kliimavööd
Kliimavööd is a term used in geography and meteorology to describe large-scale atmospheric circulation patterns that influence climate across different regions of the Earth. These zones are characterized by specific temperature ranges, precipitation patterns, and prevailing winds. They are primarily driven by the uneven heating of the Earth's surface by the sun and the planet's rotation, which leads to the formation of Hadley, Ferrel, and Polar cells.
The tropical zone, located around the equator, experiences consistently high temperatures and significant rainfall, often associated
The boundaries and characteristics of these kliimavööd are not static and can shift over time due to