Tsunami key terms Flashcards
Tsunami genesis
- 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
ocean waves near shore
• 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
tsunami wave height
height of wave at the shore
tsunami run-up height
maximum height that the wave reaches on land
tsunami locations
- large subducation zones produce the most tsunamis
- pacific has the most (ring of fire)
Smaller tsunami wave effects:
• 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
Wave diffraction
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
tsunami warning
• 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
Can warning improve?
• 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
Volcanic induced tsunami
- Anak Krakatau, december, 2018
Storegga slides
- largest mass movement event to have effected NW Europe in 50,000 years
- 3 events between 8,000 and 5,000
Storegga slide preceding conditions
- sea level lowering (onset glaciation)
- glacial expansion (glaciers extend off shore and sediment flushed out to continental margin
- glacial retreat (unstable, unconsolidated sediment
triggers of Storegga
- 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
Seiches
- 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