Temperature:
-
varies considerably at the surface of the ocean but little variation at depth
- there is a gradual decrease in temperature with depth
- a cold, highly saline, deep mass of water is very dense, while a warm, less saline, surface water mass is less dense
- when larger masses of water meet with different densities, denser water mass slips under the less dense mass
- because of these responses, this is the reason for some of the deep ocean circulation patterns
Salinity:
-
concentrations of salt are higher in warm seas due to high evaporation rates
- salinity increases with depth