- overturning circulation, density of surface water in atlantic greater than other oceans due to high salinity, in northern winter, atmosphere extreacts huge amounts of heat from waters of north atlantic, water can become dense enough to sink to the bottom of the ocean, initiates the oceans' deep overturning circulation, after sinking this water slowly spreads throughout the global ocean and eventurally returns to the surface, thermos refers to fact driven by cooling of N atlantic surface waters, haline refers to face it is drien by waters high salinity