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  Comments on 'Current GCMs' unrealistic negative feedback in the Artic'

Pithan, F., & Mauritsen, T. (2013). Comments on 'Current GCMs' unrealistic negative feedback in the Artic'. Journal of Climate, 26, 7783-7788. doi:10.1175/JCLI-D-12-00331.1.

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90398431.pdf (Publisher version), 607KB
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 Creators:
Pithan, Felix1, 2, Author
Mauritsen, Thorsten1, Author           
Affiliations:
1Climate Dynamics, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society, ou_913568              
2IMPRS on Earth System Modelling, MPI for Meteorology, Max Planck Society, Bundesstraße 53, 20146 Hamburg, DE, ou_913547              

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Free keywords: Arctic; Feedback; General circulation models; Inversions; Model comparison; Statistics
 Abstract: In contrast to prior studies showing a positive lapse-rate feedback associated with the Arctic inversion, Boe et al. reported that strong present-day Arctic temperature inversions are associated with stronger negative longwave feedbacks and thus reduced Arctic amplification in the model ensemble from phase 3 of the Coupled Model Intercomparison Project (CMIP3). A permutation test reveals that the relation between longwave feedbacks and inversion strength is an artifact of statistical self-correlation and that shortwave feedbacks have a stronger correlation with intermodel spread. The present comment concludes that the conventional understanding of a positive lapse-rate feedback associated with the Arctic inversion is consistent with the CMIP3 model ensemble.

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Language(s): eng - English
 Dates: 20122013-10-012013-10-01
 Publication Status: Issued
 Pages: -
 Publishing info: -
 Table of Contents: -
 Rev. Type: Peer
 Identifiers: DOI: 10.1175/JCLI-D-12-00331.1
 Degree: -

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Title: Journal of Climate
Source Genre: Journal
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Publ. Info: Boston, MA : American Meteorological Society
Pages: - Volume / Issue: 26 Sequence Number: - Start / End Page: 7783 - 7788 Identifier: ISSN: 0894-8755
CoNE: https://pure.mpg.de/cone/journals/resource/954925559525