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The Indian Monsoon Low causes notable impacts on the region's climate during the summer. It forms as a result of rising land temperatures in the Indian subcontinent, which leads to a decrease in air pressure and the pulling of moist winds toward the land. This low-pressure system results in the formation of cumulonimbus clouds and heavy rainfall, especially in July and August. It also leads to increased humidity and higher temperatures in some parts of the Middle East, with the risk of floods and droughts depending on its seasonal activity. Meteorologists continuously monitor the low-pressure system to track its path and intensity, aiming to issue early warnings and minimize its adverse effects on residents and the economy.
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