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Thunderstorms occur nearly every afternoon in the Equatorial doldrums due to the intense solar heating of the Earth's surface, which leads to significant evaporation and rising warm, moist air. This warm air cools as it ascends, causing condensation and the formation of cumulus clouds that develop into thunderstorms. Additionally, the convergence of trade winds in this region enhances uplift, contributing to the frequency and intensity of these storms. The combination of high humidity and strong convection makes afternoon thunderstorms a regular phenomenon in the equatorial zone.

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1mo ago

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