Comments on 'Current GCMs' Unrealistic Negative Feedback in the Arctic'
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 fro...
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American Meteorological Society
2013
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ftunivreading:oai:centaur.reading.ac.uk:39341 2024-09-15T17:50:46+00:00 Comments on 'Current GCMs' Unrealistic Negative Feedback in the Arctic' Pithan, Felix Mauritsen, Thorsten 2013 https://centaur.reading.ac.uk/39341/ unknown American Meteorological Society Pithan, F. <https://centaur.reading.ac.uk/view/creators/90005860.html> 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: https://doi.org/10.1175/JCLI-D-12-00331.1 <https://doi.org/10.1175/JCLI-D-12-00331.1> Article PeerReviewed 2013 ftunivreading https://doi.org/10.1175/JCLI-D-12-00331.1 2024-06-25T14:57:10Z 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. Article in Journal/Newspaper Arctic Arctic CentAUR: Central Archive at the University of Reading Journal of Climate 26 19 7783 7788 |
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CentAUR: Central Archive at the University of Reading |
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ftunivreading |
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description |
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. |
format |
Article in Journal/Newspaper |
author |
Pithan, Felix Mauritsen, Thorsten |
spellingShingle |
Pithan, Felix Mauritsen, Thorsten Comments on 'Current GCMs' Unrealistic Negative Feedback in the Arctic' |
author_facet |
Pithan, Felix Mauritsen, Thorsten |
author_sort |
Pithan, Felix |
title |
Comments on 'Current GCMs' Unrealistic Negative Feedback in the Arctic' |
title_short |
Comments on 'Current GCMs' Unrealistic Negative Feedback in the Arctic' |
title_full |
Comments on 'Current GCMs' Unrealistic Negative Feedback in the Arctic' |
title_fullStr |
Comments on 'Current GCMs' Unrealistic Negative Feedback in the Arctic' |
title_full_unstemmed |
Comments on 'Current GCMs' Unrealistic Negative Feedback in the Arctic' |
title_sort |
comments on 'current gcms' unrealistic negative feedback in the arctic' |
publisher |
American Meteorological Society |
publishDate |
2013 |
url |
https://centaur.reading.ac.uk/39341/ |
genre |
Arctic Arctic |
genre_facet |
Arctic Arctic |
op_relation |
Pithan, F. <https://centaur.reading.ac.uk/view/creators/90005860.html> 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: https://doi.org/10.1175/JCLI-D-12-00331.1 <https://doi.org/10.1175/JCLI-D-12-00331.1> |
op_doi |
https://doi.org/10.1175/JCLI-D-12-00331.1 |
container_title |
Journal of Climate |
container_volume |
26 |
container_issue |
19 |
container_start_page |
7783 |
op_container_end_page |
7788 |
_version_ |
1810292564339720192 |