Ocean heat convergence and north atlantic multidecadal heat content variability

HIGHLIGHTS

• What: The approach is to investigate the upper ocean heat content, as this is an integral part of AMV. These processes are the focus of the present study. As organised changes of OHC over large areas are needed to affect the overlying atmospheric circulation (the Jet Stream and the storm track), the authors focus on the North Atlantic Ocean heat budget over large spatial scales (1000+ km). The model is forced by surface meteorological conditions using the CORE2 surface forcing dataset: 6-hourly 2m air temperature and humidity and 10m wind speed are used to calculate turbulent . . .
  

   

  

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