Robust but weak winter atmospheric circulation response to future Arctic sea ice loss

The possibility that Arctic sea ice loss weakens mid-latitude westerlies, promoting more severe cold winters, has sparked more than a decade of scientific debate, with apparent support from observations but inconclusive modelling evidence. Here we show that sixteen models contributing to the Polar A...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Smith, D. M., Eade, R., Andrews, M. B., Ayres, H., Clark, A., Chripko, S., Deser, Clara, Dunstone, N. J., García-Serrano, Javier, Gastineau, G., Graff, L. S., Hardiman, S. C., He, B., Hermanson, L., Jung, Thomas, Knight, J., Levine, X., Magnusdottir, G., Manzini, E., Matei, Daniela, Mori, M., Msadek, Rym, Ortega, P., Peings, Y., Scaife, A. A., Screen, J. A., Seabrook, M., Semmler, Tido, Sigmond, M., Streffing, Jan, Sun, L., Walsh, A.
Format: Article in Journal/Newspaper
Language:unknown
Published: Nature Research 2022
Subjects:
Arctic
North Atlantic
North Atlantic oscillation
Sea ice
Online Access:https://epic.awi.de/id/eprint/56471/
https://epic.awi.de/id/eprint/56471/1/Smith_2022.pdf
https://www.nature.com/articles/s41467-022-28283-y
https://hdl.handle.net/10013/epic.ba84fad9-cf5b-42d6-bf48-1d3746ebd79c
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Summary:The possibility that Arctic sea ice loss weakens mid-latitude westerlies, promoting more severe cold winters, has sparked more than a decade of scientific debate, with apparent support from observations but inconclusive modelling evidence. Here we show that sixteen models contributing to the Polar Amplification Model Intercomparison Project simulate a weakening of mid-latitude westerlies in response to projected Arctic sea ice loss. We develop an emergent constraint based on eddy feedback, which is 1.2 to 3 times too weak in the models, suggesting that the real-world weakening lies towards the higher end of the model simulations. Still, the modelled response to Arctic sea ice loss is weak: the North Atlantic Oscillation response is similar in magnitude and offsets the projected response to increased greenhouse gases, but would only account for around 10% of variations in individual years. We further find that relationships between Arctic sea ice and atmospheric circulation have weakened recently in observations and are no longer inconsistent with those in models.

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