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Springtime atmospheric energy transport and the control of Arctic summer sea-ice extent

Abstract

The summer sea-ice extent in the Arctic has decreased in recent decades, a feature that has become one of the most distinct signals of the continuing climate change1,2,3,4. However, the inter-annual variability is large—the ice extent by the end of the summer varies by several million square kilometres from year to year5. The underlying processes driving this year-to-year variability are not well understood. Here we demonstrate that the greenhouse effect associated with clouds and water vapour in spring is crucial for the development of the sea ice during the subsequent months. In years where the end-of-summer sea-ice extent is well below normal, a significantly enhanced transport of humid air is evident during spring into the region where the ice retreat is encountered. This enhanced transport of humid air leads to an anomalous convergence of humidity, and to an increase of the cloudiness. The increase of the cloudiness and humidity results in an enhancement of the greenhouse effect. As a result, downward long-wave radiation at the surface is larger than usual in spring, which enhances the ice melt. In addition, the increase of clouds causes an increase of the reflection of incoming solar radiation. This leads to the counter-intuitive effect: for years with little sea ice in September, the downwelling short-wave radiation at the surface is smaller than usual. That is, the downwelling short-wave radiation is not responsible for the initiation of the ice anomaly but acts as an amplifying feedback once the melt is started.

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Figure 1: Arctic sea-ice extent and ice-concentration anomalies for September, 1979–2010.
Figure 2: Radiative and turbulent flux anomalies at the surface for LIYs.
Figure 3: Atmospheric water content and energy convergence anomalies for LIYs.

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Acknowledgements

This work is part of the ADSIMNOR programme, funded by a grant from the Swedish research council Formas. The ECMWF ERA-Interim reanalysis data are obtained from the ECMWF data server and the sea-ice extent from the NSIDC.

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The original idea for the paper was suggested by R.G.G. and discussed and developed by all authors. The data analysis was carried out by M-L.K., who also prepared the figures. M-L.K. and R.G.G. wrote the manuscript and M.T. provided feedback. All authors contributed to the discussion and interpretation of the results.

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Correspondence to Marie-Luise Kapsch.

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The authors declare no competing financial interests.

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Kapsch, ML., Graversen, R. & Tjernström, M. Springtime atmospheric energy transport and the control of Arctic summer sea-ice extent. Nature Clim Change 3, 744–748 (2013). https://doi.org/10.1038/nclimate1884

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