A climate zone is defined as a distinct area of the Earth characterized by specific climate conditions, including temperature, precipitation, and seasonal variations. These zones are often identified based on geographical factors such as latitude and elevation, as well as the influence of nearby landforms and bodies of water. The classification of climate zones is crucial for understanding the distribution of ecosystems and biodiversity, and helps determine which plants and animals can thrive in different regions[1][4][5].
The concept of climate zones can be traced back to the classification system developed by Wladimir Köppen in the early 1900s, which categorizes climates into five main groups: tropical, dry, temperate, continental, and polar[4][5][6]. Each of these major climate zones can be further subdivided based on specific characteristics, such as seasonal precipitation patterns and temperature ranges[1][3].
Understanding climate zones is essential for various applications, including agriculture, as it helps farmers know which crops are suitable for their local climate conditions[3][6]. Additionally, it is important for scientists monitoring climate change, as shifts in climate zones can indicate changes in global weather patterns[5][6].
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