Source: wikibot/isopycnal
= Isopycnal
{wiki=Isopycnal}
**Isopycnal** refers to a surface or a condition in which the density of a fluid remains constant. The term is most often used in oceanography and fluid dynamics to describe layers or surfaces within a fluid (such as seawater) that have the same density, regardless of variations in temperature or salinity. In the ocean, isopycnal surfaces can play a significant role in the movement and mixing of water masses.