Question

Because cyclones are low pressure system, air flows _____________________ them.

Answer 1

Because cyclones are low-pressure systems, air flows towards them.

Step-by-step explanation:

In atmospheric science, cyclones are characterized by low atmospheric pressure at their center. Air naturally moves from areas of high pressure to areas of low pressure, creating a pressure gradient. In the case of cyclones, the low pressure at the center acts as a "vacuum," pulling surrounding air towards it.

As air flows towards a cyclone, it experiences a change in direction due to the Coriolis effect, which is caused by the rotation of the Earth. In the Northern Hemisphere, the air is deflected to the right, while in the Southern Hemisphere, it is deflected to the left. This deflection leads to the characteristic circular motion of air around a cyclone.

The inflowing air near the surface of a cyclone spirals counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere. This inward flow of air towards the low-pressure center of a cyclone is responsible for the formation of cloud bands, precipitation, and other weather phenomena associated with cyclonic systems.

In summary, because cyclones are low-pressure systems, air flows towards them. The low pressure at the center of a cyclone acts as a "vacuum" that pulls surrounding air towards it, resulting in the characteristic circular motion and weather patterns associated with cyclonic systems.

Answer 2

Because cyclones are low-pressure systems, air flows inward toward the center of the cyclone them.

Step-by-step explanation:

Cyclones, as low-pressure systems, exhibit a characteristic pattern of air movement. Air flows from areas of higher pressure to areas of lower pressure. In the case of cyclones, the pressure at the center is lower than the surrounding areas. This pressure difference causes air to move inward toward the center of the cyclone. This inward movement is often referred to as convergence, where air converges towards the low-pressure center.

As the air moves closer to the center, it spirals inwards due to the Coriolis effect, creating the distinct circular motion associated with cyclones. This inward flow of air contributes to the intensification and sustenance of the cyclone, as the warm, moist air fuels its energy and strength. Overall, the movement of air around cyclones follows a pattern of inward flow towards the central low-pressure region, setting the stage for the characteristic weather conditions associated with cyclonic systems.