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David F. Porter, John J. Cassano and Mark C. Serreze Local and large-scale atmospheric responses to reduced Arctic sea ice and ocean warming in the WRF model Journal of Geophysical Research: Atmospheres (1984–2012) 117

Version of Record online: 12 JUN 2012 | DOI: 10.1029/2011JD016969

Key Points

  • When sea ice is reduced in WRF, surface turbulent heat fluxes increase
  • A warmer and moister atmosphere increases liquid cloud cover and precipitation
  • Low latitude SST changes have some effects on the Arctic atmosphere

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