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moving energy wind driven boundaries between/within fluids of different densities |
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waves from: coastal landslides calving icebergs (when a chunk of icebergs fall off into the ocean |
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waves from: tsunami sea floor movement |
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waves from: gravitational attraction among moon, sun, and earth |
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when the water doesn't move |
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when the water is disturbed |
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H distance between crest and trough |
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L distance between crest and crest, or trough and trough |
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T time it takes for full wavelength to pass a fixed position |
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F number of waves passing a fixed location per unit of time F = 1/T |
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No, Its only the wave form (energy is moving) ex. wheat field |
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back and forth (longitudinal) up and down (transverse) around and around (orbital) |
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distance that wind can blow over without being interrupted |
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push and pull waves particles: move back and forth energy transmitted through solid, liquid, gas |
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particles: move up and down (90 degree angles) energy transmitted by vibration |
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particles: move in around and around combination of longitudinal and transverse energy transmitted along interface between two fluids of different density |
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equal to one half of the wavelength (at still water level) or L/2 |
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the rate at which the wave travels S= wavelength (L)/wave period (T) more correctly known as celerity (nothing is in motion so there is no real speed) |
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occur in water deeper than their wave base move at speeds controlled by wavelength water depth: > or = 1/2 L ex: all wind generated waters |
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exist in water shallower than 1/20 of their wavelength, move at speeds controlled by water depth long wave water depth: < or = 1/20 L deeper the water, the faster shallow water waves move ex: tsunamis, tides, wind-generated waves that move into shallow near shore areas |
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are in between shallow and deep waves have characteristics of both 1/20 L < or = t = of < 1/2 L |
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constructive interference |
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wave + wave leads to a dramatic increase in wave height |
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crest and trough (opposites) --> cancel energy flat sea |
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slow wave + fast wave --> unpredictable patterns hard to sail in |
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quantify the severity of wind driven surface waves scale 0-11 |
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categories of rogue waves |
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walls of water three sisters single giant storm wave |
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wave energy: max: wave height, wave length, and duration duration of winds at equilibrium conditions |
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uniform symmetrical waves that travel outward from storm area long crests transport energy long distances |
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RMS Q Eliz II: 1995, 29 meters, like white cliffs of dover US Naval Research Lab: 2004, 27.7 m high and 200 m long, Hurricane Ivan |
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