Forecasted deep stratospheric intrusions over Central Europe: case studies and climatologies

Based on daily predictions of stratospheric air intrusions, obtained from trajectory calculations by ETH Zürich with wind fields from ECMWF forecasts, a high number of measurements with the ozone lidar at IMK-IFU (Garmisch-Partenkirchen, Germany) were carried out in 2001. The lidar measurements show...

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Main Authors: Trickl, Thomas, Feldmann, H., Kanter, Hans-Joachim, Scheel, H.-E., Sprenger, M., Stohl, Andreas, Wernli, Heini
Format: Text
Language:English
Published: ETH Zurich 2010
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Online Access:https://dx.doi.org/10.3929/ethz-b-000017293
http://hdl.handle.net/20.500.11850/17293
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spelling ftdatacite:10.3929/ethz-b-000017293 2023-05-15T16:30:40+02:00 Forecasted deep stratospheric intrusions over Central Europe: case studies and climatologies Trickl, Thomas Feldmann, H. Kanter, Hans-Joachim Scheel, H.-E. Sprenger, M. Stohl, Andreas Wernli, Heini 2010 application/pdf https://dx.doi.org/10.3929/ethz-b-000017293 http://hdl.handle.net/20.500.11850/17293 en eng ETH Zurich info:eu-repo/semantics/openAccess Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CC-BY Text article-journal Journal Article ScholarlyArticle 2010 ftdatacite https://doi.org/10.3929/ethz-b-000017293 2021-11-05T12:55:41Z Based on daily predictions of stratospheric air intrusions, obtained from trajectory calculations by ETH Zürich with wind fields from ECMWF forecasts, a high number of measurements with the ozone lidar at IMK-IFU (Garmisch-Partenkirchen, Germany) were carried out in 2001. The lidar measurements show a large variety of rather different cases reflecting the full complexity of intrusion episodes that is not visible in classical case studies. In part, tropopause folds could be fully captured. The frequency of intrusion cases forecasted and verified by vertical sounding or in the in-situ data recorded at the nearby Zugspitze summit (2962 m a.s.l.) exceed that in previous work by more than a factor of two. Three cases mapped with the lidar were selected to validate the results for the corresponding time periods extracted from a one-year run with the new hemispheric version of the chemistry-transport model EURAD. Due to the high spatial resolution chosen for these simulations the agreement with the lidar measurements is satisfactory. The Zugspitze ozone data from 1978 to 2004 were recently filtered by applying different criteria for stratospheric air, based on the 7Be and humidity measurements. Here, by using the daily model forecasts during the time period 2001–2005, we examine three criteria and determine how well they represent the stratospheric air intrusions reaching the mountain site. Seasonal cycles for the period 2001–2005 were derived for the forecasts as well as the intrusion frequency per month for the forecasted intrusions and each of the criteria, distinguishing eight different characteristic transport pathways. In most cases a winter maximum and a summer minimum was obtained, but in the case of cyclonic arrival of intrusions starting over Greenland a late-spring maximum is seen. Two of the filtering criteria examined, based on combining a relative-humidity (RH) threshold of 60% with either a 7Be threshold of 5.5 mBq m−3 or the requirement for RH≤30% within ±6 h, rather reliably predict periods of deep intrusions reaching the Zugspitze station. An "or" combination of both these criteria yields slightly more cases and covers 77.9% of the intrusions identified. The lack of observations in the complementary 22.1% are mostly explained by overpasses. In this way the long-term trend of stratospheric ozone observed at this site as well as the corresponding ozone budget may be derived on the basis of measurements only. This effort will be the subject of a subsequent publication. : Atmospheric Chemistry and Physics, 10 (2) : ISSN:1680-7375 : ISSN:1680-7367 Text Greenland DataCite Metadata Store (German National Library of Science and Technology) Greenland
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description Based on daily predictions of stratospheric air intrusions, obtained from trajectory calculations by ETH Zürich with wind fields from ECMWF forecasts, a high number of measurements with the ozone lidar at IMK-IFU (Garmisch-Partenkirchen, Germany) were carried out in 2001. The lidar measurements show a large variety of rather different cases reflecting the full complexity of intrusion episodes that is not visible in classical case studies. In part, tropopause folds could be fully captured. The frequency of intrusion cases forecasted and verified by vertical sounding or in the in-situ data recorded at the nearby Zugspitze summit (2962 m a.s.l.) exceed that in previous work by more than a factor of two. Three cases mapped with the lidar were selected to validate the results for the corresponding time periods extracted from a one-year run with the new hemispheric version of the chemistry-transport model EURAD. Due to the high spatial resolution chosen for these simulations the agreement with the lidar measurements is satisfactory. The Zugspitze ozone data from 1978 to 2004 were recently filtered by applying different criteria for stratospheric air, based on the 7Be and humidity measurements. Here, by using the daily model forecasts during the time period 2001–2005, we examine three criteria and determine how well they represent the stratospheric air intrusions reaching the mountain site. Seasonal cycles for the period 2001–2005 were derived for the forecasts as well as the intrusion frequency per month for the forecasted intrusions and each of the criteria, distinguishing eight different characteristic transport pathways. In most cases a winter maximum and a summer minimum was obtained, but in the case of cyclonic arrival of intrusions starting over Greenland a late-spring maximum is seen. Two of the filtering criteria examined, based on combining a relative-humidity (RH) threshold of 60% with either a 7Be threshold of 5.5 mBq m−3 or the requirement for RH≤30% within ±6 h, rather reliably predict periods of deep intrusions reaching the Zugspitze station. An "or" combination of both these criteria yields slightly more cases and covers 77.9% of the intrusions identified. The lack of observations in the complementary 22.1% are mostly explained by overpasses. In this way the long-term trend of stratospheric ozone observed at this site as well as the corresponding ozone budget may be derived on the basis of measurements only. This effort will be the subject of a subsequent publication. : Atmospheric Chemistry and Physics, 10 (2) : ISSN:1680-7375 : ISSN:1680-7367
format Text
author Trickl, Thomas
Feldmann, H.
Kanter, Hans-Joachim
Scheel, H.-E.
Sprenger, M.
Stohl, Andreas
Wernli, Heini
spellingShingle Trickl, Thomas
Feldmann, H.
Kanter, Hans-Joachim
Scheel, H.-E.
Sprenger, M.
Stohl, Andreas
Wernli, Heini
Forecasted deep stratospheric intrusions over Central Europe: case studies and climatologies
author_facet Trickl, Thomas
Feldmann, H.
Kanter, Hans-Joachim
Scheel, H.-E.
Sprenger, M.
Stohl, Andreas
Wernli, Heini
author_sort Trickl, Thomas
title Forecasted deep stratospheric intrusions over Central Europe: case studies and climatologies
title_short Forecasted deep stratospheric intrusions over Central Europe: case studies and climatologies
title_full Forecasted deep stratospheric intrusions over Central Europe: case studies and climatologies
title_fullStr Forecasted deep stratospheric intrusions over Central Europe: case studies and climatologies
title_full_unstemmed Forecasted deep stratospheric intrusions over Central Europe: case studies and climatologies
title_sort forecasted deep stratospheric intrusions over central europe: case studies and climatologies
publisher ETH Zurich
publishDate 2010
url https://dx.doi.org/10.3929/ethz-b-000017293
http://hdl.handle.net/20.500.11850/17293
geographic Greenland
geographic_facet Greenland
genre Greenland
genre_facet Greenland
op_rights info:eu-repo/semantics/openAccess
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https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.3929/ethz-b-000017293
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