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Atmospheric Blocking and Atlantic Multidecadal Ocean Variability

Atmospheric blocking over the northern North Atlantic, which involves isolation of large regions of air from the westerly circulation for 5 days or more, influences fundamentally the ocean circulation and upper ocean properties by affecting wind patterns. Winters with clusters of more frequent block...

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Published in:Science (American Association for the Advancement of Science) 2011-11, Vol.334 (6056), p.655-659
Main Authors: Häkkinen, Sirpa, Rhines, Peter B., Worthen, Denise L.
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Language:English
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description Atmospheric blocking over the northern North Atlantic, which involves isolation of large regions of air from the westerly circulation for 5 days or more, influences fundamentally the ocean circulation and upper ocean properties by affecting wind patterns. Winters with clusters of more frequent blocking between Greenland and western Europe correspond to a warmer, more saline subpolar ocean. The correspondence between blocked westerly winds and warm ocean holds in recent decadal episodes (especially 1996 to 2010). It also describes much longer time scale Atlantic multidecadal ocean variability (AMV), including the extreme pre-greenhouse-gas northern warming of the 1930s to 1960s. The space-time structure of the wind forcing associated with a blocked regime leads to weaker ocean gyres and weaker heat exchange, both of which contribute to the warm phase of AMV.
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subjects Atmospheric circulation
Atmospherics
Climate
Climate change
Climate models
Climatology. Bioclimatology. Climate change
Curl
Earth, ocean, space
Exact sciences and technology
External geophysics
Gyres
Meteorology
Meteorology And Climatology
Ocean circulation
Ocean-atmosphere interaction
Oceans
Physics of the oceans
Sea-air exchange processes
Storms
Subtropics
Time series
Winds and their effects
title Atmospheric Blocking and Atlantic Multidecadal Ocean Variability
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