Oceanography Exam 3 UMASS
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thermohaline circulation
movement of ocean water between the surface and deeper layers, driven by differences
in temperature (thermo) and salinity (haline), which cause changes in water density
Starting from the surface: 1)
Thermocline
Starting from the surface: 2)
Mediterranean Intermediate Water (MIW)
Which was does Mediterranean Intermediate Water (MIW) flow?
right to left (←)
Starting from the surface: 3)
Antarctic Intermediate Water (AAIW)
Which was does Antarctic Intermediate Water (AAIW) flow?
right to left (←)
Starting from the surface: 4)
North Atlantic Deep Water (NADW)
Which was does North Atlantic Deep Water (NADW) flow?
left to right (→)
Starting from the surface: 5)
Antarctic Bottom Water (AABW)
Which was does Antarctic Bottom Water (AABW) flow?
right to left (←)
2nd defintion of thermohaline circulation
the density-driven circulation of the ocean below the pycnocline
- both temperature and salinity are important in the production of bottom, deep, and
intermediate water masses
Where does deep water acquire its physical and chemical characteristics?
At the surface where they formed