week 6 - ocean circulation Flashcards

1
Q

three types of water masses with different densities

A
  1. stable
  2. unstable
  3. neutral
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2
Q

stable water mass

A

low density on top, high density on the bottom
- mixing is inhibited

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3
Q

unstable water mass

A

high density on top, low density on bottom
- mixing is spontaneous

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4
Q

neutral water mass

A

density is medium/same on the top and bottom
- mixing is easy

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5
Q

thermocline

A

a region of rapid temperature change
- separates the top mixed layer (turbulent) from the bottom deep water (calm)

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6
Q

pyconocline

A

rapid change in density

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7
Q

where is heat greater?

A

at lower latitudes
-because of this, winds are generated to restore equilibrium
- warm air rises near the equator and travels toward the poles (deflected by coriolis effect)

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8
Q

coriolis effect

A

things moving in the northern hemisphere appear to be deflected to the right, and to the left on the southern hemisphere

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9
Q

major winds

A
  1. westerlies
  2. trade winds
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10
Q

ekman transport

A

the net motion of water at a 90 degree angle to the prevailing wind direction

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11
Q

what causes coastal upwelling on the southern hemisphere and downwelling on the northern hemisphere?

A

southerly winds parallel to the coast (winds coming from the south)

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12
Q

what causes coastal upwelling on the northern hemisphere and downwelling on the southern hemisphere?

A

northerly winds parallel to the coast (winds coming from the north)

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13
Q

equatorial divergence

A

winds moving toward each other deflect the water away from each other (45 degrees)
- happens at the equator
- causes upwelling (ekman suction)

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14
Q

upwelling

A

bringing water from the deep to the surface while surface water is being moved away due to the wind

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15
Q

subtropical convergence

A

when winds are going in the opposite direction, the water moves toward each other (ekman pumping)
- westerlies and trade winds
- causes downwelling

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16
Q

downwelling

A

because water cannot pile on top of itself, it is forced to go downward, creating downwelling

17
Q

basics of subtropical gyres

A
  1. happens at the equator
  2. coastal winds go north with deflection and westerlies deflect water to the right
  3. all deflected water points to the same center, which creates a mound of water and high pressure
  4. because everything is deflected to the right, it creates a circle
  5. creates a pressure gradient force with high pressure on the inside and low pressure on the outside

clockwise on the north, counterclockwise on the south

18
Q

four components of subtropical gyres

A
  1. equatorial current driven by tradewinds
  2. western boundary current (hot) deflected
  3. west wind drift driven by westerlies
  4. eastern boundary current (cold) deflected
19
Q

5 major ocean gyres

A
  1. indian ocean gyre
  2. north pacific gyre
  3. south pacific gyre
  4. north atlantic gyre
  5. south atlantic gyre
20
Q

basics of deep currents (6 things)

A
  1. driven by bouyancy (density) forces
    - gravity is the driving force
  2. also known as thermohaline circulation
    thermo = heat, haline = salt
  3. both of these affect density
  4. flow is much slower than surface currents (1000 years for deep water to circulate)
  5. formation of deep water is due to evaporation and formation of sea ice
    - makes the water more dense and thus sinks to the bottom
21
Q

two places of deep water formation

A
  1. north atlantic deep water (NADW)
    - forms near greenland; evaporation and cooling causes surface water to sink and flow south
  2. anarctic bottom water (AABW)
    - densest deep water
    - cold, dense water from sea ice formation in the weddell sea sinks and mixes with NADW form AABW
22
Q

how can water masses be distinguished?

A

by their temperatures and salinities

23
Q

what are surface currents driven by?

A

winds

24
Q

what is deep ocean circulation driven by?

A

gravity