3A Basic Physical Oceanography Flashcards

1
Q

What is pressure?

A

force pressing against an object

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2
Q

what happens when pressure is not uniform?

A

not force goes from the high pressure side to the low pressure side

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3
Q

what makes pressure not as strong in the ocean

A

liquid is almost incompressible, pressing down on it causes it to push out laterally

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4
Q

which direction does pressure come from in the ocean

A

all directions

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5
Q

what is hydrostatic balance

A

pressure below a water parcel is slightly higher to balance pressure and gravity coming from above

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6
Q

what are the two forces in the ocean at rest

A

gravity
pressure gradient

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7
Q

what is the equation representing the balance of forces in the ocean at rest

A

Fgravity = - Fpressure
-pg = deritive of p/z

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8
Q

what direction to pressure and gravity work in

A

vertical

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9
Q

equation for mass

A

density x volume

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10
Q

equation for weight

A

mass x g

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11
Q

what is the weight per unit area

A

integral of density gravity area per vertical depth

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12
Q

what is hydrostatic pressure

A

weight of the water above per unit area

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13
Q

how does density vary with depth

A

heavier as we got deeper

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14
Q

what is happening horizontally in terms of pressure gradients

A

spatial changes in density cause very small gradients
compared to the vertical

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15
Q

what can cause pressure to vary horizontally at a given depth

A

surface height variation
horizontal density variations

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16
Q

what happens to light availability as we go deeper into the ocean

A

decreases exponentially

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17
Q

what is the two layer ocean model

A

a layer where photosynthesis is significant and one underneath that is not significant
2 weakly stratified layers

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18
Q

does the layer boundary in the two layer model change?

A

yes, depending on processes we’re considering

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19
Q

what is one way to choose an interface depth in a two layer approximation from a sigma t and depth graph?

A

choose spot where density is changing rapidly with depth

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20
Q

benefits of the two layer model

A

simplify conceptually

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21
Q

what causes the pressure to increase in a two layer model

A

raising the ocean surface
raising the interface surface

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22
Q

what is the equation for pressure

A

P = pgh

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23
Q

what is different about the pressure change at from change of height at the surface vs the interface

A

need to consider the lost/gained amount of pressure from the other layer when the interface height changes

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24
Q

what does a change in density below you cause in water

A

nothing, density is allows weight of water above you

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25
what causes mixing to work faster?
turbulence
26
what does moleculatr mixing depend on?
transport of heat due to diffusion Fd
27
how fast is molecular mixing
slow, works best over sharp gradients
28
what does turbulent mixing depend on
transport of heat due to diffusion transport of heat by turbulent flow Fd + Fadvective
29
how fast is turbulent mixing
much faster than molecular mixing
30
how is turbulence enhancing molecular diffusion
stretching fluid increase SA wide range of scales highly intermittent in the ocean
31
what is the main thing that causes mixing in the ocean
turbulent eddies
32
what direction can eddies mix?
both horizontal and vertical
33
what are the two ways to generate turbulence?
shear convection
34
what is shear?
spatial gradient in flow velocity (fast moving water beside/above/below slow moving water
35
what are examples of turbulence caused by shear
tides/ internal waves wind-driven mixing
36
what is convection?
movement caused by less dense fluid rising and more dense fluid sinking because of gravity unstable densities cause vertical turbulence
37
examples of turbulence caused by convection
winter cooling at surface freezing/evaporation causing high salinity at surface double diffusion process
38
what do tides cause
strong mixing near the bottom internal waves on rough bottoms
39
what are internal waves
wave that are 5-10 meters down moving water faster over another neighbour layer break causes mixing
40
what are the causes of internal waves
winds tides
41
wind driven mixing
wind moving the surface layer faster than below layers surface wave and top layer wave breaking causes mixing
42
what is type one of convection driven mixing?
classic convection
43
what is classic convection
convection due to 'classic' convection instability dense water going under lighter water
44
what are examples of classic convection
winter cooling at surface freezing/evaporation causing high salinity at surface
45
what is type two of convection driven mixing?
double diffusion
46
what is double diffusion
convection driven by two different density gradients with different rates of diffusion
47
what are the two types of double diffusion
diffusive instability fingering instability
48
diffusive instability
cold, fresh (light) water above warm salty (dense) water
49
fingering instability
warm salty (light) water above cold fresh water (dense)
50
what is the basic steps of finger instability
perturbation causes tongues to enter each layer from each layer water diffuses 100 faster than salt, so water changes temperature and becomes lighter/denser becomes heavier/lighter than other water until salt has also diffused
51
what kind of eddies cause stronger/faster mixing
faster bigger
52
why does more mixing happen horizontally vs vertically
much more energy to move water across density surfaces (up/down) than acroess density surfaces (sides)
53
what can cause more mixing to occur in the vertical
when water is less stratified and vice versa
54
what two processes are happening at the surface mixing layer
wind is mixing surface, less stratified sun is warming surface, more stratified
55
what kind of energy does wind change? how?
increase kinetic energy of mixing indirectly increase potential energy of stratification by making density difference smaller between surface and depth; moves center of mass up
56
what kind of energy does cooling/evaporation change? how?
increase potential energy of stratification by making density difference smaller between surface and depth; moves center of mass up
57
what kind of energy does solar warming change
decrease potential energy of stratification by making density differences larger
58
what kind of energy does rain/runoff change
decrease potential energy of stratification by making density differences larger
59
mixing layer
region of the upper ocean that is actively mixing not necessarily mixed yet processes that change mixing energy affect depth
60
surface mixed layer
region of upper ocean that is homogeneous not necessarily mixing now
61
why does the mixed layer deepen in the fall
cooling strong winds
62
when is maximum depth of mixed layer usually
early spring
63
why does the mixed layer shallow in the spring
warming weak winds