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Physical Oceanography

Across
The vertical measurement from the trough to the crest of the wave.
The circular flow of currents in an ocean basin due to the Coriolis effect
Outermost layer of the atmosphere from 90000 meters above sea level
The lowest wave point above the average water level
Waves with wavelengths longer than 1.73 centimeters
An area where the waves have reached the maximum possible size for the wind speed, duration and fetch.
The time it takes for the same spot on two waves to pass a single point
The tendency for the path of an object moving in the northern hemisphere to deflect to the right, or to deflect left in the southern hemisphere
The horizontal distance between the identical point on two waves
The highest wave point above the average water level
The tendency of energy to shift within a wave upon reaching an obstacle, allowing a new wave pattern to form
A long line of waves that have the same frequency and wavelengths
Down
Waves with wavelengths of 1.73 centimeters or smaller , with surface tension being the primary restoring force that acts on them
The number of waves that pass a fixed point in one second
Layer of the atmosphere from 50000 to 90000 meters above sea level
Large circular loops that break away from currents; caused by friction from the flow of a current
A vertical circulation pattern in a gas or liquid caused by hot materiel rising and cold material sinking
The amount time that the wind blows in a particular spot
The area over which the wind blows
The layer of the atmosphere from 15000 to 50000 meters above sea level
Wave that exceeds the maximum theoretical size in a fully developed sea
Bending of waves
The layer of the atmosphere in contact with the surface of the Earth up to 15000 meters above sea level
A series of swells traveling together with the leading wave dissipating and the following waves forming