H
H. E. Scheel
Researcher at Karlsruhe Institute of Technology
Publications - 20
Citations - 2179
H. E. Scheel is an academic researcher from Karlsruhe Institute of Technology. The author has contributed to research in topics: Troposphere & Stratosphere. The author has an hindex of 15, co-authored 20 publications receiving 1998 citations. Previous affiliations of H. E. Scheel include June.
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Journal ArticleDOI
Stratosphere-troposphere exchange: A review, and what we have learned from STACCATO
Andreas Stohl,Paolo Bonasoni,Paolo Cristofanelli,William J. Collins,Johann Feichter,A. Frank,Caroline Forster,Evangelos Gerasopoulos,Heinz W. Gäggeler,P. James,T. Kentarchos,Helga Kromp-Kolb,B. C. Krüger,C. Land,J. Meloen,Alexandros Papayannis,Alfred Priller,Petra Seibert,Michael Sprenger,Geert-Jan Roelofs,H. E. Scheel,Christoph Schnabel,Peter Siegmund,Leonhard Tobler,Thomas Trickl,Heini Wernli,Volkmar Wirth,Prodromos Zanis,Christos Zerefos +28 more
TL;DR: The Influence of Stratosphere-Troposphere Exchange in a Changing Climate on Atmospheric Transport and Oxidation Capacity (STACCATO), recently funded by the European Union, provides a review of stratosphere-troposphere exchange (STE), with a focus on processes in the extratropics.
Journal ArticleDOI
Long-term changes in tropospheric ozone
Samuel J. Oltmans,Allen S. Lefohn,J. M. Harris,Ian E. Galbally,H. E. Scheel,Greg Bodeker,E.-G. Brunke,Hans Claude,David W. Tarasick,Beverly J. Johnson,Peter Simmonds,Douglas S. Shadwick,Kurt G. Anlauf,Katherine Hayden,F. J. Schmidlin,Toshifumi Fujimoto,K. Akagi,C. P. Meyer,S. Nichol,J. Davies,Alberto Redondas,Emilio Cuevas +21 more
TL;DR: Tropospheric ozone changes are investigated using a selected network of surface and ozonesonde sites to give a broad geographic picture of long-term variations as discussed by the authors, and three time series of � 20 years in length agree in showing increases that are strongest in the austral spring (August-October). Profile measurements show this increase extending through the mid troposphere but not into the highest levels of the troposphere.
Journal ArticleDOI
Long-term changes in lower tropospheric baseline ozone concentrations at northern mid-latitudes
David D. Parrish,Kathy S. Law,Johannes Staehelin,Richard G. Derwent,Owen R. Cooper,Owen R. Cooper,Hiroshi Tanimoto,Andreas Volz-Thomas,S. Gilge,H. E. Scheel,Martin Steinbacher,Elton Chan +11 more
TL;DR: In this article, changes in baseline (here understood as representative of continental to hemispheric scales) tropospheric O3 concentrations that have occurred at northern midlatitudes over the past six decades are quantified from available measurement records with the goal of providing benchmarks to which retrospective model calculations of the global O3 distribution can be compared.
Journal ArticleDOI
Recent tropospheric ozone changes – A pattern dominated by slow or no growth
Samuel J. Oltmans,Samuel J. Oltmans,Allen S. Lefohn,Douglas S. Shadwick,J. M. Harris,H. E. Scheel,Ian E. Galbally,David W. Tarasick,Beverly J. Johnson,E.-G. Brunke,Hans Claude,Guang Zeng,S. Nichol,F. J. Schmidlin,Jonathan Davies,Emilio Cuevas,Alberto Redondas,Hiroaki Naoe,Tatsumi Nakano,Taro Kawasato +19 more
TL;DR: In this article, the authors analyzed long-term (20-40 years) Tropospheric ozone (O3) time series obtained from surface and ozonesonde observations to assess possible changes with time through 2010.
Journal ArticleDOI
Long-term changes in lower tropospheric baseline ozone concentrations: Comparing chemistry-climate models and observations at northern midlatitudes
David D. Parrish,Jean-Francois Lamarque,Vaishali Naik,Larry W. Horowitz,Drew Shindell,Johannes Staehelin,Richard G. Derwent,Owen R. Cooper,Owen R. Cooper,Hiroshi Tanimoto,Andreas Volz-Thomas,S. Gilge,H. E. Scheel,Martin Steinbacher,Marina Fröhlich +14 more
TL;DR: The authors presented an approach for quantitative comparisons of model results with measurements for seasonally averaged tropospheric ozone (O3) concentrations, concluding that only limited confidence can be placed on estimates of present-day radiative forcing of ozone derived from modeled historic concentration changes and on predicted future O3 concentrations.