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  • Ethiopian Highlands Rainfall: Understanding Bimodal & Orographic Patterns
    The Ethiopian Highlands experience a diverse range of rainfall patterns, but the dominant type is bimodal rainfall.

    Here's a breakdown:

    * Bimodal Rainfall: This means there are two distinct rainy seasons:

    * The "Belg" season: Occurs from February to May, fueled by the retreating Northeast Monsoon.

    * The "Kiremt" season: Occurs from June to September, driven by the Southwest Monsoon.

    Other types of rainfall in the Ethiopian Highlands:

    * Orographic Rainfall: Due to the highlands' elevation, air is forced to rise, cool, and condense, resulting in significant rainfall on the windward slopes.

    * Convective Rainfall: Often occurs during the afternoon and evening, fueled by localized heating of the land surface.

    * Frontal Rainfall: Less common, but can occur during periods of cold fronts, especially during the transition between seasons.

    Important Note: The specific rainfall patterns and amounts vary significantly across the Ethiopian Highlands, depending on factors like altitude, location, and proximity to mountains.

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