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Convectional currents in Pakistan typically occur during the hot summer months, particularly from May to August. During this period, intense solar heating causes the surface air to warm up, become less dense, and rise, leading to the formation of thermals. This process can result in localized thunderstorms and heavy rainfall, especially in regions like Punjab and Sindh. Additionally, these currents can influence weather patterns and contribute to the monsoon season's onset in the region.

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