Articles | Volume 17, issue 5
https://doi.org/10.5194/acp-17-3573-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-17-3573-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
HEPPA-II model–measurement intercomparison project: EPP indirect effects during the dynamically perturbed NH winter 2008–2009
Instituto de Astrofísica de Andalucía, CSIC, Apdo. 3004, 18008 Granada, Spain
William Ball
Physikalisch-Meteorologisches Observatorium, World Radiation Center, Davos, Switzerland
Stefan Bender
Karlsruhe Institute of Technology (KIT), Institute of Meteorology and Climate Research (IMK-ASF), P.O. Box 3640, 76021 Karlsruhe, Germany
Angela Gardini
Instituto de Astrofísica de Andalucía, CSIC, Apdo. 3004, 18008 Granada, Spain
V. Lynn Harvey
Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, USA
Alyn Lambert
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA
Manuel López-Puertas
Instituto de Astrofísica de Andalucía, CSIC, Apdo. 3004, 18008 Granada, Spain
Daniel R. Marsh
National Center for Atmospheric Research, Boulder, Colorado, USA
Katharina Meraner
Max Planck Institute for Meteorology, Hamburg, Germany
Holger Nieder
Karlsruhe Institute of Technology (KIT), Institute of Meteorology and Climate Research (IMK-ASF), P.O. Box 3640, 76021 Karlsruhe, Germany
Sanna-Mari Päivärinta
Earth Observation Unit, Finnish Meteorological Institute, Helsinki, Finland
Department of Physics, University of Helsinki, Helsinki, Finland
Kristell Pérot
Chalmers University of Technology, Göteborg, Sweden
Cora E. Randall
Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, USA
Thomas Reddmann
Karlsruhe Institute of Technology (KIT), Institute of Meteorology and Climate Research (IMK-ASF), P.O. Box 3640, 76021 Karlsruhe, Germany
Eugene Rozanov
Physikalisch-Meteorologisches Observatorium, World Radiation Center, Davos, Switzerland
Institute for Atmospheric and Climate Science ETH, Zurich, Switzerland
Hauke Schmidt
Max Planck Institute for Meteorology, Hamburg, Germany
Annika Seppälä
Earth Observation Unit, Finnish Meteorological Institute, Helsinki, Finland
Miriam Sinnhuber
Karlsruhe Institute of Technology (KIT), Institute of Meteorology and Climate Research (IMK-ASF), P.O. Box 3640, 76021 Karlsruhe, Germany
Timofei Sukhodolov
Physikalisch-Meteorologisches Observatorium, World Radiation Center, Davos, Switzerland
Gabriele P. Stiller
Karlsruhe Institute of Technology (KIT), Institute of Meteorology and Climate Research (IMK-ASF), P.O. Box 3640, 76021 Karlsruhe, Germany
Natalia D. Tsvetkova
Central Aerological Observatory, Moscow, Russia
Pekka T. Verronen
Earth Observation Unit, Finnish Meteorological Institute, Helsinki, Finland
Stefan Versick
Karlsruhe Institute of Technology (KIT), Institute of Meteorology and Climate Research (IMK-ASF), P.O. Box 3640, 76021 Karlsruhe, Germany
Karlsruhe Institute of Technology (KIT), Steinbuch Centre for Computing (SCC), Karlsruhe, Germany
Thomas von Clarmann
Karlsruhe Institute of Technology (KIT), Institute of Meteorology and Climate Research (IMK-ASF), P.O. Box 3640, 76021 Karlsruhe, Germany
Kaley A. Walker
Department of Physics, University of Toronto, Toronto, Ontario, Canada
Vladimir Yushkov
Central Aerological Observatory, Moscow, Russia
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Latest update: 20 Nov 2024
Short summary
Simulations from eight atmospheric models have been compared to tracer and temperature observations from seven satellite instruments in order to evaluate the energetic particle indirect effect (EPP IE) during the perturbed northern hemispheric (NH) winter 2008/2009. Models are capable to reproduce the EPP IE in dynamically and geomagnetically quiescent NH winter conditions. The results emphasize the need for model improvements in the dynamical representation of elevated stratopause events.
Simulations from eight atmospheric models have been compared to tracer and temperature...
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