Which describes the Coriolis effect?
the direction of air currents in the Northern and Southern Hemispheres the direction of air currents in
the Northern and Southern Hemispheres the uneven heating patterns between the equator and the poles
the uneven heating patterns between the equator and the poles
the circulation pattern of air near the equator
the circulation pattern of air near the equator
the density of hot and cold air the density of hot and cold air
The Coriolis effect refers to the rotation of the Earth causing moving air and water to be deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere.
The Coriolis effect is best described as the circulation pattern of air near the equator.
The Coriolis effect describes the apparent deflection of the path of a moving object on the surface of the Earth due to the rotation of the Earth. It affects the movement of air, oceans, and other objects on the Earth's surface.
To understand the Coriolis effect, one needs to consider the following factors:
1. Earth's rotation: The Earth rotates on its axis from west to east, completing one rotation in approximately 24 hours.
2. Latitude: As you move away from the equator towards the poles, the rotational velocity of the Earth decreases.
The Coriolis effect is observed in the movement of air currents in the Northern and Southern Hemispheres. Due to the rotation of the Earth, moving objects, including air masses, are deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. This deflection is caused by the difference in rotational velocity between locations at different latitudes.
Therefore, the correct description of the Coriolis effect is "the direction of air currents in the Northern and Southern Hemispheres."