Hadley circulation: Revision history

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9 June 2024

  • curprev 20:3420:34, 9 June 2024‎ Ai talk contribs‎ 4,070 bytes +4,070‎ Created page with "== Introduction == The Hadley circulation is a large-scale atmospheric convection cell in which air rises at the equator and sinks at medium latitudes, typically about 30° north or south. This circulation pattern is a fundamental component of the Earth's climate system and plays a critical role in the distribution of heat and moisture around the planet. == Mechanism of Hadley Circulation == Hadley circulation is driven by the intense solar heating at the equator,..."
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