Physical Oceanography Flashcards

1
Q

% of water that the ocean holds
ice
ground water

A

97.6–> 137010^6km3
2.1
0.5
rest <0.001

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2
Q

Unique properties of seawater

A

High heat capacity- raise temp of 1g by 1degrees

greater solvent power than any other substance

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3
Q

Why is temperature important

A

reflects
the amount of heat held and transported by
the ocean.

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4
Q

temperature range in ocean

A

-2–28

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5
Q

The temperature of the ocean is primarily

influenced by

A

the heating at the air-sea

interface

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6
Q

define thermocline

A

a steep temperature gradient in a body of water such as a lake, marked by a layer above and below which the water is at different temperatures

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7
Q

Salinity

A

Total dissolved solids (mainly sodium chloride,
or “table salt”)
- About 3.5% by weight (average seawater)
- Usually expressed as 35 0/00 (parts per
thousand, ppt or practical salinity units, psu)
- Varies geographically according to
Evaporation, precipitation, rivers, ice
formation and ice melt.

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8
Q

Evaporation versus precipitation

A

evaporation generally exceeds precipitation
The balance is restored by rain over the
continents, returning water via rivers

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9
Q

Define halocline

A

a well-defined vertical salinity gradient in ocean or other saline water.

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10
Q

define density (p)

A

Density is the mass of sea water per unit volume.

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11
Q

Density depends on

A

Density depends on salinity, temperature and
pressure.
- Density increases with increasing salinity
- Density increases with decreasing temperature
• Seawater density ranges from 1021 – 1070 kg/m³
,
the average density is 1025 kg/m³
increases with pressure

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12
Q

lighter water is

A
  • warmer
  • less saline
  • shallower
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13
Q

denser water is

A

colder
• more saline
• deeper

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14
Q

define pycnocline

A

layer in an ocean or other body of water in which water density increases rapidly with depth

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15
Q

NADW

AABW

A

North Atlantic Deep Water

Antarctic Bottom Water

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16
Q

3 defining characteristics of GFD

A

Geophysical Fluid Dynamics
aspect
ratio, stratification, and rotatio

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17
Q

Oceans aspect ratio is large or small

A

large
horizontal/ vertical scale
like a piece of paper

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18
Q

The Coriolis force (rotation force)

A

• acts at right-angles to the actual direction
of water motion.
• causes water to move to the right in the
northern hemisphere
• causes water to move to the left in the
southern hemisphere.

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19
Q

How do surface winds drag the ocean

A

friction

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20
Q

surface winds are

A

a source of energy for the ocean

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21
Q

The extent to which the wind drags the surface

water depends on:

A
  • wind strength
  • wave conditions
  • density stratification
22
Q

give an example of an energy sink

A

friction- causes mixing in the ocean

23
Q

Interior friction

A

depends on the density and the

currents

24
Q

•Bottom friction

A

depends on the bottom currents

and the bottom roughness

25
Ocean pressure
``` is the weight of seawater per unit area mainly a function of depth Pressure in the ocean increases at a rate of about 1 “atmosphere” per 10 m of water ```
26
Pressure=
Height*density*g
27
Pressure gradient force
occurs when there is a horizontal pressure difference | high to low p
28
Explain Ekman transport
• When the wind blows on the ocean, the wind drags the surface layer with it. • Rotation causes the surface layer to deflect to the right (NH) and move at 45o to the wind direction. • Interior friction causes the surface layer to drag on the layer below. • Rotation causes this layer to again deflect to the right (NH). • The resulting currents are called Ekman transport
29
geostrophic balance and the | resulting current is referred to as a geostrophic current
• Suppose we have a difference in sea-level height. Water will be accelerated from the region of high pressure towards the region of low pressure. • As the water starts to move, the Coriolis effect (rotation) deflects the water to the right (NH) or left (SH). • The water keeps getting deflected until the force due to the pressure difference balances the Coriolis force.
30
Most of earth's surface wind energies is concentrated in
the easterlies and westerlies
31
Gyre
Due to wind-generated pressure differences and the Coriolis effect water typically moves in a circular pattern
32
effects of ocean currents
transfer heat from tropical to polar regions •influence weather and climate •distribute nutrients
33
Upwelling
refers to the process where deeper, colder, and potentially nutrient-rich water is brought to the surface
34
Why is upwelling important
it uplifts nutrients to depths where there is light (recall that both light and nutrients are needed for photosynthesis to occur). more nutrients at greater depth
35
Equatorial upwelling
The winds are predominantly easterly (or westward) along the Equator. • In the southern hemisphere the Ekman transport is to the left of the wind. • In the northern hemisphere the Ekman transport is to the right of the wind. • This corresponds to a divergence in the Ekman transport at the equator and results in equatorial upwelling
36
Wind-driven coastal upwelling
In coastal regions, when the wind blows parallel to the coast the Ekman transport is either directed onshore or offshore. • When the Ekman transport is offshore, upwelling results. • The offshore Ekman transport is “balanced” by an onshore flow below the surface Ekman layer. • As a result, colder water is uplifted to the surface. • When the Ekman transport is onshore, downwelling results. This is the opposite to upwelling
37
Spring Tides
``` Occur When the Moon Pulls along the same Line as the Sun. (new and full moon). ```
38
Neap Tides
``` Occur When the Moon Pulls at 90o to the Sun (first and last quarter moon) ```
39
Tidal waves
have wavelengths (L) on the order of 1/2 the diameter of the earth or about 20,000 km. • Since the ocean is about 4km deep, and since L/20 is about 1000km, tidal waves are shallow water waves
40
What are waves (4 points)
A wave transfers a disturbance from one part of a material to another 2. The disturbance is propagated through the material without any substantial overall motion of the material itself. 3. The disturbance is propagated without any significant distortion of the wave form. 4. The disturbance appears to be propagated with constant speed (unless fluid depth is shallow and changing).
41
what is being transported by a wave
energy
42
Surface waves
Waves which occur at an interface (wind raindrops earthquakes) Generating force = Restoring force
43
Surface waves on water--> 2 restoring forces?
Gravitational force | surface tension
44
Pressure in the vertical & buoyancy | Archimedes principle:
the upthrust force = the weight of water displaced
45
capillary waves
For waves with wavelengths less than about 1.7 cm, the principal restoring force is surface tension
46
Gravity Waves
Travel On Density Surfaces
47
Wave Speed
(length of wave) / (wave period)
48
The period of a wave remains the same
(determined by generating force)
49
Wave trains
packets of similar waves with approximately the same | period and speed
50
Wave refraction
close to the shoreline. Waves approaching shore at an angle first “feel bottom” close to shore, slowing them down there and causing waves to align themselves to the coastline
51
As a wave breaks, the energy it received from the wind is | dissipated.- where does it go
ØSome energy is reflected back out to sea. ØMost of the energy is dissipated as heat and sound (the ‘roar’ of the surf) in the final small-scale mixing of foaming water, sand and shingle. ØSome energy is used in fracturing large rock or mineral particles into smaller ones. ØSome energy is used to move sediments.