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Changes in Arctic melt season and implications for sea ice loss

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Stroeve, J. C., Markus, T., Boisvert, L., Miller, J., Barrett, A.·2014·Geophysical Research Letters

Abstract

The Arctic‐wide melt season has lengthened at a rate of 5 days decade−1 from 1979 to 2013, dominated by later autumn freezeup within the Kara, Laptev, East Siberian, Chukchi, and Beaufort seas between 6 and 11 days decade−1. While melt onset trends are generally smaller, the timing of melt onset has a large influence on the total amount of solar energy absorbed during summer. The additional heat stored in the upper ocean of approximately 752 MJ m−2 during the last decade increases sea surface temperatures by 0.5 to 1.5 °C and largely explains the observed delays in autumn freezeup within the Arctic Ocean's adjacent seas. Cumulative anomalies in total absorbed solar radiation from May through September for the most recent pentad locally exceed 300–400 MJ m−2 in the Beaufort, Chukchi, and East Siberian seas. This extra solar energy is equivalent to melting 0.97 to 1.3 m of ice during the summer.

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Metadata

Authors
Stroeve, J. C., Markus, T., Boisvert, L., Miller, J., & Barrett, A.
Venue
Geophysical Research Letters
Published
2014-02-22
Volume
41
Issue
4
Pages
1216-1225
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2159841501
Cited by
748
References
0
FWCI
43.69
Type
journal article
Language
en
Open access
hybrid

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CoChat. (2026). Citation check: Changes in Arctic melt season and implications for sea ice loss. https://app.cochat.ai/papers/10.1002/2013gl058951
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Stroeve, J. C., Markus, T., Boisvert, L., Miller, J., & Barrett, A. (2014). Changes in Arctic melt season and implications for sea ice loss. Geophysical Research Letters. https://doi.org/10.1002/2013gl058951

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