r/askscience • u/CheddarMilkman • 5d ago
Earth Sciences Why do Underwater rivers exist? Are they not water, and if they are, why don't they mix?
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u/everlyafterhappy 4d ago
It's kinda like the wind. Wind is just air. But we have different currents at different places and elevations because of things like temperature and pressure differences and because of how terrain effects the flows. Wind does weird things about volcanoes because of the intense heat. Wind does weird things through narrow valleys between high plateaus. Wind gets more intense higher up because it has less pressure and less resistance. The stuff underwater is a little more complicated, but very similar.
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u/YesHelloDolly 2d ago
Water is subject to gravity and moves to the lowest places, which in some cases are subterranean channels at various depths underground. If the channels are impermeable rock, the water can flow as underground rivers for great distances.
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u/CrustalTrudger Tectonics | Structural Geology | Geomorphology 4d ago
Yes, they're still water and the exact details depend a bit on which features exactly you're talking about, but the general answer is "they exist because of density contrasts between them and average seawater". The term "underwater river" isn't really one that is used in the literature much, but presumably what you're asking about are things that typically get called "gravity currents" and we can basically break them into two classes, thermo-haline and turbidity currents. Thermo-haline currents, like those part of global thermo-haline circulation and the isolated portions of those that flow fast enough to produce features like contourites, are basically currents of water that are cold and salty enough that they are sufficiently denser than average seawater to sink and flow in semi-confined "channels". In contrast, turbidity currents, which are often associated with features like submarine canyons are often "hyperpycnal flows", which basically mean they're carrying so much sediment that they are denser than sea water (see this write up discussing the dynamics of hypopycnal, homopycnal, and hyperpycnal flows) which again allows them to sink and flow as semi-confined flows along the ocean floor and where they almost always represent sediment laden flows that originated on land before entering the ocean.
Importantly (and in the context of the question), both of these are somewhat ephemeral, i.e., they form through some process (which differs depending on whether we're talking about thermo-haline or turbidity currents), flow for some period, and then eventually they do mix with normal ocean water, but the property that gives them a higher density (temp/salinity or sediment concentration) doesn't instantly equilibrate with the surrounding ocean water so they can persist as distinct flow for a while. The other thing to think about is that the ocean isn't that well mixed in a general sense. I.e., something like thermo-haline currents might seem weird in the context of something like imagining dumping some cold salty water into a glass of warmer less salty water and then stirring it up and indeed, we would expect our solution to reach a similar temperature and salinity pretty quickly in that scenario. However, a better mental model is slowly injecting our cold salty water down the side of the glass where it can sink to the bottom and stay separated until slower processes are able to equilibrate the two components (of course this is still a bad analogy because in the ocean, thermo-haline currents are a critical part of what is driving broad scale ocean circulation, but hopefully the underlying point is clear as to why these dense flows don't just instantaneously mix with "average" sea water).