Cline (hydrology)
From Wikipedia, the free encyclopedia
In hydrology and related sciences and technologies, a cline is a comparatively thin, typically horizontal layer within a fluid, in which a property of the fluid varies greatly over a relatively short vertical distance.
Such clines and, and the respectively varying properties include:
This article is issued from Wikipedia. The text is available under the Creative Commons Attribution/Share Alike; additional terms may apply for the media files.