lecture 15 Flashcards
what are the 3 stages of tsunami wave
- generation: seafloor motion pushes up column of water
- propagation: as seabed shallows, speed slows and height grows (500-800km/hr)
- indundation: energy dissapates as water spreads over large area
sources of tsunami generation
anything that dispalces the ocean water column
ex. volcanoes, landslides, meteorite impacts, earthquakes
what does geographical reach depend on
volume of water displaces
ex. megathrust earthquakes uplift over 1000s of kms which generates ocean wide tsunamis
landslides are <1km so can produce local or regional tsunamis
water waves
pulses of energy that move through water mass causing water molecules to rotate in place
- flattens orbits as enter shallow water which decreases wavelengthand concentrates wave energy, heights increase (SHOALING)
wind waves
created by friction at wind/ocean surface
- size, frequency and period determined by velocity, duration and consistency of wind with water
- water runup/retreat is confined to the beach
tsunami run up
arrive as the leading edge of elevated mass of water
- run up and over beach which floods inlands
- might not be tall but have large momentum and a mass of water and debris
tsunami propagation
long wavelength means waves can bend around islands and hit all shorelines by refracting and hit all sides of an island
tsunami inudation
when entering shallow water the wave slows down and amplitude increases, run up heights depend on nearshore bathymetry and shape of coastline
- waterdrawback occurs if trough arrives first
seiche
standing wave in enclosed or partially enclosed body of water that sloshs back and forth across bays, lakes or swimming pools
- common in great lakes
lake superior 2001
seiche that reached dangerous heights
lake michigan
experienced deadly seiches in 1929 that killed 10, 1938 killed 5 and 1954 killed 8
- april 2018 ahd a. small seiche
lake erie
prone to seiches due to shallow water depth and alignment with prevailing south-westerly winds
- buffalo at east end, toledo at west and cleveland in middle
japan earthquake–>
small seiche in norweigan fjord caused by 9.0 japan earthquake 80000km away