Tropical monsoon climate is characterized by distinct wet and dry seasons, with heavy rainfall occurring during the monsoon months, typically associated with the southwest winds. This climate features high temperatures year-round, with average annual temperatures often exceeding 25°C (77°F). The dry season can lead to significant water shortages, while the wet season supports lush vegetation and agriculture. Additionally, this climate is commonly found in regions such as parts of South Asia, Southeast Asia, and West Africa.
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