What is Adiabatic Gradient?
The decrease in temperature with height in an adiabatically rising air parcel (lapse rate). For dry air, this value is 1 °C per 100 m. For moist air, this value can drop to 0.4 °C.
Schedule a Demo Today
A new era is starting with fundamentally new forecasting with unprecedented precision!
Contact UsGlossary
The belt between 50-70 ° N and S latitudes in the Northern and Southern Hemispheres, adjacent to the Polar Region. Although...
A rapidly rotating column of air extending from a thunderstorm to the ground, capable of causing significant damage.
The term used for turbulence occurring in the absence of clouds or cloud-like elements in the visible area. It is often observed...
A weather front where two air masses meet but neither is strong enough to move the other, often resulting in prolonged periods...
A low-pressure area with converging winds, rotating counterclockwise in the Northern Hemisphere and clockwise in the Southern...
A weather front formed when a cold front overtakes a warm front, lifting the warm air off the ground and resulting in a mix...
The expected rate of temperature decrease in an adiabatically rising air parcel when there is no heat exchange with the environment....
The term used for semi-stationary high-pressure centers such as the Azores and North Pacific Highs, which occur in the narrow...
A middle cloud type within the B family in the international cloud classification. These clouds consist of water droplets...
Nimbostratus clouds are thick, dark, gray clouds associated with rainy and gloomy days that block the Sun. These clouds,...

