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
A weather front where two air masses meet but neither is strong enough to move the other, often resulting in prolonged periods...
The heating of the Earth by the sun causes daily changes in both the direction and speed of the wind. During the day, ground...
CONQ is a meteorological abbreviation for significant convection observed in a specific area, often indicating unstable atmospheric...
The expected rate of temperature decrease in an adiabatically rising air parcel when there is no heat exchange with the environment....
Large, fluffy white clouds with flat bases, typically indicating fair weather, though they can develop into storm clouds...
The term used for semi-stationary high-pressure centers such as the Azores and North Pacific Highs, which occur in the narrow...
Ball lightning appears during thunderstorms, taking the shape of glowing, electric orbs in the sky. It can appear in a variety...
Bright and dark rays with changing colors and contrast in the sky. These rays become visible due to the reflection of atmospheric...
The trapping of heat in the Earth's atmosphere due to greenhouse gases, such as carbon dioxide and methane, which allows...
A cold core low is a low-pressure system where the coldest temperatures are found near the center. These systems are often...