What is the role of the Coriolis effect on ocean currents?(1 point)
Responses
The Coriolis effect turns currents counterclockwise in the Northern Hemisphere.
The Coriolis effect turns currents counterclockwise in the Northern Hemisphere.
The Coriolis effect turns wind to the right in the Southern Hemisphere.
The Coriolis effect turns wind to the right in the Southern Hemisphere.
The Coriolis effect turns wind to the right in the Northern Hemisphere.
The Coriolis effect turns wind to the right in the Northern Hemisphere.
The Coriolis effect turns currents clockwise in the Southern Hemisphere.
The Coriolis effect turns currents counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere.
The correct response is: The Coriolis effect turns currents counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere.
The correct answer is: The Coriolis effect turns currents counterclockwise in the Northern Hemisphere.
The Coriolis effect is a phenomenon that is caused by the rotation of the Earth. As the Earth rotates, any moving object, such as wind or ocean currents, appears to be deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. This deflection is known as the Coriolis effect.
In the case of ocean currents, the Coriolis effect influences their direction of flow. In the Northern Hemisphere, the Coriolis effect deflects currents to the right, causing them to rotate counterclockwise. This means that currents in the Northern Hemisphere generally flow in a clockwise direction around ocean basins.
On the other hand, in the Southern Hemisphere, the Coriolis effect deflects currents to the left, resulting in a clockwise rotation of currents. Therefore, ocean currents in the Southern Hemisphere tend to flow in a counterclockwise direction.
Understanding the Coriolis effect and its impact on ocean currents is important for studying and predicting ocean circulation patterns, as well as for various applications such as navigation and climate modeling.