http://www.cnr.it/ontology/cnr/individuo/prodotto/ID261538
Reconciliation of essential process parameters for an enhanced predictability of Arctic stratospheric ozone loss and its climate interactions (RECONCILE): activities and results (Articolo in rivista)
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- Label
- Reconciliation of essential process parameters for an enhanced predictability of Arctic stratospheric ozone loss and its climate interactions (RECONCILE): activities and results (Articolo in rivista) (literal)
- Anno
- 2013-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.5194/acp-13-9233-2013 (literal)
- Alternative label
von Hobe M. [1] ; Bekki S. [2] ; S. Borrmann [3] ; Cairo F. [4] ; D'Amato F. [5] ; Di Donfrancesco G. [32] ; Dörnbrack A. [6] ; Ebersoldt A. [7] ; Ebert M. [8] ; Emde C. [9] ; Engel I. [10] ; Ern M. [1] ; Frey W. [3] ; Genco S. [4] ; Griessbach S. [11] ; Grooß J.-U. [1] ; Gulde T. [12] ; Günther G. [1] ; Hösen E. [13] ; Hoffmann L. [11] ; Homonnai V. [14] ; Hoyle C. R. [10] ; Isaksen I. S. A. [15] ; Jackson D. R. [16] ;. Jánosi I.M. [14] ; Jones R. L. [17] ; Kandler K. [8] ; Kalicinsky C. [13] ; Keil A. [18] ; Khaykin S.M. [19] ; Khosrawi F. [20] ; Kivi R. [21] ; Kuttippurath J. [2] ; Laube J. C. [22] ; Lefèvre F. [2] ; Lehmann R. [23] ; Ludmann S. [24] ; Luo B. P. [10] ; Marchand M. [2] ; Meyer J. [1] ; Mitev V. [25] ; Molleker S. [3] ; Müller R. [1] ; Oelhaf H. [12] ; Olschewski F. [13] ; Orsolini Y. [26] ; Peter T. [10] ; Pfeilsticker K. [24] ; Piesch C. [12] ; Pitts M.C. [27] ; Poole L. R. [28] ; Pope F. D. [17] ; Ravegnani F. [4] ; Rex M. [23] ; Riese M. [1] ; Röckmann T. [29] ; Rognerud B. [15] ; Roiger A. [6] ;Rolf C. [1] ; Santee M. L. [30] ; Scheibe M. [6] ; Schiller C. [1] ; Schlager H. [6] ; M. Siciliani de Cumis M. [5] ; N. Sitnikov N. [19] ; Søvde O. A. [15] ; Spang R. [1] ; Spelten N. [1] ; Stordal F. [15] ; Sumi´nska-Ebersoldt O. [1] ; Ulanovski A. [19] ; Ungermann J. [1] ; Viciani S. [5] ; Volk C. M. [13] ; vom Scheidt M. [13] ; von der Gathen P. [23] ; Walker K. [31] ; Wegner T. [1] ; Weigel R. [3] ; Weinbruch S. [8] ; G. Wetzel [12] ; Wienhold F.G. [10] ; Wohltmann I. [23] ; Woiwode W. [12] ; Young I. A. K. [17] ; Yushkov V. [19] ; Zobrist B. [10] ; Stroh F. [1] (2013)
Reconciliation of essential process parameters for an enhanced predictability of Arctic stratospheric ozone loss and its climate interactions (RECONCILE): activities and results
in Atmospheric chemistry and physics (Print); Copernicus publications, Göttingen (Germania)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- von Hobe M. [1] ; Bekki S. [2] ; S. Borrmann [3] ; Cairo F. [4] ; D'Amato F. [5] ; Di Donfrancesco G. [32] ; Dörnbrack A. [6] ; Ebersoldt A. [7] ; Ebert M. [8] ; Emde C. [9] ; Engel I. [10] ; Ern M. [1] ; Frey W. [3] ; Genco S. [4] ; Griessbach S. [11] ; Grooß J.-U. [1] ; Gulde T. [12] ; Günther G. [1] ; Hösen E. [13] ; Hoffmann L. [11] ; Homonnai V. [14] ; Hoyle C. R. [10] ; Isaksen I. S. A. [15] ; Jackson D. R. [16] ;. Jánosi I.M. [14] ; Jones R. L. [17] ; Kandler K. [8] ; Kalicinsky C. [13] ; Keil A. [18] ; Khaykin S.M. [19] ; Khosrawi F. [20] ; Kivi R. [21] ; Kuttippurath J. [2] ; Laube J. C. [22] ; Lefèvre F. [2] ; Lehmann R. [23] ; Ludmann S. [24] ; Luo B. P. [10] ; Marchand M. [2] ; Meyer J. [1] ; Mitev V. [25] ; Molleker S. [3] ; Müller R. [1] ; Oelhaf H. [12] ; Olschewski F. [13] ; Orsolini Y. [26] ; Peter T. [10] ; Pfeilsticker K. [24] ; Piesch C. [12] ; Pitts M.C. [27] ; Poole L. R. [28] ; Pope F. D. [17] ; Ravegnani F. [4] ; Rex M. [23] ; Riese M. [1] ; Röckmann T. [29] ; Rognerud B. [15] ; Roiger A. [6] ;Rolf C. [1] ; Santee M. L. [30] ; Scheibe M. [6] ; Schiller C. [1] ; Schlager H. [6] ; M. Siciliani de Cumis M. [5] ; N. Sitnikov N. [19] ; Søvde O. A. [15] ; Spang R. [1] ; Spelten N. [1] ; Stordal F. [15] ; Sumi´nska-Ebersoldt O. [1] ; Ulanovski A. [19] ; Ungermann J. [1] ; Viciani S. [5] ; Volk C. M. [13] ; vom Scheidt M. [13] ; von der Gathen P. [23] ; Walker K. [31] ; Wegner T. [1] ; Weigel R. [3] ; Weinbruch S. [8] ; G. Wetzel [12] ; Wienhold F.G. [10] ; Wohltmann I. [23] ; Woiwode W. [12] ; Young I. A. K. [17] ; Yushkov V. [19] ; Zobrist B. [10] ; Stroh F. [1] (literal)
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- 1 Forschungszentrum Jülich GmbH, Institute of Energy and Climate Research (IEK-7), Jülich, Germany
2 LATMOS-IPSL, UPMC Univ. Paris 06, Université Versailles St.-Quentin, CNRS/INSU, Paris, France
3 Max Planck Institute for Chemistry, Particle Chemistry Department, Mainz, Germany
4 Institute of Atmospheric Science and Climate, ISAC-CNR, Italy
5 CNR-INO (Istituto Nazionale di Ottica), Largo E. Fermi, 6, 50125 Firenze, Italy
6 Deutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, 82234 Weßling,
Germany
7 Institute for Data Processing and Electronics, Karlsruhe Institute of Technology, Karlsruhe, Germany
8 Technische Universität Darmstadt, Institut für Angewandte Geowissenschaften, Umweltmineralogie, Darmstadt, Germany
9 Meteorologisches Institut, Ludwig-Maximilians-Universität, München, Germany
10 ETH Zurich, Institute for Atmospheric and Climate Science, Zurich, Switzerland
11 Jülich Supercomputing Centre (JSC), Forschungszentrum Jülich GmbH, Jülich, Germany
12 Institute for Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany
13 Department of Physics, University of Wuppertal, Germany
14 Department of Physics of Complex Systems, Eötvös Loránd University, Pázmány P. s. 1/A, 1117 Budapest, Hungary
15 Department of Geosciences, University of Oslo, Oslo, Norway
16 Met Office, Exeter, UK
17 University of Cambridge, Department of Chemistry, Cambridge, UK
18 Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt, Germany
19 Central Aerological Observatory, Dolgoprudny, Moskow Region, Russia
20 MISU, Stockholm University, Stockholm, Sweden
21 Finnish Meteorological Institute, Arctic Research, Sodankylä, Finland
22 University of East Anglia, School of Environmental Sciences, Norwich, UK
23 Alfred Wegener Institute for Polar and Marine Research, Potsdam, Germany
24 Institut für Umweltphysik, University of Heidelberg, Germany
25 CSEM Centre Suisse d'Electronique et de Microtechnique SA, Neuchâtel, Switzerland
26 Norwegian Institute for Air Research, Kjeller, Norway
27 NASA Langley Research Center, Hampton, VA 23681, USA
28 Science Systems and Applications, Inc. Hampton, VA 23666, USA
29 Institute for Marine and Atmospheric Research Utrecht (IMAU), Utrecht University, Utrecht, the Netherlands
30 JPL/NASA, California Institute of Technology, Pasadena, California, USA
31 Department of Physics, University of Toronto, Toronto, Canada
32 Ente Nazionale per le Nuove tecnologie, l'Energia e l'Ambiente, Roma, Italy
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- Titolo
- Reconciliation of essential process parameters for an enhanced predictability of Arctic stratospheric ozone loss and its climate interactions (RECONCILE): activities and results (literal)
- Abstract
- The international research project RECONCILE has addressed central questions regarding polar ozone depletion, with the objective to quantify some of the most relevant yet still uncertain physical and chemical processes and thereby improve prognostic modelling capabilities to realistically predict the response of the ozone layer to climate change. This overview paper outlines the scope and the general approach of RECONCILE, and it provides a summary of observations and modelling in 2010 and 2011 that have generated an in many respects unprecedented dataset to study processes in the Arctic winter stratosphere. Principally, it summarises important outcomes of RECONCILE including (i) better constraints and enhanced consistency on the set of parameters governing catalytic ozone destruction cycles, (ii) a better understanding of the role of cold binary aerosols in heterogeneous chlorine activation, (iii) an improved scheme of polar stratospheric cloud (PSC) processes that includes heterogeneous nucleation of nitric acid trihydrate (NAT) and ice on non-volatile background aerosol leading to better model parameterisations with respect to denitrification, and (iv) long transient simulations with a chemistry-
climate model (CCM) updated based on the results of RECONCILE that better reproduce past ozone trends in Antarctica
and are deemed to produce more reliable predictions of future ozone trends. The process studies and the global simulations
conducted in RECONCILE show that in the Arctic, ozone depletion uncertainties in the chemical and microphysical processes are now clearly smaller than the sensitivity to dynamic variability. (literal)
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