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A. B. Sandø, Y. Gao and H. R. Langehaug Poleward ocean heat transports, sea ice processes, and Arctic sea ice variability in NorESM1-M simulations Journal of Geophysical Research: Oceans 119

Version of Record online: 21 MAR 2014 | DOI: 10.1002/2013JC009435

Key Points

  • BSO heat transport controls Barents Sea ice cover in terms of congelation growth
  • Bottom melting controls sea ice mass variability in the Central Arctic Ocean
  • Ocean has stronger direct impact on changes in sea ice mass than the atmosphere

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