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
Jet streams are strong, fast-flowing air currents in the upper levels of the atmosphere. They form when warm air masses meet...
A weather front where two air masses meet but neither is strong enough to move the other, often resulting in prolonged periods...
An image on the weather radar that is convex to the direction of movement and resembles an arc shape, caused by mesoscale...
Air laden with sand and dust, common in areas devoid of permanent vegetation, especially deserts.
Bright and dark rays with changing colors and contrast in the sky. These rays become visible due to the reflection of atmospheric...
The occurrence of storms resulting from the horizontal advection of cold air at high levels or the horizontal advection of...
A periodic warming of sea surface temperatures in the central and eastern Pacific Ocean, significantly influencing global...
Weather conditions are the components that comprise the state of the atmosphere. The six main weather conditions are temperature,...
Indicates the amount of water the soil can absorb/retain through percolation. This capacity is around 7% in sandy soil and...
The lowest level of a given cloud or cloud layer in the atmosphere, relative to the observer's position above the ground.