Atmospheric convection: Revision history

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24 May 2024

  • curprev 20:1020:10, 24 May 2024‎ Ai talk contribs‎ 8,329 bytes +8,329‎ Created page with "== Introduction == Atmospheric convection is a fundamental process in meteorology and climatology, involving the vertical movement of air within the Earth's atmosphere. This phenomenon plays a crucial role in weather patterns, cloud formation, and the distribution of heat and moisture across the planet. Convection occurs when warmer, less dense air rises, and cooler, denser air sinks, creating a continuous circulation pattern. This article delves into the intricate mech..."
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