Explanation:
Subtropical high-pressure belts are characterized by sinking air (subsidence), which leads to clear skies, dry conditions, and the formation of deserts (e.g., Sahara, Kalahari).
Explanation:
Convectional rainfall is most common in the equatorial regions. The intense heating of the ground causes moist air to rise rapidly, cool, condense, and form heavy afternoon thunderstorms.
Explanation:
Humidity does not directly affect wind speed. Wind speed is influenced by the pressure gradient (difference in pressure), the Coriolis effect (deflection), and friction (with the Earth's surface).
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