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Quantifying climate feedbacks in polar regions

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10.1038/s41467-018-04173-0
 
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hdl:2117/119331

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Goosse, Hugues
Kay, Jennifer E.
Armour, Kyle C.
Bodas-Salcedo, Alejandro
Chepfer, Helene
Docquier, David
Jonko, Alexandra
Kushner, Paul J.
Lecomte, Olivier
Massonnet, François
Park, Hyo-Seok
Pithan, Felix
Svensson, Gunilla
Vancoppenolle, Martin
Document typeArticle
Defense date2018-05-15
PublisherNature Publishing Group
Rights accessOpen Access
Attribution-NonCommercial-NoDerivs 4.0 Spain
Except where otherwise noted, content on this work is licensed under a Creative Commons license : Attribution-NonCommercial-NoDerivs 4.0 Spain
ProjectPRIMAVERA - PRocess-based climate sIMulation: AdVances in high resolution modelling and European climate Risk Assessment (EC-H2020-641727)
Abstract
The concept of feedback is key in assessing whether a perturbation to a system is amplified or damped by mechanisms internal to the system. In polar regions, climate dynamics are controlled by both radiative and non-radiative interactions between the atmosphere, ocean, sea ice, ice sheets and land surfaces. Precisely quantifying polar feedbacks is required for a process-oriented evaluation of climate models, a clear understanding of the processes responsible for polar climate changes, and a reduction in uncertainty associated with model projections. This quantification can be performed using a simple and consistent approach that is valid for a wide range of feedbacks, offering the opportunity for more systematic feedback analyses and a better understanding of polar climate changes.
CitationGoosse, H. [et al.]. Quantifying climate feedbacks in polar regions. "Nature Communications", 15 Maig 2018, vol. 9. 
URIhttp://hdl.handle.net/2117/119331
DOI10.1038/s41467-018-04173-0
ISSN2041-1723
Publisher versionhttps://www.nature.com/articles/s41467-018-04173-0
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  • Earth Sciences - Articles de revista [307]
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