Transpordikihi

Transpordikihi refers to a layer in the Earth's atmosphere, specifically a region where wind speeds increase significantly with altitude. This phenomenon is most commonly observed in the troposphere, the lowest layer of the atmosphere. The term originates from Estonian, combining "transpordi" (transport) and "kihi" (layer). It is not a formally defined meteorological term like the jet stream, but rather a descriptive phrase used to identify an area characterized by strong, directional winds.

These high-speed wind currents are often a result of pressure gradients and temperature differences within the atmosphere. While not as consistently powerful or geographically defined as the jet stream, transpordikihi can influence weather patterns, aircraft navigation, and the dispersal of pollutants. The existence and strength of such layers can vary greatly depending on location, season, and specific atmospheric conditions. Understanding these regions of accelerated airflow is important for meteorologists and aviation professionals.