Editorial Type:
Corrigendum
Article Type:
Correction

Corrigendum

Reinhard Schiemann National Centre for Atmospheric Science, Department of Meteorology, University of Reading, Reading, United Kingdom

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Marie-Estelle Demory National Centre for Atmospheric Science, Department of Meteorology, University of Reading, Reading, United Kingdom

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Len C. Shaffrey National Centre for Atmospheric Science, Department of Meteorology, University of Reading, Reading, United Kingdom

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Jane Strachan National Centre for Atmospheric Science, Department of Meteorology, University of Reading, Reading, United Kingdom

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Pier Luigi Vidale National Centre for Atmospheric Science, Department of Meteorology, University of Reading, Reading, United Kingdom

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Matthew S. Mizielinski Met Office Hadley Centre, Exeter, United Kingdom

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Malcolm J. Roberts Met Office Hadley Centre, Exeter, United Kingdom

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Mio Matsueda Center for Computational Sciences, University of Tsukuba, Japan, and Department of Physics, University of Oxford, Oxford, United Kingdom

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Michael F. Wehner Lawrence Berkeley National Laboratory, Berkeley, California

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Thomas Jung European Centre for Medium-Range Weather Forecasts, Reading, United Kingdom, and Alfred Wegener Institute, Bremerhaven, Germany

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Print Publication:
15 Jun 2017
DOI:
https://doi.org/10.1175/JCLI-D-17-0091.1
Page(s):
4777–4778
A related article is available
Restricted access

Current affiliation: Met Office Hadley Centre, Exeter, United Kingdom.

Denotes content that is immediately available upon publication as open access.

© 2017 American Meteorological Society.

Corresponding authore-mail: R. Schiemann, r.k.schiemann@reading.ac.uk

Current affiliation: Met Office Hadley Centre, Exeter, United Kingdom.

Denotes content that is immediately available upon publication as open access.

© 2017 American Meteorological Society.

Corresponding authore-mail: R. Schiemann, r.k.schiemann@reading.ac.uk
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Journal of Climate

  • Schiemann, R., and Coauthors, 2017: The resolution sensitivity of Northern Hemisphere blocking in four 25-km atmospheric global circulation models. J. Climate, 30, 337–358, doi:10.1175/JCLI-D-16-0100.1.

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