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Alexandra Jahn and Marika M. Holland Implications of Arctic sea ice changes for North Atlantic deep convection and the meridional overturning circulation in CCSM4-CMIP5 simulations Geophysical Research Letters 40

Version of Record online: 26 MAR 2013 | DOI: 10.1002/grl.50183

Key Points

  • Deep convection in the North Atlantic ceases by 2145 in RCP8.5
  • The deep convection stops due an increase in the Arctic freshwater export
  • The deep convection shuts down abruptly, but the MOC shows no abrupt changes

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