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Air moves in large, circular patterns called
differences in air pressure
local geographic features
Coriolis Effect.
differences in temperature and elevation
trade winds
westerlies
Warm air rises at the equator, and cold air sinks at the poles.
convection cells.
Mountain and valley breeses are caused by
differences in air pressure
local geographic features
Coriolis Effect.
differences in temperature and elevation
trade winds
westerlies
Warm air rises at the equator, and cold air sinks at the poles.
convection cells.
Global winds that blow from west to east are called
differences in air pressure
local geographic features
Coriolis Effect.
differences in temperature and elevation
trade winds
westerlies
Warm air rises at the equator, and cold air sinks at the poles.
convection cells.
What causes differences in air pressure around the Earth?
differences in air pressure
local geographic features
Coriolis Effect.
differences in temperature and elevation
trade winds
westerlies
Warm air rises at the equator, and cold air sinks at the poles.
convection cells.
What causes wind?
differences in air pressure
local geographic features
Coriolis Effect.
differences in temperature and elevation
trade winds
westerlies
Warm air rises at the equator, and cold air sinks at the poles.
convection cells.
In the Northern Hemisphere, winds traveling north appear to curve to the east because of the
differences in air pressure
local geographic features
Coriolis Effect.
differences in temperature and elevation
trade winds
westerlies
Warm air rises at the equator, and cold air sinks at the poles.
convection cells.
Global winds that blow northeast from 30 degrees north latitude and southeast from 30 degrees south latitude are called
differences in air pressure
local geographic features
Coriolis Effect.
differences in temperature and elevation
trade winds
westerlies
Warm air rises at the equator, and cold air sinks at the poles.
convection cells.
Local winds are produced by
differences in air pressure
local geographic features
Coriolis Effect.
differences in temperature and elevation
trade winds
westerlies
Warm air rises at the equator, and cold air sinks at the poles.
convection cells.
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