Ocean Structure Flashcards
Density stratification
Density almost always increases with depth in the ocean
3 layers:
* surface mixed layer
* Upper water in pycnocline/thermocline
* deep water
Main control on density
- temperature
- pycnocline often mirros the thermocline
- exceptions: polar regions, coastal areas
Stable stratification
More dense beneath less dense
Depth of neutral buouyancy
Where a water parcel has the same density as the surroundung waters
Surface mixed layer
- No stratification
- All properties well mixed
- Drivers of mixing: wind stress, wave breaking, sea spray, evaporation/precipitation, heat transfer
Ocean horizontal structure
Geographical variations in stratification
Polar regions - thermocline and pycnocline are usually weak, but they are there, more uniform water column
Tropics - big change in temp/desnity with depth
Density is important driver of ocean dynamics
- differences in density can both prohibit movemenr and casue movement of water
- Horixontal density gradients are main driver of ocean currents
- Vertical density gradients inhibit motion and inhibit mixing
- waves propogate on density interfaces in the ocean = internal waves
- desne waters from polar region fill in the deep ocean
Water mass
a parcel of water with a distinct range of temp and salinity characteristics
LeConte T/S