Winds and Waves
Exterior Effects
Currents and Tides
Risky Waters
Miscellaneous
200

The distance of the crest of one wave to the crest of the next wave.

Wavelength

200

One way that coastal engineers can reduce wave erosion is to build these.

Groins

200

Ocean movement primarily produced by gravity.

Tides

200

High tide on a coast is caused when that location passes through the deepest point of this.

Tidal Bulge (-777) and (+777)

200

The most direct method to measure sea level in a coastal harbor.

Tide Gauge

400

The vertical distance between a wave’s crest and trough.

Wave Height

400

A mass of rock that has been cut off from the mainland by erosion.

Stack

400

Ocean movement that most affects ocean navigation.

Currents

400

The main reason why the Bay of Fundy has such unusual tides.

Shape / Topography (+1999)

400

As a wave approaches shore, its speed and wavelength have this same reaction.

Decrease

600

This feature of a surface wave is the distance that wind blows over the water’s surface in one direction.

Fetch

600

Coastal stacks are usually remnants of these structures.

Sea Arches

600

Ocean currents driven by global winds.

Surface Currents

600

The location of an ocean gyre rotating counterclockwise.

Southern Hemisphere (-1700)

600

The change in a wave‘s height as it nears the shore.

Increase

800

The characteristic of a wave that most directly corresponds with its speed.

Wave Period

800

THE ABSOLUTE GAMBLER

(pick a number 1-2000)

+ (whatever they said)

800

Subsurface currents that flow due to differences in salinity or temperature are types these currents.

Density Currents

800

These have the most effect on surface currents, and therefore have the least effect on subsurface currents.

Prevailing Winds (-500)

800

The strongest force acting on our tides.

Moon
1000

The feature of water with the least amount of effects on a wave’s height.

Water Temperature

1000

THE ABSOLUTE GAMBLER

(pick a number 1-2000)

- ( whatever they picked )

1000

The Great Pacific Garbage Patch is the result of our own carelessness and a strong oceanic this.

Gyre

1000

A combination of the Coriolis effect, current speed, and water depth that change the direction of a current.

Ekman Spiral (+988)

1000

Compared to its surroundings, water with more oxygen but less nutrients likely went through this.

Downwelling

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