Secondary circulation

Secondary circulation refers to the smaller, additional patterns of air movement that occur within the larger, primary circulation systems in the atmosphere. While primary circulation is driven by large-scale factors such as temperature gradients, Earth's rotation (Coriolis effect), and the general circulation of the atmosphere, secondary circulation often arises from more localized phenomena. Examples of secondary circulation include: 1. **Sea Breezes and Land Breezes**: These occur due to differential heating between land and water bodies.