Steric sea level is driven by volume changes
through ocean salinity (halosteric) and ocean temperature (thermosteric) effects, from which the latter is known to play a dominant role in observed contemporary rise of GSSL.
Not exact matches
Along one string of sites, or «stations,» that stretches from Antarctica to the southern Indian
Ocean, researchers have tracked the conditions of AABW — a layer of profoundly cold water less than 0 °C (it stays liquid because of its salt content, or salinity) that moves through the abyssal ocean, mixing with warmer waters as it circulates around the globe in the Southern Ocean and northward into all three of the major ocean ba
Ocean, researchers have tracked the conditions of AABW — a layer of profoundly cold water less than 0 °C (it stays liquid because of its salt content, or
salinity) that moves
through the abyssal
ocean, mixing with warmer waters as it circulates around the globe in the Southern Ocean and northward into all three of the major ocean ba
ocean, mixing with warmer waters as it circulates around the globe in the Southern
Ocean and northward into all three of the major ocean ba
Ocean and northward into all three of the major
ocean ba
ocean basins.
Since salt is (for these purposes) a conserved variable in the
ocean, mean changes in
salinity can only occur
through fresh water addition.
They have to be quick to react, because different masses of water are often very different in
salinity, pH, DIC, and alkalinity... if the
ocean creatures couldn't adapt very quickly to the shock of some storm - or current - driven new water mass coming
through the area where they live, they'd have gone extinct millennia ago.
Better characterize the deep
ocean to quantify the role of deep temperature and
salinity signals that contribute to AMOC variability
through enhancements to the observing system that directly measure deep
ocean properties (temperature,
salinity, and velocity) such as Deep Argo, Deep gliders, and moored instrumentation.
It seems unlikely, for example, that the
salinity of a particular
ocean location will change dramatically from one period to another unless the two time periods are separated by tens of millions of years (
through moving continents) or there's some extraordinary temporary event (such as the emptying of a large glacial lake) just before one of the two measuring points.
Currents that move
through the upper
ocean then dive down to depth may move some of the surface heat to the deeper waters, especially where the currents have dived not just from cooling water (hot water would tend to go up, cold water would tend to go down) but because it is driven in «conveyor» systems which may run counter to expectations of where water should go when considering only local conditions, and especially, if the water is dropping because of an increase in
salinity.
The flow of freshwater from the northern continents represents an export to the world
ocean that goes almost entirely into the Atlantic, about 5.1 Sv passing as relatively low
salinity water
through the passages between Greenland and Ellesmere Island into the Labrador Sea, a flow of low
salinity water that can subsequently be traced around the subpolar gyre.
Meridional Overturning Circulation includes the action of wind, as well as density changes
through differences in temperature and
salinity in order to drive the
ocean currents.
Perhaps the model results do open a door for Arctic geoengineering approaches though, for instance by influencing Arctic
Ocean salinity and heat transport or
through Arctic solar radiation management.
Ocean temperature (bottom) and
salinity (top) at 450 - m depth below Petermann Gletscher from May - 25
through June - 16 2017 (red) and 2016 (black).