full An algorithm to detect tropopause folds from ozone soundings
title_fullStr An algorithm to detect tropopause folds from ozone soundings
title_full_unstemmed An algorithm to detect tropopause folds from ozone soundings
title_short An algorithm to detect tropopause folds from ozone soundings
title_sort algorithm to detect tropopause folds from ozone soundings
topic tropopause folds
ozone soundings
vorticity
tropopausenfaltungen
ozonanomalien
url http://dx.doi.org/10.1127/metz/7/1998/153
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AT peterspeth analgorithmtodetecttropopausefoldsfromozonesoundings
AT susanneblonsky algorithmtodetecttropopausefoldsfromozonesoundings
AT peterspeth algorithmtodetecttropopausefoldsfromozonesoundings