tides & currents Flashcards

1
Q

why does the moon and sun look the same size to us

A

Moon = small, Sun = further away

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2
Q

how does the moon move in a circular orbit around the earth

A

Earth has gravitational pull on moon, moon has gravitational pull on earth - but moon is trying to move in a straight line

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3
Q

how many days does it take for moon to go around the earth + earth to spin around sun

A

27 days for moon to go around the earth
365 days for earth to spin around sun

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4
Q

why isn’t the centre of gravity centered on the planet

A

The gravitational pull of the earth on the moon and moon on the earth mean its slightly off to one side towards where the moon is

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5
Q

what causes high tides

A

the fact the centre of gravity is slightly to one side where the moon is also affects the oceans – water gets sucked to the same side as the moon (gravitational bulge)

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6
Q

what’s the Gravitational force equation (F)

A

G m1 x m2
————–
r2
- m1, m2 = Mas of earth and moon
- r2 = distance between the two

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7
Q

explain why distance (r2) affects gravitational pull (F)

A
  • The further away you are from something that has a gravitational pull, the quicker the gravitational pull is going to drop off from it
  • Means there will be a strong gravitational pull on the right side of the planet (smaller distance) - water being pulled towards the moon
  • pull on the other side of the planet is smaller - water is dropping away from the moon
  • This is what gives us a bulge on either side of the planet
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8
Q

how do tides change

A

go up and down sinusoidally – they change more slowly at high or low water + change more rapid in the middle of the tide e.g. 3hrs after high water

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9
Q

how can we predict tides

A
  • earth rotates once every 24 hours, which should give a tidal cycle every 12 hours
  • BUT the moon orbits once every 27 days, which moves to tide forward ~1 hour a day - So the tide cycles approximately every 12 hours and 25 minutes
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10
Q

why does the moon have more than twice the influence the sun has on tides

A

its closer to earth

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11
Q

2 components of tidal force

A
  • the pull of the moon sucking the water
  • the earth sucking it back
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12
Q

what are spring tides and why does it happen

A
  • Tidal range is at its biggest – biggest high waters + lowest low waters
  • Happens because sun + moon are in line – pulling in the same direction
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13
Q

what are neap tides and why does it happen

A
  • Smallest change in tidal heights
  • 90 degrees – moon is in opposite direction to the sun - Sun is pulling to one side, moon pulling to the other
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14
Q

over how many days do we get 2 sets of both tide types

A

Over 27 days

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15
Q

what kind of tide does full moon an half moon tie in with

A

Full moon = spring tides
Half moon = neap tides

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16
Q

what would happen to tides If there was no land masses or seabeds

A

a tidal bulge with a frequency of 2 cycles per day would continue around the earth

17
Q

how does land affect tidal ranges

A
  • there is an interaction between land and the energy of the tidal bulge – waves reflect and refract as they hit land
  • This in combination with coriolis results in interference patterns – can both increase + ameliorate tidal range
18
Q

what are Amphidromic points

A

Where interference completely cancels tidal movement out - no tidal variation

19
Q

how can Coastal morphology affect tidal range

A

e.g. esturines, can affect tidal range by increasing or decreasing it - compresses energy and results in water pushing up

20
Q

what are Coriolis forces and what does it result in

A
  • to do with Earth’s rotation
  • When an object travels across latitudes, the inertia causes deflection to the trajectory
  • So…..because planet rotates west to east:
    In N. Hemisphere: object deflects to right
    In S. Hemisphere: object deflects to left
21
Q

what’s the Major driving force of SURFACE ocean circulation

A

wind

22
Q

what’s the Major driving force of ATMOSPHERIC circulation

A

solar energy

23
Q

why is Heat distribution uneven across Earth’s surface

A

Warm air rises (less dense); cold air sinks

24
Q

what does Hadley’s model of atmospheric circulation show

A
  • Planet is warm in the equator (tropics)
  • The hot air in these areas will rise (less dense) - to replace this air it is taken from the sides (from north to south)
  • But air movement is modified by Coriolis effect – means there are 3 cells in each hemisphere instead of one just going from north to south
25
Q

what effects the air movement

A
  • Coriolis effect
  • means there are 3 cells in each hemisphere instead of one just going from north to south
  • as air flows from high pressure zone to low pressure zone, its trajectory is modified by Earth’s rotation
26
Q

apart from wind, what are the ocean circulation patterns further modified by

A

 Coriolis effect
 Pressure gradient
 Presence of landmass

27
Q

what keeps surface water moving for a period of time even after the winds have stopped

A

Inertia - Surface ocean circulation thus responds more to average atmospheric circulation than to short term weather changes

28
Q

how is the ocean circulation patterns deflected by Coriolis effect

A

Because of small frictional coupling between air and water

29
Q

what is ekman motion

A

Interaction of wind + coriolis effect
- Deflects the movement of water to the right – net movement = 90degrees to the direction or the wind

30
Q

what is the product of Coriolis force combined with Ekman transport

A

large, cyclical currents in the north and south hemispheres (subtropicl gyres)
- Warm, nutrient poor water is piled up into the centre of these gyre systems - marine deserts

31
Q

what are the largest surface water currents on the planet

A

subtropical gyres in the north and south hemispheres

32
Q

what areas do Tropical organisms and cold loving organisms extend into

A
  • Tropical organisms e.g. corals extend into higher latitudes on the western side of the oceans
  • Cold loving organisms e.g. kelp extend into lower latitudes on the eastern side of the oceans
33
Q

what are Coastal upwellings

A
  • Southern hemisphere
  • Wind comes down the coast from north -> south – pushes the surface waters this way
  • Ekman transfer pushes this water 90degrees on average to the right of the wind direction (offshore)
  • The cold nutrient-rich water underneath rises up to replace the water that has moved – results in coastal upwellings