Airborne observation of mixing across the entrainment zone during PARADE 2011

This study presents the analysis of the structure and air mass characteristics of the lower atmosphere during the field campaign PARADE (PArticles and RAdicals: Diel observations of the impact of urban and biogenic Emissions) on Mount Kleiner Feldberg in southwestern Germany during late summer 2...

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Main Authors: F. Berkes, P. Hoor, H. Bozem, D. Kunkel, M. Sprenger, S. Henne
Format: Article
Language:English
Published: Copernicus Publications 2016-05-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/16/6011/2016/acp-16-6011-2016.pdf
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author F. Berkes
F. Berkes
F. Berkes
P. Hoor
H. Bozem
D. Kunkel
M. Sprenger
S. Henne
author_facet F. Berkes
F. Berkes
F. Berkes
P. Hoor
H. Bozem
D. Kunkel
M. Sprenger
S. Henne
author_sort F. Berkes
collection DOAJ
description This study presents the analysis of the structure and air mass characteristics of the lower atmosphere during the field campaign PARADE (PArticles and RAdicals: Diel observations of the impact of urban and biogenic Emissions) on Mount Kleiner Feldberg in southwestern Germany during late summer 2011. We analysed measurements of meteorological variables (temperature, moisture, pressure, wind speed and direction) from radio soundings and of chemical tracers (carbon dioxide, ozone) from aircraft measurements. We focus on the thermodynamic and dynamic properties that control the chemical distribution of atmospheric constituents in the boundary layer. We show that the evolution of tracer profiles of CO<sub>2</sub> and O<sub>3</sub> indicate mixing across the inversion layer (or entrainment zone). This finding is supported by the analysis of tracer–tracer correlations which are indicative for mixing and the relation of tracer profiles in relation to the evolution of the boundary layer height deduced from radio soundings. The study shows the relevance of entrainment processes for the lower troposphere in general and specifically that the tracer–tracer correlation method can be used to identify mixing and irreversible exchange processes across the inversion layer.
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spelling doaj.art-5d3fcd0ae9884e88b9895ee558e181a42022-12-22T01:33:33ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242016-05-01166011602510.5194/acp-16-6011-2016Airborne observation of mixing across the entrainment zone during PARADE 2011F. Berkes0F. Berkes1F. Berkes2P. Hoor3H. Bozem4D. Kunkel5M. Sprenger6S. Henne7Institute for Atmospheric Physics, Johannes Gutenberg University Mainz, Mainz, GermanyDepartment of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, Germanynow at: Institute of Energy and Climate Research-8: Troposphere, Forschungszentrum Jülich GmbH, Jülich, GermanyInstitute for Atmospheric Physics, Johannes Gutenberg University Mainz, Mainz, GermanyInstitute for Atmospheric Physics, Johannes Gutenberg University Mainz, Mainz, GermanyInstitute for Atmospheric Physics, Johannes Gutenberg University Mainz, Mainz, GermanyInstitute for Atmospheric and Climate Science, ETH Zurich, Zürich, SwitzerlandEmpa Swiss Federal Laboratories for Materials Science and Technology, Dübendorf, SwitzerlandThis study presents the analysis of the structure and air mass characteristics of the lower atmosphere during the field campaign PARADE (PArticles and RAdicals: Diel observations of the impact of urban and biogenic Emissions) on Mount Kleiner Feldberg in southwestern Germany during late summer 2011. We analysed measurements of meteorological variables (temperature, moisture, pressure, wind speed and direction) from radio soundings and of chemical tracers (carbon dioxide, ozone) from aircraft measurements. We focus on the thermodynamic and dynamic properties that control the chemical distribution of atmospheric constituents in the boundary layer. We show that the evolution of tracer profiles of CO<sub>2</sub> and O<sub>3</sub> indicate mixing across the inversion layer (or entrainment zone). This finding is supported by the analysis of tracer–tracer correlations which are indicative for mixing and the relation of tracer profiles in relation to the evolution of the boundary layer height deduced from radio soundings. The study shows the relevance of entrainment processes for the lower troposphere in general and specifically that the tracer–tracer correlation method can be used to identify mixing and irreversible exchange processes across the inversion layer.https://www.atmos-chem-phys.net/16/6011/2016/acp-16-6011-2016.pdf
spellingShingle F. Berkes
F. Berkes
F. Berkes
P. Hoor
H. Bozem
D. Kunkel
M. Sprenger
S. Henne
Airborne observation of mixing across the entrainment zone during PARADE 2011
Atmospheric Chemistry and Physics
title Airborne observation of mixing across the entrainment zone during PARADE 2011
title_full Airborne observation of mixing across the entrainment zone during PARADE 2011
title_fullStr Airborne observation of mixing across the entrainment zone during PARADE 2011
title_full_unstemmed Airborne observation of mixing across the entrainment zone during PARADE 2011
title_short Airborne observation of mixing across the entrainment zone during PARADE 2011
title_sort airborne observation of mixing across the entrainment zone during parade 2011
url https://www.atmos-chem-phys.net/16/6011/2016/acp-16-6011-2016.pdf
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