Abstract
Observations show that reduced regional sea-ice cover is coincident with cold mid-latitude winters on interannual timescales. However, it remains unclear whether these observed links are causal, and model experiments suggest that they might not be. Here we apply two independent approaches to infer causality from observations and climate models and to reconcile these sources of data. Models capture the observed correlations between reduced sea ice and cold mid-latitude winters, but only when reduced sea ice coincides with anomalous heat transfer from the atmosphere to the ocean, implying that the atmosphere is driving the loss. Causal inference from the physics-based approach is corroborated by a leadâlag analysis, showing that circulation-driven temperature anomalies precede, but do not follow, reduced sea ice. Furthermore, no mid-latitude cooling is found in modelling experiments with imposed future sea-ice loss. Our results show robust support for anomalous atmospheric circulation simultaneously driving cold mid-latitude winters and mild Arctic conditions, and reduced sea ice having a minimal influence on severe mid-latitude winters.
This is a preview of subscription content, access via your institution
Access options
Access Nature and 54 other Nature Portfolio journals
Get Nature+, our best-value online-access subscription
$29.99 /Â 30Â days
cancel any time
Subscribe to this journal
Receive 12 print issues and online access
$209.00 per year
only $17.42 per issue
Buy this article
- Purchase on SpringerLink
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout





Similar content being viewed by others
Data availability
The model output is available on reasonable request from the corresponding author. ERA-Interim reanalysis data were obtained from the ECMWF data server (https://www.ecmwf.int/en/forecasts/datasets/reanalysis-datasets/era-interim).
Code availability
The code used to create the figures is available on request from the corresponding author.
References
Screen, J. A. & Simmonds, I. The central role of diminishing sea ice in recent Arctic temperature amplification. Nature 464, 1334â1337 (2010).
Walsh, J. E. Intensified warming of the Arctic: causes and impacts on middle latitudes. Glob. Planet. Change 117, 52â63 (2014).
Cohen, J. et al. Recent Arctic amplification and extreme mid-latitude weather. Nat. Geosci. 7, 627â637 (2014).
Stroeve, J., Holland, M. M., Meier, W., Scambos, T. & Serreze, M. Arctic sea ice decline: faster than forecast. Geophys. Res. Lett. 34, L09501 (2007).
Stroeve, J. C. et al. Trends in Arctic sea ice extent from CMIP5, CMIP3 and observations. Geophys. Res. Lett. 39, L16502 (2012).
Overland, J. E., Wood, K. R. & Wang, M. Warm Arctic-cold continents: climate impacts of the newly open Arctic Sea. Polar Res. 30, 15787 (2011).
Kug, J.-S. et al. Two distinct influences of Arctic warming on cold winters over North America and East Asia. Nat. Geosci. 8, 759â762 (2015).
Mori, M., Watanabe, M., Shiogama, H., Inoue, J. & Kimoto, M. Robust Arctic sea-ice influence on the frequent Eurasian cold winters in past decades. Nat. Geosci. 7, 869â873 (2014).
Inoue, J., Hori, M. E. & Takaya, K. The role of Barents Sea ice in the wintertime cyclone track and emergence of a warm-Arctic cold-Siberian anomaly. J. Clim. 25, 2561â2568 (2012).
Tang, Q., Zhang, X., Yang, X. & Francis, J. A. Cold winter extremes in northern continents linked to Arctic sea ice loss. Environ. Res. Lett. 8, 014036 (2013).
Kim, J.-S. et al. Reduced North American terrestrial primary productivity linked to anomalous Arctic warming. Nat. Geosci. 10, 572â576 (2017).
Cohen, J., Pfeiffer, K. & Francis, J. A. Warm Arctic episodes linked with increased frequency of extreme winter weather in the United States. Nat. Commun. 9, 869 (2018).
McCusker, K. E., Fyfe, J. C. & Sigmond, M. Twenty-five winters of unexpected Eurasian cooling unlikely due to Arctic sea-ice loss. Nat. Geosci. 9, 838â842 (2016).
Sun, L., Perlwitz, J. & Hoerling, M. What caused the recent âWarm Arctic, Cold Continentsâ trend pattern in winter temperatures? Geophys. Res. Lett. 43, 5345â5352 (2016).
Collow, T. W., Wang, W. & Kumar, A. Simulations of Eurasian winter temperature trends in coupled and uncoupled CFSv2. Adv. Atmos. Sci. 35, 14â26 (2018).
Ogawa, F. et al. Evaluating impacts of recent Arctic sea ice loss on the Northern Hemisphere winter climate change. Geophys. Res. Lett. 45, 3255â3263 (2018).
Koenigk, T. et al. Impact of Arctic sea ice variations on winter temperature anomalies in northern hemispheric land areas. Clim. Dynam. 52, 3111â3137 (2019).
Honda, M., Inoue, J. & Yamane, S. Influence of low Arctic seaâice minima on anomalously cold Eurasian winters. Geophys. Res. Lett. 36, L08707 (2009).
Mori, M., Kosaka, Y., Watanabe, M., Nakamura, H. & Kimoto, M. A reconciled estimate of the influence of Arctic sea-ice loss on recent Eurasian cooling. Nat. Clim. Change 9, 123â129 (2019).
Deser, C., Walsh, J. E. & Timlin, M. S. Arctic sea ice variability in the context of recent atmospheric circulation trends. J. Clim. 13, 617â633 (2000).
Deser, C., Tomas, R., Alexander, M. & Lawrence, D. The seasonal atmospheric response to projected Arctic sea ice loss in the late twenty-first century. J. Clim. 23, 333â351 (2010).
Park, H.-S., Lee, S., Son, S.-W., Feldstein, S. B. & Kosaka, Y. The impact of poleward moisture and sensible heat flux on Arctic winter sea ice variability. J. Clim. 28, 5030â5040 (2015).
Woods, C. & Caballero, R. The role of moist intrusions in winter Arctic warming and sea ice decline. J. Clim. 29, 4473â4485 (2016).
Lee, S., Gong, T., Feldstein, S. B., Screen, J. A. & Simmonds, I. Revisiting the cause of the 1989â2009 Arctic surface warming using the surface energy budget: downward infrared radiation dominates the surface fluxes. Geophys. Res. Lett. 44, 10654â10661 (2017).
Luo, B., Luo, D., Wu, L., Zhong, L. & Simmonds, I. Atmospheric circulation patterns which promote winter Arctic sea ice decline. Environ. Res. Lett. 12, 054017 (2017).
Sorokina, S. A., Li, C., Wettstein, J. J. & Kvamstø, N. G. Observed atmospheric coupling between Barents Sea ice and the warm-Arctic cold-Siberian anomaly pattern. J. Clim. 29, 495â511 (2016).
Jakobson, E. et al. Validation of atmospheric reanalyses over the central Arctic Ocean. Geophys. Res. Lett. 39, L10802 (2012).
Dee, D. P. et al. The ERA-Interim reanalysis: configuration and performance of the data assimilation system. Q. J. R. Meteorol. Soc. 137, 553â597 (2011).
Martin, G. M. et al. The HadGEM2 family of Met Office Unified Model climate configurations. Geosci. Model Dev. 4, 723â757 (2011).
Hazeleger, W. et al. EC-Earth V2.2: description and validation of a new seamless earth system prediction model. Clim. Dynam. 39, 2611â2629 (2012).
Blackport, R. & Kushner, P. J. Isolating the atmospheric circulation response to Arctic sea ice loss in the coupled climate system. J. Clim. 30, 2163â2185 (2017).
Blackport, R. & Kushner, P. J. The transient and equilibrium climate response to rapid summertime sea ice loss in CCSM4. J. Clim. 29, 401â417 (2016).
McCusker, K. E. et al. Remarkable separability of circulation response to Arctic sea ice loss and greenhouse gas forcing. Geophys. Res. Lett. 44, 7955â7964 (2017).
Oudar, T. et al. Respective roles of direct GHG radiative forcing and induced Arctic sea ice loss on the Northern Hemisphere atmospheric circulation. Clim. Dynam. 49, 3693â3713 (2017).
Peings, Y. & Magnusdottir, G. Response of the wintertime Northern Hemisphere atmospheric circulation to current and projected Arctic sea ice decline: a numerical study with CAM5. J. Clim. 27, 244â264 (2014).
Deser, C., Sun, L., Tomas, R. A. & Screen, J. Does ocean coupling matter for the northern extratropical response to projected Arctic sea ice loss? Geophys. Res. Lett. 43, 2149â2157 (2016).
Screen, J. A. et al. Consistency and discrepancy in the atmospheric response to Arctic sea-ice loss across climate models. Nat. Geosci. 11, 155â163 (2018).
Screen, J. A. Simulated atmospheric response to regional and pan-Arctic sea ice loss. J. Clim. 30, 3945â3962 (2017).
Woods, C., Caballero, R. & Svensson, G. Large-scale circulation associated with moisture intrusions into the Arctic during winter. Geophys. Res. Lett. 40, 4717â4721 (2013).
Sato, K., Inoue, J. & Watanabe, M. Influence of the Gulf Stream on the Barents Sea ice retreat and Eurasian coldness during early winter. Environ. Res. Lett. 9, 084009 (2014).
Sun, L., Deser, C. & Tomas, R. A. Mechanisms of stratospheric and tropospheric circulation response to projected Arctic sea ice loss. J. Clim. 28, 7824â7845 (2015).
Kim, B.-M. et al. Weakening of the stratospheric polar vortex by Arctic sea-ice loss. Nat. Commun. 5, 4646 (2014).
Zhang, P., Wu, Y. & Smith, K. L. Prolonged effect of the stratospheric pathway in linking BarentsâKara Sea sea ice variability to the midlatitude circulation in a simplified model. Clim. Dynam. 50, 527â539 (2018).
Nakamura, T. et al. The stratospheric pathway for Arctic impacts on midlatitude climate. Geophys. Res. Lett. 43, 3494â3501 (2016).
Zhang, P. et al. A stratospheric pathway linking a colder Siberia to BarentsâKara Sea sea ice loss. Sci. Adv. 4, eaat6025 (2018).
Peings, Y. Ural blocking as a driver of early-winter stratospheric warmings. Geophys. Res. Lett. 46, 5460â5468 (2019).
Screen, J. A. The missing Northern European winter cooling response to Arctic sea ice loss. Nat. Commun. 8, 14603 (2017).
Cavalieri, D. J., Parkinson, C. L., Gloersen, P. & Zwally, H. J. Sea Ice Concentrations from Nimbus-7 SMMR and DMSP SSM/I-SSMIS Passive Microwave Data, Version 1 (NSIDC, 1996); https://doi.org/10.5067/8GQ8LZQVL0VL
Acknowledgements
We thank the ECMWF for making the ERA-Interim reanalysis data available for use. The HadGEM2 model simulations were performed on the ARCHER UK national computing service. R.Blackport and J.A.S. were supported by Natural Environment Research Council grant number NE/P006760/1. For the creation of maps included in all figures, the authors used Python package âbasemapâ (https://matplotlib.org/basemap/), copyright Jeffrey Whitaker 2011.
Author information
Authors and Affiliations
Contributions
R.Blackport conceived the study, analysed the data and wrote the manuscript. J.A.S. provided guidance on writing the manuscript and interpreting the results. R.Blackport and K.W. performed the climate model simulations. All authors contributed to the design of model simulations and commented on the manuscript.
Corresponding author
Ethics declarations
Competing interests
The authors declare no competing interests.
Additional information
Peer review information: Nature Climate Change thanks John Fyfe, Qiuhong Tang and the other, anonymous, reviewer(s) for their contribution to the peer review of this work.
Publisherâs note: Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Supplementary information
Supplementary Information
Supplementary Figs. 1â12, Notes 1â5 and references.
Rights and permissions
About this article
Cite this article
Blackport, R., Screen, J.A., van der Wiel, K. et al. Minimal influence of reduced Arctic sea ice on coincident cold winters in mid-latitudes. Nat. Clim. Chang. 9, 697â704 (2019). https://doi.org/10.1038/s41558-019-0551-4
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1038/s41558-019-0551-4
This article is cited by
-
The atmospheric connection between the Arctic and Eurasia is underestimated in simulations with prescribed sea ice
Communications Earth & Environment (2024)
-
Drivers of summer Arctic sea-ice extent at interannual time scale in CMIP6 large ensembles revealed by information flow
Scientific Reports (2024)
-
Significant contribution of internal variability to recent BarentsâKara sea ice loss in winter
Communications Earth & Environment (2024)
-
Recent autumn sea ice loss in the eastern Arctic enhanced by summer Asian-Pacific Oscillation
Nature Communications (2024)
-
Winter âwarm Arctic-cold Eurasiaâ pattern and its statistical linkages to oceanic precursors during the era of satellite observations
Climate Dynamics (2024)