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Atmos. Chem. Phys., 14, 9923–9923, 2014 www.atmos-chem-phys.net/14/9923/2014/

doi:10.5194/acp-14-9923-2014

© Author(s) 2014. CC Attribution 3.0 License.

Corrigendum to

“Advances in understanding and parameterization of small-scale physical processes in the marine Arctic climate system: a review”

published in Atmos. Chem. Phys., 14, 9403–9450, 2014

T. Vihma1,2, R. Pirazzini1, I. Fer3, I. A. Renfrew4, J. Sedlar5,6, M. Tjernström5,6, C. Lüpkes7, T. Nygård1, D. Notz8, J. Weiss9, D. Marsan10, B. Cheng1, G. Birnbaum7, S. Gerland11, D. Chechin12, and J. C. Gascard13

1Finnish Meteorological Institute, Helsinki, Finland

2The University Centre in Svalbard, Longyearbyen, Norway

3University of Bergen, Bergen, Norway

4University of East Anglia, Norwich, UK

5Bert Bolin Center for Climate Research, Stockholm, Sweden

6Department of Meteorology, Stockholm University, Stockholm, Sweden

7Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany

8Max Planck Institute for Meteorology, Hamburg, Germany

9LGGE, Université de Grenoble, CNRS, Grenoble, France

10ISTerre, Université de Savoie, CNRS, Le Bourget-du-Lac, France

11Norwegian Polar Institute, Tromsø, Norway

12A. M. Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences, Moscow, Russia

13Université Pierre et Marie Curie, Paris, France

Correspondence to: T. Vihma (timo.vihma@fmi.fi)

Figure 9 was incorrect. The correct figure is presented below.Figure 9 was incorrect. The correct figure is presented below.

Figure 9. Spatial distribution of the magnitude of inertial oscillations in Arctic sea ice in summer in (a) 1979–2001 and (b) 2002–2008. The colour scale presents a non-dimensional parameter that Gimbert et al. (2012a) calculated to represent the magnitude of inertial oscillation. Reproduced with permission from Gimbert et al. (2012a).

Figure 9. Spatial distribution of the magnitude of inertial oscillations in Arctic sea ice in summer in (a) 1979–2001 and (b) 2002–2008. The colour scale presents a non-dimensional parameter that Gimbert et al. (2012a) calculated to represent the magnitude of inertial oscillation.

Reproduced with permission from Gimbert et al. (2012a).

Published by Copernicus Publications on behalf of the European Geosciences Union.

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