Lecture 1 & 2 Flashcards

1
Q

Purpose of Oceanography

A

ocean circulation and climate linked

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2
Q

Fundamental Properties of Water

A

1) Temperature
2) Salinity
3) Desnity
4) Transmission of light and sound

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3
Q

Structure of pure water

A

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

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4
Q

Latent heat capacity

A

heat/energy needed to phase change

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5
Q

Effect of adding salt

A

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

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6
Q

Osmotic Pressure

A

molecules from high concentration to low concentration

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7
Q

Factors influencing ocean temperature

A

Solar radiation = more at equator and less at poles

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8
Q

How does the ocean moderates Earth’s temperature

A

Thermal inertia of ocean surface water
o Annual freezing and thawing of ice
o Movement of water vapour from tropics to poles

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9
Q

Temperature profile

A

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)

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10
Q

Salinity of ocean

A

Surface = similar to temperature (not equator)
controlled by evaporation/precipitation
Variation = freshwater discharge/storms

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11
Q

Salinity profile

A

Well-mixed, halocline, deep ocean

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12
Q

Density increases with

A

increasing salinity and pressure

decreasing temperature

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13
Q

How do we measure density?

A

salinity, pressure + temp

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14
Q

Potential Density

A

corrected density for compression

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15
Q

Density profile

A

well-mixed, pycnocline - barrier to mixing + freezing, deep ocean

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16
Q

Light Absorption

A

Purple/red absorbed rapidly (ultrared/infrared)

blue/green reflected

17
Q

Sound travelling in water

A

3x faster in water

Highly NON-LINEAR

18
Q

Instruments to Measure Water Properties

A
CTD Measurement (Conductivity - Salinity, Temperature, Depth - pressure)
Bathythermographs
-	Provide vertical profile of temperature & pressure
-	Sensor head freefalls while transmitting data back through uncoiling wire
Drifters
-	SOFAR Float
-	RAFOS
-	ARGO
-	ALACE
-	PALACE
-	APEX
-	Slocum Glider
19
Q

Shadow zones

A

A zone where the divergence of sound waves creates a region that has little sound energy penetration.