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As the temperature of surface water increases from 10 C to 30 C, how does the water density change?
high density
the Coriolis Effect
ocean basin
salinity and temperature
Decreases
Gulf Stream
Latitude
differences in density of ocean water
One characteristic of the Antartic bottom water that makes thermohaline circulation possible is
high density
the Coriolis Effect
ocean basin
salinity and temperature
Decreases
Gulf Stream
Latitude
differences in density of ocean water
Winds and ocean currents move in curved paths because of
high density
the Coriolis Effect
ocean basin
salinity and temperature
Decreases
Gulf Stream
Latitude
differences in density of ocean water
The warm surface current that flows along the east coast of the United States and transfers heat to England is called
high density
the Coriolis Effect
ocean basin
salinity and temperature
Decreases
Gulf Stream
Latitude
differences in density of ocean water
Ocean surface water temperature depends on the solar energy an area receives due to which of the following?
high density
the Coriolis Effect
ocean basin
salinity and temperature
Decreases
Gulf Stream
Latitude
differences in density of ocean water
Deep ocean currents are caused by
high density
the Coriolis Effect
ocean basin
salinity and temperature
Decreases
Gulf Stream
Latitude
differences in density of ocean water
Two factors that affect the density of ocean water are
high density
the Coriolis Effect
ocean basin
salinity and temperature
Decreases
Gulf Stream
Latitude
differences in density of ocean water
Cold ocean water sinks and moves along the
high density
the Coriolis Effect
ocean basin
salinity and temperature
Decreases
Gulf Stream
Latitude
differences in density of ocean water
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