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Published byGervais Hines Modified over 9 years ago
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RD Instruments Home of the ADCP Coastal & Inland Business Unit 1. Why Waves? 2. Waves Features 3. Waves Observed
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Why Waves? Critical Factor for Coastal Region Beaches … summer fun, winter destruction Coastal economy Safety Shipping & Boating: ocean routes, coastal lanes Coastal Destruction: storm surges, tsunamis Coastal and Offshore Engineering Shore Protection, Structures: design, survival Mechanism for restoring natural equilibrium Energy Source: Wave & Tidal Power
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Specific Examples Vessel Berthing Structure Design Sediment Transport Estuary Processes Air / Sea Interaction Oil Spill Response
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Vessel Berthing Direction #1 Direction #2 Biased Direction
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Structure Design To Build A Jetty Direction #1 Direction #2 Biased Direction
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Sediment Transport Direction #1 Direction #2 Biased Direction
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Background Wave characteristics Wave characteristics Periodic oscillation that propagates through space Transfers energy but not mass Engineering & Science Interest: Energy Variation Engineering & Science Interest: Energy Variation With frequency With direction (and frequency)
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Describing Waves Frequency (time variation) Frequency (time variation) sets Wavelength for wave type Direction (propagation through space) Direction (propagation through space) Height (2 x amplitude) Height (2 x amplitude) Energy (height 2 ) x wavelength Energy (height 2 ) x wavelength
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Wave Words Figures taken from Oceanography of the British Columbia Coast, Richard E. Thompson
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Background 1-d … wave propagates along line 1-d … wave propagates along line Single wave: sinusoidal variation, amplitude, period Wave group 2-d … wave propagates across plane: direction 2-d … wave propagates across plane: direction Two classes: long & short wavelength Two classes: long & short wavelength Relative to water depth Energy of short waves decays with depth
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Two Wave Types
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Wave Orbits
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Orbital Currents
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Background Two categories: sea and swell (co-exist) Two categories: sea and swell (co-exist) Sea High frequency, short waves Surface variation appears random (snapshot) Energy from local winds Swell Lower frequency, longer waves Surface appears corrugated (more coherent), movement of crests more apparent Energy from distant storms
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Waves Spectrum WIND SUN, MOON STORMS, TSUNAMIS Tides
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Storms & Swell Strength Strength Duration Duration Fetch Fetch
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Storms & Swell
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Waves at Beach
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Refraction at Headland
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Reflection, Standing Waves
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RD Instruments Home of the ADCP Coastal & Inland Business Unit Background Wave Group: More than one wave Wave Group: More than one wave Interfere (reinforce, attenuate) Amplitude of resulting wave shape can vary along line (e.g. sets of waves arriving at beach) Boundaries: reflections, standing wave Boundaries: reflections, standing wave Resonance: forcing at natural oscillation period of system leads to efficient transfer of energy Resonance: forcing at natural oscillation period of system leads to efficient transfer of energy
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