Editing Internal wave (section)

==Internal waves in the ocean==
[[File:ISS034-E-032377annotated.jpg|thumb|right|400px|Internal Wave trains around Trinidad, as seen from space]]
Most people think of waves as a surface phenomenon, which acts between water (as in lakes or oceans) and the air. Where low density water overlies high density water in the [[ocean]], internal waves propagate along the boundary. They are especially common over the [[continental shelf]] regions of the world oceans and where [[brackish]] water overlies salt water at the outlet of large rivers. There is typically little surface expression of the waves, aside from slick bands that can form over the trough of the waves.

Internal waves are the source of a curious phenomenon called '''[[dead water]]''', first reported in 1893 by the Norwegian oceanographer [[Fridtjof Nansen]], in which a boat may experience strong resistance to forward motion in apparently calm conditions. This occurs when the ship is sailing on a layer of relatively fresh water whose depth is comparable to the ship's draft. This causes a wake of internal waves that dissipates a huge amount of energy.<ref name=Cushman-Roisin>{{harv|Cushman-Roisin|Beckers|2011|pages=7}}</ref>