Large Scale Processes (L1-6) Flashcards

1
Q

What is the pycnocline?

A

The density increase between the surface ocean and deep waters, confined to a thin layer
Can be permanent or seasonal
It takes a lot of energy to mix through the pycnocline, therefore is an effective barrier to vertical mixing

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2
Q

Why is the pycnocline important to phytoplankton?

A

They require light from the surface and nutrients from depth, but these are separated by the density stratification of the pycnocline

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3
Q

Why is ocean stratification becoming stronger and what are the impacts of this?

A

More than 90% of the excess atmospheric heating is going into the ocean and causing it to become more stratified (increase by 18% in upper 150m)
This leads to less vertical mixing and more heat in the upper ocean (usually in the form of heatwaves)
This impacts many marine organisms, due the increase in heat, as well as the reduced supply of nutrients and the alteration of productivity, biodiversity, and food webs, and an increase in sedimentation

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4
Q

What does sea water density depend on?

A

Temperature, salinity, pressure

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5
Q

What is cabling?

A

Where water masses have different temperatures and salinities, yet still arrive at the same density

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6
Q

How does temperature affect density?

A

Density increases with decreasing temperature

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7
Q

How does salinity affect density?

A

Density increases with increasing salinity

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8
Q

How does pressure affect density?

A

Density increases with pressure (increasing pressure squeezes water into a smaller volume)

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9
Q

What is Archimede’s Principle?

A

An object submerged in a fluid will experience an upward buoyant force that is equal to the weight of fluid it displaces

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10
Q

What is stable stratification and the consequence of this?

A

This occurs when each layer is less dense than the one below it
Buoyancy forces tend to preserve stable stratification
A consequence of this is that internal waves are formed which propagate horizontally along the pycnocline

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11
Q

What are the impacts of internal waves?

A

They drive cold water into shallow oceans/coastal waters, injecting nutrients into the euphotic zone, transporting marine larvae into coastal areas, and delivering cooler water to coral reefs

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12
Q

What is unstable stratification?

A

This occurs when a layer is denser than the once below it
Buoyancy triggers convection
Cannot persist as buoyant forces will always try to return it back to stable stratification
This could happen near the poles where it cools dramatically in winter

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13
Q

What is hydrostatic pressure?

A

The pressure at any depth in the ocean is the weight of the water that is acting on a unit area
Pressure acts equally in all directions

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14
Q

What is advection?

A

The transport of properties by the flow of a fluid

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15
Q

What is diffusion?

A

The redistribution of properties from an area of higher to lower concentration (spreading)
Requires a concentration gradient

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16
Q

Do advection and diffusion occur together or separately?

A

It is very rare that only one of these processes is occurring at a time

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17
Q

What is volume flux?

A

The volume of fluid passing through a prescribed area per unit time
The flow rate of an ocean current

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18
Q

What is a Sverdrup?

A

A measure of the amount of water
1 million m³/s

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19
Q

What is molecular diffusion?

A

Where properties are redistributed due to random motion of water molecules
Usually a slow process as it relies on the movement of individual particles
It is always at the same constant random motion due to thermal energy

Rate of diffusion is k = 1x10⁻⁷ m²/s

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20
Q

What is eddy diffusion?

A

Where properties are redistributed as a result of stirring by eddies
Large range of spatial scales (mm-km)
Stirring speeds up the rate of mixing, and is much faster than molecular diffusion as more kinetic energy is introduced

Rate of diffusion is k = 500 m²/s

21
Q

What is the principle of continuity?

A

Volume in the ocean must be conserved, volume flux into an area must equal the volume flux out of an area

22
Q

Why is it important that seawater is nearly incompressible?

A

It means a flow that is converging in one direction must be diverging in another direction
Converging leads to downwelling
Diverging leads to upwelling

23
Q

What is Newton’s Second Law of Motion?

A

The rate of change of velocity (acceleration) of an object is equal to the sum of the forces acting upon it, and inversely proportional to the mass of the object

24
Q

What happens if the forces in the ocean are unbalanced?

A

The parcel of water will move in the same direction as the forces
The opposite will occur if the forces are balanced, and the water may not move, or continue at a constant velocity (steady-state), dependent on the magnitude of the force

25
Q

What are the four forces that affect motion in the ocean?

A

Gravity - from the Earth, Moon and Sun
Pressure Gradient Force - from variations in the weight of fluid
Friction - predominantly seen at ocean boundaries (sea surface, sea floor, coastlines)
Coriolis Force - due to the movement of water/air and Earth’s rotation

26
Q

What are the three types of frictional forces in the ocean?

A

Wind stress (accelerating)
Viscosity or internal friction (resistant)
Frictional drag at boundaries (resistant)

27
Q

What way does the Coriolis Force act in the different hemispheres?

A

Acts 90° to the right of motion in the Northern Hemisphere
Acts 90° to the left of motion in the Southern Hemisphere

28
Q

Where is the Coriolis Force the strongest?

A

It is strongest at the poles and weakest at the equator
The faster the motion, the stronger the effect of the Coriolis Force

29
Q

What does the Rossby number tell us?

A

Whether the Coriolis Force is important in a system
Ro < 1 signifies a system affected by the Coriolis Force
Ro <1 indicates a system with little influence from the Coriolis Force

30
Q

When is the Coriolis Force most important?

A

It becomes the most important when travelling relatively slowly over large distances

31
Q

What are the different directions of motion?

A

x = positive east
y = positive north
z = positive up

32
Q

What are the different velocities of motion?

A

u = positive east
v = positive north
w = positive up

33
Q

What are the different accelerations of motion?

A

du/dt = positive east
dv/dt = positive north
dw/dt = positive up

34
Q

Why are ocean surface currents important?

A

They play a role in controlling climate, transporting dissolved and floating material (nutrients, gasses, larvae) and the determine the fate of pollutants in coastal waters

35
Q

What is geostrophic balance?

A

It the horizontal force balance, where the horizontal pressure gradient force and Coriolis force balance each other
It is responsible for large-scale ocean circulation

36
Q

What is occurring if a fluid is in geostrophic balance?

A

The PGF acts from higher toward lower pressure
The PGF and CF act in opposite directions but with equal magnitude
The direction of the geostrophic flow is at 90° to the PGF (R in NH, L in SH)
The velocity of the geostrophic flow is proportional to the strength of the PGF

37
Q

What does satellite altimetry measure?

A

The sea surface height and topography of land

38
Q

Why does the pressure gradient force change with sea surface height?

A

Due to the changes in pressure between the different heights
Higher/taller water column has more density, while a shorter/lower water column is less dense
Gradients in the height of sea surface height produce horizontal pressure gradients

39
Q

What does a circle with a cross mean?

A

Movement into the page

40
Q

What does a circle with a dot mean?

A

Movement out of the page

41
Q

What is Ekman transport?

A

The net movement of fluid within a wind-affected layer (the Ekman layer)
The direction of Ekman transport it at 90° to the wind (R in NH, L in SH)

42
Q

Why is Ekman transport important?

A

It is responsible for the horizontal fluxes of water properties (temperature, salinity, nutrients, gasses, dissolved material, larvae, and marine debris)
Convergences and divergences produce vertical water movement (upwelling and downwelling)

43
Q

What is wind stress?

A

Wind blowing across the sea surface producing a force per unit area

44
Q

How is the direction of wind stress described?

A

Wind stress on the x-axis is τₓ
It is positive towards the east, negative towards the west
Wind blowing west to east (westerly) would have a τₓ > 0

Wind stress on the x-axis is τᵧ
It is positive towards the north, negative towards the south
Wind blowing north to south (northerly) would have a τᵧ < 0

45
Q

What is sheared flow?

A

Where one part of the ocean is moving faster than others causing turbulence

46
Q

What is the Ekman depth?

A

Momentum at the surface from wind stress cause turbulence, which acts as a gearing mechanism and transfers wind stress force down into the water column
As the wind imparts on the surface, turbulence acts to transfer down into the ocean
The depth to which the effects of wind stress are felt is the Ekman depth

47
Q

How long does force balance between wind stress and Coriolis force take to develop?

A

About 36 hours
Varies with the Ekman depth and the strength of the Coriolis force

48
Q

How do the velocities of Ekman transport and wind stress differ?

A

The velocity of flow in the Ekman layer is proportional to the strength of the wind stress
The direction of flow in the Ekman layer is at right angles (R in NH, L in SH) to the direction of the wind stress

49
Q

What happens when the wind stress causes divergences and convergences?

A

Upwelling and downwelling of seawater occur