Pithan, F. and Mauritsen, T. (2013) Comments on 'Current GCMs' Unrealistic Negative Feedback in the Arctic'. Journal of Climate, 26 (19). pp. 7783-7788. ISSN 1520-0442 doi: 10.1175/JCLI-D-12-00331.1
Abstract/Summary
In contrast to prior studies showing a positive lapse-rate feedback associated with the Arctic inversion, Boé 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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Item Type | Article |
URI | https://reading-clone.eprints-hosting.org/id/eprint/39341 |
Item Type | Article |
Refereed | Yes |
Divisions | No Reading authors. Back catalogue items |
Publisher | American Meteorological Society |
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