Lecture 1 & 2 Flashcards
Purpose of Oceanography
ocean circulation and climate linked
Fundamental Properties of Water
1) Temperature
2) Salinity
3) Desnity
4) Transmission of light and sound
Structure of pure water
H2O covalently bonded @105 degrees -> charge bias
High surface tension due to ‘stick’ of molecules
High heat capacity
High latent heat capacity
Density = max @3.98 degrees
Latent heat capacity
heat/energy needed to phase change
Effect of adding salt
Increased
o Boiling point
o Density
o Surface tension
o Electrical conductivity (due to charges)
o Osmotic pressure
Decreased
o Heat capacity Less heat required to raise the temperature
o Freezing point Extra ions disrupt ice crystal formation
o Maximum density temperature Extra ions change packing arrangements
o Vapour pressure
Osmotic Pressure
molecules from high concentration to low concentration
Factors influencing ocean temperature
Solar radiation = more at equator and less at poles
How does the ocean moderates Earth’s temperature
Thermal inertia of ocean surface water
o Annual freezing and thawing of ice
o Movement of water vapour from tropics to poles
Temperature profile
Epipelagic zone heated most
Epilimnion = mixed layer (50-500m)
Thermocline = Rapid temp decrease (500m - 1000m) seasonal @ mid-lat, max @ summer + absent winter
high-lat -> thin/absent (maintained by upwelling)
Hypolimnion = deep ocean (>2500m)
Salinity of ocean
Surface = similar to temperature (not equator)
controlled by evaporation/precipitation
Variation = freshwater discharge/storms
Salinity profile
Well-mixed, halocline, deep ocean
Density increases with
increasing salinity and pressure
decreasing temperature
How do we measure density?
salinity, pressure + temp
Potential Density
corrected density for compression
Density profile
well-mixed, pycnocline - barrier to mixing + freezing, deep ocean