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Movement of Ocean Water

Chapter 3

AB
salinitya measure of the amount of dissolved salts in a given amount of liquid
ocean currentsthe movement of ocean water that follows a regular pattern
surface currentsthe horizontal movement of ocean water that is caused by wind and that occurs near the ocean's surface
deep currenta streamlike movement of ocean water far below the surface
Coriolis effectthe apparent curving path of a moving object from an otherwise straight path due to the Earth's rotation
deep currenta streamlike movement of ocean water far below the surface
upwellingthe movement of deep, cold, and nutrient-rich water to the surface
El Ninoa change in the water temperature in the Pacific Ocean that produces a warm current
crestthe highest point of a wave
troughthe lowest point of a wave
wavelengththe distance between two adjacent wave crests or wave troughs
wave periodthe time between the passage of two wave crests or troughs at a fixed point
breakerswhere waves first begin to tumble downward or break
surfThe area between the breaker zone and the shore
tidesthe periodic rise and fall of the water level in the oceans and other large bodies of water
tidal rangethe difference in levels of ocean water at high tide and low tide
spring tidea tide of increased range that occurs two times a month, at new and full moon
neap tidetide of minimum range that occurs during the first and third quarters of the moon
La Ninaa change in the eastern Pacific Ocean in which the surface water temperature becomes unusually cool
longshore currentsa water current that travels near and parallel to the shoreline
storm surgea local rise is sea level near the shore that is caused by strong winds from a storm
tsunamisa giant ocean wave that forms after a volcanic eruption, submarine earthquake, or landslide


HS English
Clarinda High School
IA

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