Coriolis Force – Factors Affecting Wind Movement
- Coriolis Force
- Earth’s Rotation
- Pressure Gradient Force
- Friction
- Convection
- Topography
- Seasons
- Mountains
- Oceans
- Ice Caps
- Human Activity
The Coriolis force is an apparent force that deflects objects moving in a straight line on a rotating object. It is caused by the difference in the speed of rotation between different parts of the object. The Coriolis force is strongest at the poles and weakest at the equator.
The Earth’s rotation causes the Coriolis force to deflect winds to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. This is why hurricanes and other large storms rotate in opposite directions in the two hemispheres.
The pressure gradient force is the force that causes air to move from areas of high pressure to areas of low pressure. The pressure gradient force is strongest when the pressure difference is large.
Friction is the force that opposes the motion of objects. Friction between the Earth’s surface and the air slows down the wind. Friction is strongest near the surface and decreases with height.
Convection is the transfer of heat by the movement of fluids. Convection currents in the AtmosphereAtmosphere can cause winds to blow.
Topography is the shape of the Earth’s surface. Mountains and other landforms can block the wind and cause it to change direction.
Seasons are caused by the Earth’s tilt relative to the sun. The tilt of the Earth causes the sun’s rays to hit different parts of the Earth more directly at different times of the year. This causes the temperature to vary throughout the year.
Mountains can affect the wind by blocking it and causing it to change direction. Mountains can also cause the wind to speed up or slow down.
Oceans can affect the wind by absorbing and releasing heat. The oceans can also cause the wind to speed up or slow down.
Ice caps can affect the wind by reflecting sunlight back into space. This can cause the temperature to drop and the wind to speed up.
Human activity can affect the wind by changing the Earth’s surface. For example, deforestation can cause the wind to speed up.
The Coriolis force, pressure gradient force, friction, convection, topography, seasons, mountains, oceans, ice caps, and human activity are all factors that affect wind movement. The strength of each factor can vary depending on the location and time of year.
Coriolis Force
The Coriolis force is an apparent force that deflects objects moving in a straight line on a rotating object. It is caused by the difference in the speed of rotation at different latitudes. The Earth’s rotation is faster at the equator than at the poles, so objects moving in a straight line on the Earth’s surface appear to curve to the right in the Northern Hemisphere and to the left in the Southern Hemisphere.
Earth’s Rotation
The Earth rotates on its axis once every 24 hours. This rotation causes the Earth’s surface to move from west to east. The speed of rotation is fastest at the equator and slowest at the poles.
Pressure Gradient Force
The pressure gradient force is a force that pushes air from areas of high pressure to areas of low pressure. The pressure gradient is the difference in pressure between two points divided by the distance between the points. The stronger the pressure gradient, the stronger the pressure gradient force.
Friction
Friction is a force that opposes the relative motion of two objects. Friction between the Earth’s surface and the air slows down the air and causes it to curve.
Convection
Convection is the movement of heat through a fluid. In the atmosphere, convection currents are caused by the difference in temperature between the Earth’s surface and the atmosphere. Warm air rises from the Earth’s surface and cool air sinks. This movement of air creates wind.
Topography
Topography is the shape of the Earth’s surface. Mountains, valleys, and other landforms can affect the way that wind blows. For example, mountains can block the flow of air, causing it to rise and create clouds and rain.
Seasons
The seasons are caused by the tilt of the Earth’s axis. The Earth’s axis is tilted at an angle of 23.5 degrees relative to its orbital plane. This tilt causes the Sun’s rays to hit the Earth’s surface at different angles throughout the year. In the Northern Hemisphere, the Sun’s rays hit the Earth more directly in the summer than in the winter. This causes the summer to be warmer than the winter.
Mountains
Mountains can affect the way that wind blows in several ways. First, mountains can block the flow of air, causing it to rise and create clouds and rain. Second, mountains can create their own wind systems, called orographic winds. Orographic winds blow up the side of a mountain and then down the other side. Third, mountains can cause the wind to change direction. For example, if the wind is blowing from the west, it will be deflected to the north when it reaches a mountain range that runs from north to south.
Oceans
The oceans can affect the way that wind blows in several ways. First, the oceans can store heat. This heat can be released into the atmosphere, causing the air to rise and create clouds and rain. Second, the oceans can create their own wind systems, called sea breezes and land breezes. Sea breezes blow from the ocean to the land during the day, while land breezes blow from the land to the ocean at night. Third, the oceans can cause the wind to change direction. For example, if the wind is blowing from the west, it will be deflected to the north when it reaches a coastline that runs from north to south.
Ice Caps
Ice caps can affect the way that wind blows in several ways. First, ice caps can reflect sunlight back into space, which cools the air. This can cause the wind to slow down. Second, ice caps can store heat. This heat can be released into the atmosphere, causing the air to rise and create clouds and rain. Third, ice caps can cause the wind to change direction. For example, if the wind is blowing from the west, it will be deflected to the north when it reaches an ice cap that runs from north to south.
Human Activity
Human activity can affect the way that wind blows in several ways. First, human activity can release greenhouse gases into the atmosphere, which trap heat and cause the Earth to warm. This warming can cause the wind to change direction and speed. Second, human activity can build structures, such as buildings and roads, which can block the flow of air and cause the wind to change direction. Third, human activity can clear forests, which can expose the ground and cause the wind to blow more strongly.
1. Which of the following is not a factor affecting wind movement?
(A) Coriolis force
(B) Earth’s rotation
(CC) Pressure gradient force
(D) Friction
(E) Convection
The Coriolis force is caused by the Earth’s:
(A) rotation
(B) revolution
(C) gravity
(D) Magnetic Field
(E) atmosphereThe Coriolis force is strongest at the:
(A) equator
(B) poles
(C) tropics
(D) mid-latitudes
(E) subtropicsThe Coriolis force causes winds to:
(A) blow parallel to the Earth’s surface
(B) blow perpendicular to the Earth’s surface
(C) blow clockwise in the Northern Hemisphere and counterclockwise in the Southern Hemisphere
(D) blow counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere
(E) blow in a straight lineThe pressure gradient force is caused by:
(A) the difference in air pressure between two locations
(B) the Coriolis force
(C) friction
(D) convection
(E) the Earth’s rotationThe pressure gradient force causes winds to:
(A) blow parallel to the Earth’s surface
(B) blow perpendicular to the Earth’s surface
(C) blow clockwise in the Northern Hemisphere and counterclockwise in the Southern Hemisphere
(D) blow counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere
(E) blow in a straight lineFriction is caused by:
(A) the difference in air pressure between two locations
(B) the Coriolis force
(C) the Earth’s rotation
(D) the interaction of air with the Earth’s surface
(E) convectionFriction causes winds to:
(A) blow parallel to the Earth’s surface
(B) blow perpendicular to the Earth’s surface
(C) blow clockwise in the Northern Hemisphere and counterclockwise in the Southern Hemisphere
(D) blow counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere
(E) blow in a straight lineConvection is caused by:
(A) the difference in air pressure between two locations
(B) the Coriolis force
(C) the Earth’s rotation
(D) the interaction of air with the Earth’s surface
(E) the heating of the Earth’s surfaceConvection causes winds to:
(A) blow parallel to the Earth’s surface
(B) blow perpendicular to the Earth’s surface
(C) blow clockwise in the Northern Hemisphere and counterclockwise in the Southern Hemisphere
(D) blow counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere
(E) blow in a straight lineTopography is the:
(A) shape of the Earth’s surface
(B) Earth’s rotation
(C) Coriolis force
(D) pressure gradient force
(E) frictionTopography can affect wind movement by:
(A) creating obstacles to airflow
(B) creating areas of high and low pressure
(C) causing friction
(D) all of the aboveSeasons are caused by:
(A) the Earth’s orbit around the Sun
(B) the Earth’s tilt
(C) the Coriolis force
(D) the Earth’s rotation
(E) the Earth’s atmosphereSeasons affect wind movement by:
(A) causing changes in air pressure
(B) causing changes in temperature
(C) causing changes in the amount of sunlight
(D) all of the aboveMountains can affect wind movement by:
(A) creating obstacles to airflow
(B) creating areas of high and low pressure
(C) causing friction
(D) all of the aboveOceans can affect wind movement by:
(A) creating areas of high and low pressure
(B) causing friction
(C) causing upwelling and downwelling
(D) all of the aboveIce caps can affect wind movement by:
(A) reflecting sunlight
(B) absorbing sunlight
(C) creating areas of high and low pressure
(D) all of the aboveHuman activity can affect wind movement by:
(A) deforestation
(B) urbanization
(C) agriculture
(D) all of the aboveDeforestation can affect wind movement by:
(A) reducing the amount of vegetation
(B) increasing the amount of sunlight