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.
Schedule a Demo Today
A new era is starting with fundamentally new forecasting with unprecedented precision!
Contact UsGlossary
The situation where there is no advection because the constant pressure surfaces and temperature surfaces in the atmosphere...
Condensation pressure deficit refers to the difference between the actual vapor pressure and the saturation vapor pressure...
The percentage of water vapor in the air relative to the maximum amount of water vapor the air can hold at a given temperature.
The scientific study of climate, focusing on the analysis of long-term weather patterns and trends over time.
A body that has the property of absorbing all electromagnetic radiation falling on it, and therefore is the theoretical body...
A low-pressure area with converging winds, rotating counterclockwise in the Northern Hemisphere and clockwise in the Southern...
The temperature at which air becomes saturated with moisture and water vapor begins to condense into liquid form, leading...
An image on the weather radar that is convex to the direction of movement and resembles an arc shape, caused by mesoscale...
The belt between 50-70 ° N and S latitudes in the Northern and Southern Hemispheres, adjacent to the Polar Region. Although...
In a severe storm, with a swirling motion in its left rear quadrant, a vertically rotating column of air, often seen with...