Chapter 10 Flashcards
surface currents
masses of water that move from one place to another
how are surface currents formed?
by friction of wind passing over the ocean
gyres
a collection of currents that form a circular system
5 major gyres
North Atlantic South Atlantic North Pacific South Pacific Indian
Coriolis Effect
caused by the rotation of the planet
Coriolis Effect in N. Hemisphere
currents are deflected to the right (clockwise)
Coriolis Effect in S. Hemisphere
currents are deflected to the left (counterclockwise)
Effect of ocean currents on Earth as a whole
gains in solar energy equal the losses to space of heat radiated from the surface
Net gain of energy in _____ latitudes and net loss at ____ latitudes
lower, higher
The transfer of heat by winds and ocean currents equalizes:
latitude energy imbalances
Ocean currents account for __% of total heat transport, and winds account for __%
25, 75
the presence of cold currents causes temperatures to reach a ___ _____
dew point
upwelling
the rising of cold water from deeper layers to replace warmer surface water
coastal upwelling
most characteristic along west coasts of continents
coastal upwelling occurs when
winds blow toward the equator and parallel to the coast
Upwelling brings greater concentrations of:
dissolved nutrients to the ocean surface
deep-ocean circulation has a significant _______ component
vertical
deep ocean circulation AKA _____ circulation
thermohaline
An increase in seawater density can be caused by:
decrease in temperature OR increase in salinity
Density changes due to salinity are important in very ___ latitudes
high
Where does most water involved in deep-ocean currents begin?
high latitudes at the surface
Where surface waters are cold, salinity _____
increases
the coastal zone
the land/sea interface
waves are:
energy traveling along the ocean/air interface
most of the energy to make waves comes from
wind
wave period
the time it takes for one wavelength to pass by a location/fixed point
the height, wavelength, and period of a wave are affected by: (3)
1-wind speed
2-length of time the wind has blown
3-fetch
fetch
distance over which the wind blows
surf zone=
1/20 wavelength
The beach is
a river of sand
whitecaps
critical point reached where wave grow tall and topple over
the sea waves seen from shore are a mixture of
swells from faraway storms and wave created by local winds
circular orbital motion
as the wave travels, the water passes energy along by moving in a circle
surf
the turbulent water created by breaking waves
swash
turbulent sheet of water from collapsing breakers
backwash
water flows back down the beach toward the surf zone