Correct option is A
Introduction
The
Equatorial Regions (around the equator, within the Intertropical Convergence Zone or ITCZ) are characterized by persistently high temperatures and high humidity. These conditions lead to intense solar heating, causing the air to rise rapidly, cool, and condense, resulting in heavy
convectional rainfall almost every afternoon. This type of rainfall is the most common in the hot, humid equatorial zone.
Information Booster
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Mechanism: Caused by the heating of the Earth's surface, which warms the air above it. The warm, light air rises (
convection), cools, and condenses to form rain clouds.
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Location: Most common in the
Equatorial Regions due to constant high solar insolation.
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Pattern: Typically occurs almost every day in the afternoon or early evening.
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Intensity: Often characterized by heavy downpours and thunderstorms.
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Other Types: It is also common in mid-latitude regions during the summer.
Additional Points
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Orographic: Caused by moist air being forced to rise over a mountain barrier; not the
most common type in the flat or low-lying equatorial regions.
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Cyclonic: Associated with the meeting of different air masses in temperate or mid-latitude cyclones; less common in the uniform heat and pressure environment of the equatorial zone.
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Both orographic and cyclonic: Incorrect as convectional is the dominant type, and cyclonic is less common.