First 4 lectures init Flashcards

1
Q

Description of Upper Mixed Layer

A
  • Layer at surface of ocean of ocean driven by winds and possibly convection via T & S fluxes
  • Turbulence is present which homogenises momentum, temperature and salinity
  • Thickness 10-200m depending on stratification & season
  • Directly below is permanent thermocline
  • Thermocline stretches from 300-1000m and is steep T gradient
  • A seasonal thermocline may also be present
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

Physical Description of Ekman layer

A
  • Layer at top of ocean directly influenced by wind stress
  • Ocean currents at the surface are 45 to the wind direction (R in N hemi)
  • Ekman spiral where magnitudes of currents decay exponentially and at increasing angle to wind with depth
  • Vertically intergrated transport perpendicular to wind stress direction
  • Balance between coriolis and vertical viscous effects (coriolis, drag, wind)
  • 50-300m depth
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Why is there Ekman Pumping at the equator?

A

Sign of coriolis changes across the equator resulting in divergence of surface currents resulting from trade winds.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

What are the units of flux?

A
Q = X m-2 s-1   e.g. J m-2 s-1
Q = Qm-2 (Watts per m squared)
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

What is an f-plane approximation?

When is it used?

A

Assume Coriolis force is constant

Describing flow in small regions relative to the radius of earth but larger than few 10s km

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

What is an beta-plane approximation?

When is it used?

A

For larger domains than f-plane where Coriolis assumed to vary linearly with latitude

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

What are the major aspects of circulation in N. Atlantic

A
  • Basin scale sub-tropical and sub-polar gyres
  • WBC, the gulf stream
  • Gulf stream recirculation due to baroclinic instability (2-3x mass transport as larger gyre)
  • Equatorial current and counter-currents
  • Strong cross equatorial flow in West
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

What behaviour do we expect for large reynolds numbers?

A

Turbulent behavior

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

What is turbulent behavior

A
  • Property of fluid flow
  • Irregular and unpredictable advection of interacting vortices
  • on varying temporal and spatial scales
  • where small perturbations can grow rapidly
  • Leads to enhanced mixing of momentum
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

Describe the four principal processes that influence freshwater fluxes

A
  • Evap
  • Ppt
  • River runoff
  • Ice freeze/melt
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

List four components of heat flux in order of their relative magnitudes close to the equator

A

Shortwave (insolation)
Latent
Longwave
Sensible

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

Describe the concept of eddy diffusivity

A

-Large Reynolds no
- Turbulent Behaviour
- Leads to enhanced mixing of momentum
-

How well did you know this?
1
Not at all
2
3
4
5
Perfectly