What is Anabatic Wind?

Local winds that blow from slopes to peaks as a result of the heating of the top slopes without being affected by general pressure changes. Generally, the term is used for upward air currents, vertical movements in the formation of cumulus clouds, and valley breezes rather than anabatic winds. Anabatic winds are less common than katabatic winds, which occur through the opposite process.

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Glossary

The term used for semi-stationary high-pressure centers such as the Azores and North Pacific Highs, which occur in the narrow...

A continental air mass is a large body of air that forms over land, characterized by dry conditions due to the lack of moisture...

A small, intense downdraft that produces damaging winds at the surface, typically lasting a few minutes and often associated...

A rapidly rotating column of air extending from a thunderstorm to the ground, capable of causing significant damage.

The formation of ice crystals on surfaces when the temperature drops below freezing, typically overnight, causing potential...

A body that has the property of absorbing all electromagnetic radiation falling on it, and therefore is the theoretical body...

A bomb cyclone is a large mid-latitude storm that forms when a storm’s central pressure drops (i.e. “bombs out”), resulting...

The belt between 50-70 ° N and S latitudes in the Northern and Southern Hemispheres, adjacent to the Polar Region. Although...

A prefix used in cloud nomenclature to describe middle-altitude clouds that form between 6,500 and 20,000 feet, such as altostratus...

A fixed potential temperature line on adiabats, or the process of thermodynamic changes within a system without any exchange...

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