Tsunami key terms Flashcards

1
Q

Tsunami genesis

A
  • Dome collapse = tsunami wave (aftershocks)
  • spacing of waves can be >100km (barley detected in deep ocean)
  • shallowing = reduction in speed and wave spacing
  • apparent rapid sea level rise rather than wave
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2
Q

ocean waves near shore

A

• As the wave approaches shallow water the shape of the motion becomes more
elliptical and the velocity slows down.
• To conserve energy the wave rises higher

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3
Q

tsunami wave height

A

height of wave at the shore

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4
Q

tsunami run-up height

A

maximum height that the wave reaches on land

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5
Q

tsunami locations

A
  • large subducation zones produce the most tsunamis

- pacific has the most (ring of fire)

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6
Q

Smaller tsunami wave effects:

A

• Even small events can generate locally high waves
• In a bay the waves can be focused and increase their
amplitude
• A landslide triggered by an earthquake in a fjord in Alaska in
1958 created waves with a run-up up to 518 m high
• The warning time can be dramatically short

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7
Q

Wave diffraction

A

waves that pass from a media where they move fast to a media where they move more slowly, are refracted and waves that move around obstacles are diffracted.
- this can highly influence the local damaged resulting from the waves

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8
Q

tsunami warning

A
• as soon as an earthquake of magnitude >6.5 is located in the sea the alarm start 
• Using computer simulations and
maps allows forecast the time of
arrival in different locations
• Buoy and tide gauges help to verify
the effective presence of a tsunami
• Initiation of emergency plans
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9
Q

Can warning improve?

A

• Improved sensor networks in hazards areas of the world (seismic, tide
gauge, ocean buoys) and coordinated distribution and processing of
data
• Better information content that can better assist emergency responders
to assess the scope of the disaster
• Coordination and integration with national, regional and local
emergency response agencies and civil authorities
• Education and training at national, regional and local levels of
government and the general population

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10
Q

Volcanic induced tsunami

A
  • Anak Krakatau, december, 2018
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11
Q

Storegga slides

A
  • largest mass movement event to have effected NW Europe in 50,000 years
  • 3 events between 8,000 and 5,000
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12
Q

Storegga slide preceding conditions

A
  • sea level lowering (onset glaciation)
  • glacial expansion (glaciers extend off shore and sediment flushed out to continental margin
  • glacial retreat (unstable, unconsolidated sediment
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13
Q

triggers of Storegga

A
  • sediment loading following glaciation
  • earthquakes
  • M7 inland, result of isostatic rebound following deglaciation
  • Gas hydrate melting
  • warm water influx after deglaciation affected areas close to head of slide = change in pressure = initiation of slide
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14
Q

Seiches

A
  • sloshing of closed water bodies during an earthquake
  • large earthquake have produced these observed over large areas
  • although seiches have produced waves with height of few feet, damage was minimal
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