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Ocean Structure and Circulation
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Mixed Layer
a surface layer ten to a few hundred of meters thick
Thermocline
a region extending from the bottom of the mixed layer to a depth of about 1000 m
Isothermal Layer
a layer of constant temperature
Halocline
marked change in salinity with depth
Pycnocline
closely follows the thermocline; extends from the bottom of the mixed layer to a depth of about 1000 m
If the density of the water increases with depth, the water column from the surface to that depth is _________.
stable
If there is higher density water on top of lower density water, the water column is __________.
unstable
Continuity of flow
because water is a fixed quantity in the oceans, it cannot be accumulated at one location or removed at another location without movement of water between those locations
Thermohaline circulation
motion caused by variations in density due to differences in temperature and salinity
Downwelling zones
areas of thermohaline circulation where water sinks
Upwelling zones
areas of rising waters
Convergence
formed when the surface waters are driven together by the wind or against a coast
Divergence
occurs when the wind blows surface waters away from an area or a coast
Isopycnal
when the water column has the same density over depth, it has neutral stability
Isothermal
water temperature is unchanging over depth
Isohaline
salinity is constant over depth
Caballing
mixture of two water types with the same density – produces new water types with greater density that will sink
What happens at downwelling zones?
Transports oxygen-rich surface water to depth, where it is needed for deep living animals
What happens at upwelling zones?
Returns low-oxygen content water with dissolved, decay produced nutrients to the surface, where the nutrients act as fertilizers to promote photosynthesis and the production of more oxygen in sunlit surface waters
Water at a convergence ___________.
sinks or downwells
Water at a divergence __________________.
upwells from below