What is Adiabatic?
Thermodynamic changes occurring within a system without any exchange of heat with the surroundings. In the atmosphere, changes in temperature due to adiabatic expansion and contraction occur with the increase and decrease of atmospheric pressure. The ascent and descent of an air parcel in the atmosphere are examples of this.
Schedule a Demo Today
A new era is starting with fundamentally new forecasting with unprecedented precision!
Contact UsGlossary
A weather system refers to the movement of warm and cold air across the globe, usually in a recurring pattern. Systems can...
A weather front where two air masses meet but neither is strong enough to move the other, often resulting in prolonged periods...
A blizzard is a storm that lasts 3 hours or more, with persistent winds/frequent gusts of 35 mph or more along with significant...
Jet streams are strong, fast-flowing air currents in the upper levels of the atmosphere. They form when warm air masses meet...
A low-pressure area with converging winds, rotating counterclockwise in the Northern Hemisphere and clockwise in the Southern...
An instrument that continuously records atmospheric pressure over time. It uses a barometer to measure pressure and creates...
The decrease in temperature with height in an adiabatically rising air parcel (lapse rate). For dry air, this value is 1...
In a severe storm, with a swirling motion in its left rear quadrant, a vertically rotating column of air, often seen with...
Local winds that blow from slopes to peaks as a result of the heating of the top slopes without being affected by general...
A strong wind typically ranging from 34 to 40 knots (39 to 46 miles per hour) and often associated with rough seas and stormy...

