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
Coastal flooding occurs when water from the ocean, sea, or large lakes inundates land areas along the coast, usually due...
A mass of very cold, dry air that mostly originates over the Arctic Ocean.
The narrow region between 35-40 ° N and S latitudes in the Northern and Southern Hemispheres, lying between the tropical...
Occurs when centers of high pressure and/or low pressure set up over a region in such a way that they prevent other weather...
Indicates the amount of water the soil can absorb/retain through percolation. This capacity is around 7% in sandy soil and...
A weather front where two air masses meet but neither is strong enough to move the other, often resulting in prolonged periods...
A small, intense downdraft that produces damaging winds at the surface, typically lasting a few minutes and often associated...
The percentage of water vapor in the air relative to the maximum amount of water vapor the air can hold at a given temperature.
Thermodynamic changes occurring within a system without any exchange of heat with the surroundings. In the atmosphere, changes...
The expected rate of temperature decrease in an adiabatically rising air parcel when there is no heat exchange with the environment....

