Does a cyclonic pressure system in the northern hemisphere have a high or low pressure?

In the northern hemisphere, cyclonic pressure systems are characterized by low-pressure areas. This occurs due to the rotation of the Earth and the Coriolis effect, which causes winds to flow toward the center of the low-pressure system. As air converges, it rises, leading to the formation of clouds and precipitation.

In contrast, high-pressure systems, which are anticyclonic, feature descending air that creates clearer skies and generally more stable weather conditions. The dynamics of these pressure systems are essential for understanding weather patterns, as low-pressure systems typically bring stormy weather, while high-pressure systems are associated with fair weather.

Variable pressure suggests conditions that fluctuate and do not align with the defined characteristics of either high or low pressure. Similarly, "none of the above" would not fit because the definition of a cyclonic system is well-established as being associated with low pressure. Therefore, acknowledging that cyclonic pressure systems in the northern hemisphere are indeed low-pressure systems is critical for grasping meteorological concepts.