Answer:
If a low pressure is in the Northern Hemisphere, divergence is likely to happen to the right of the actual center of low pressure.
Step-by-step explanation:
In the Northern Hemisphere, air flows counterclockwise around a low-pressure system due to the Coriolis effect, which is caused by the rotation of the Earth. As the air approaches the low-pressure center, it experiences a change in direction and begins to spiral inward. However, due to the Coriolis effect, the air is deflected to the right, causing a divergence or a spreading out of air away from the center towards the right side of the low-pressure system.
This divergence of air is often associated with the formation of clouds, precipitation, and other weather phenomena. It is important to note that the actual center of low pressure is where the air is rising most rapidly, while the divergence occurs on the periphery of the low-pressure system.
In summary, if a low pressure is in the Northern Hemisphere, divergence is likely to happen to the right of the actual center of low pressure. The counterclockwise flow of air around the low-pressure system, coupled with the Coriolis effect, leads to the spreading out of air away from the center towards the right side of the system.