Köppenklíma

The Köppen climate classification is a widely used system for classifying the world's climates. Developed by the Russian-born German climatologist Wladimir Köppen in the late 19th century, it has been modified and refined by others since its initial publication. The system is based on the relationship between climate and vegetation, and it categorizes climates into five main groups, denoted by capital letters.

The five main groups are: A (tropical), B (dry), C (temperate), D (continental), and E (polar). Each of these groups is further subdivided using additional letters to indicate specific characteristics such as rainfall patterns, temperature variations, and seasonal changes. For example, the 'A' group is subdivided into Af (tropical rainforest), Am (tropical monsoon), and Aw (tropical savanna), with the second letter denoting precipitation. Similarly, 'B' climates are divided into BW (arid or desert) and BS (semi-arid or steppe), with further distinctions for temperature.

Köppen's classification is valuable for understanding global climate patterns, agricultural suitability, and the distribution of plant and animal life. While it is a simplified model and doesn't account for all climatic nuances, its logical structure and clear criteria have made it a standard tool in geography, meteorology, and environmental science. The system's longevity and continued use demonstrate its effectiveness in providing a framework for analyzing and comparing diverse climatic conditions across the globe.