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The horizontal distance between two successive crests is called the
vertically
warm
the Coriolis effect
right
wave length
wind
formation of sea ice
wave height
Ocean currents that move toward the poles are
vertically
warm
the Coriolis effect
right
wave length
wind
formation of sea ice
wave height
The energy that drives surface ocean currents comes from
vertically
warm
the Coriolis effect
right
wave length
wind
formation of sea ice
wave height
What causes surface ocean current to be deflected
vertically
warm
the Coriolis effect
right
wave length
wind
formation of sea ice
wave height
Which process does NOT decrease the salinity of waater
vertically
warm
the Coriolis effect
right
wave length
wind
formation of sea ice
wave height
The vertical distance between trough and crest is called the
vertically
warm
the Coriolis effect
right
wave length
wind
formation of sea ice
wave height
Because of the Coriolis effect, ocean currents in the Northern Hemisphere are deflected to the
vertically
warm
the Coriolis effect
right
wave length
wind
formation of sea ice
wave height
Density currents move
vertically
warm
the Coriolis effect
right
wave length
wind
formation of sea ice
wave height
Check it!