Advection
Advection, in atmospheric science, change in a property of a moving mass of air because the mass is transported by the wind to a region where the property has a different value (e.g., the change in temperature when a warm air mass moves into a cool region). Advection can refer to either the horizontal or vertical components of the motion.
This article was most recently revised and updated by John P. Rafferty.
Citation Information
Article Title:
Advection
Website Name:
Encyclopaedia Britannica
Publisher:
Encyclopaedia Britannica, Inc.
Date Published:
10 November 2026
Access Date:
November 13, 2026