Tides and SLR Flashcards

(34 cards)

1
Q

most tides controlled by

A

lunar cycle

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2
Q

Perigree

A

low orbit (moon close to earth)

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3
Q

Apogee

A

high orbit (moon further from earth)

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4
Q

Earth influenced by gravitational pull from…

A

moon and sun

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5
Q

spring tide

A

when the sun, moon and earth are in alignment = biggest tide (occur twice per month) semidinurnal

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6
Q

Semidiurnal tides

A

two high tides and two low tides per 24 hours. (1 high and low every 12 hours) - common nz

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7
Q

mixed semidiurnal

A

dissconnected symmetry but still one high and low every 12 hours. (24 hours - diff highs and lows) inequality

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8
Q

diurnal

A

one high and low over lunar day (24 hours)

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9
Q

Can we alter tides (e.g. CC)?

A

Cannot control tides, cycle continues forever, no matter what we do on earth surface

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10
Q

Micro-tidal

A

0-2m

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11
Q

MESO tidal

A

`2-4m

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12
Q

macro-tidal

A

4-6m

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13
Q

mega-tidal

A

6+ m

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14
Q

coasts can be a mix of dominated processes

A

tide, co or wave dominated

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15
Q

why are tides important in coastal systems?

A

Determine:
- where on the shore wave energy works
- vert and horiz shore distance over which wave energy is spread
- zones where species live
- tidal currents are an ocean/coastal energy source

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16
Q

Are tides predictable?

A

yes (predict week in advance)

17
Q

transgressive conditions

A

onshore migration of coastal landforms and deposits SHORELINE RETREAT

18
Q

regressive conditions/progradation

A

coastal emergence and or progradation (land extending out to sea) SHORELINE ADVANCE

19
Q

sea level

A

intersection btw sea edge and land that can shift landward or seaward depending if sea rise or fall (assume no change in land height - wrong! Tectonics)

20
Q

mean sea level

A

(made up) statistical average of conditions over many years. Varies from place to place

21
Q

Relative sea level (RSL) change

A

regional por local changes in water level due to changes in sea level or land positioning

22
Q

absolute sea level (Eustatic SL) change

A

global scale change in ocean water. Independent of land

23
Q

5 causes of sea level change

A

ecstatic, isostatic, steric sea level change, tectonism, compaction

24
Q

eustatic sea level change

A

ocean volume changes esp with ice sheets

25
steric sea level change
thermal expansion of oceans (warm water molecules take up more space than cold ones
26
isostatic sea level change
Changes in land level due to rebound of land after melting of ice (buoyancy - as lifts sl drops)
27
tectonics
Changes in relative land level position may be as subsidence in inter-seismic (btw EQ) or uplift during co-seismic events (during EQ)
28
Compaction
relative changes in density of loose sediments (become dense due to compaction - ground subsides relative sL rise!)
29
sea level in the past
had high (warm period), and cold stands (cold period) but little variation mostly
30
sea level across the globe
Different across globe, SLR in one area DOES NOT EQUAL SLR in another
31
biggest driver of SLR
thermal expansion - takes time to heat deep ocean water, heat transferred through energy migration. Can’t see problem so don’t do anything to change it!
32
Inverted Barometer Effect
Describes sea level response to changes in atmospheric pressure (important contributor to storm surge) high pressure - water level drops locally, low pressure - water level rises locally.
33
Storm surge
abnormal rise in sea level above the normal tide levels
34
ground water impacts of SLR
under threat as SLR and extreme weather events become more frequent - hazard as seawater pushes ground water upwards - potential flooding.