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
Air laden with sand and dust, common in areas devoid of permanent vegetation, especially deserts.
A body that has the property of absorbing all electromagnetic radiation falling on it, and therefore is the theoretical body...
Convection is the vertical movement of air caused by temperature differences, where warm air rises and cool air sinks. It...
Confluence refers to the area where two or more air streams or bodies of water meet and combine. In meteorology, it often...
Snow that rises to 8 feet or higher.
Condensation is the process by which water vapor in the air cools and changes into liquid water. This process is crucial...
Coastal flooding occurs when water from the ocean, sea, or large lakes inundates land areas along the coast, usually due...
A thermodynamic change process in the system without any exchange of heat or transfer of energy between systems. This process...
The formation of fog when warm and moist air passes over a cool or cold surface or, conversely, when cold air passes over...
Jet streams are strong, fast-flowing air currents in the upper levels of the atmosphere. They form when warm air masses meet...