Lecture 7: Coastal Oceanography Flashcards

1
Q

Global ocean bathymetry

A
  • 72% of globe is ocean
  • Much of the ocean bottom
    is flat
  • Coastal ocean (Continental
    shelf) is 10% of ocean area
  • Continental shelf (0 - 150 m
    depth) is land during ice
    ages
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2
Q

Are coastal regions more or less productive than the open ocean

A
  • Coastal regions are highly productive (3 to 5 times more productive than open
    ocean)
  • Coastal oceans support majority of the world’s fisheries (up to 90%)
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3
Q

Describe the anatomy of the coastal ocean.

A
  • Coastal ocean is a transition between
    terrestrial and abyssal environments
  • Coastal ocean is characterized by physical gradients (ocean bottom, hydrodynamics, water properties)
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4
Q

Describe features and consequences of coastal environments

A
  • Sandy vs. rocky nearshore:
    Sediment and breaking waves
  • Inlets, canyons, headlands:
    Coastline and bathymetric variation
  • Coral reefs:
    Shallow platforms, steep slope
  • Estuaries and Fjords:
    Freshwater input

Physical gradients means that processes are visible!

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5
Q

What is a wave?

A

“A wave is a signal or disturbance transferred from one part of a
medium to another with a recognizable speed of propagation.

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6
Q

What propagates away in a wave?

A

A wave mostly transfers energy through a
medium with minimal material transport.

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7
Q

Describe the following terminology for waves, Crest, trough, wave height, wave length, wave period, wave phase.

A
  • Crest: highest point on wave
  • Trough: lowest point on wave
  • Wave height H: vertical distance
    between crest and trough
    (Amplitude a: half of height)
  • Wavelength L: distance between
    adjacent wave crests or troughs
    Snapshot in time Time stack
  • Wave Period T:
    time between arrival of successive wave
    crests or troughs at a single location
  • Wave (phase) speed Cp= L/T
    This definition of Cp is valid for any kind of wave
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8
Q

What creates a wave in the ocean?

A

Disturbance:
sea surface is displaced by winds or pressure

Restoring Force:
gravity

Propagation:
pressure gradients due to different water heights

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9
Q

Review slide 14 on deep water vs shallow water waves

A

yeeeeeeeeeeeee

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10
Q

Compare deep water vs shallow water waves.

A

Deep vs. shallow water waves

  • In deep water ( h / L > 0.5 ), Cp varies with wavelength
  • Longer waves travel faster (dispersive)
  • In shallow water ( h / L < 0.05 ), Cp depends only on depth.
  • All waves travel at the same speed
    (non-dispersive)
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