A couple days ago I shared some research indicating that some of the heat absorbed due to the loss of Arctic sea ice is pooling mid-column under the arctic ocean. One of the questions that came up was – how can wind drive sub-surface currents? I think it helps if you can see all the currents as connected, so if the wind creates a surface current, the momentum of those vast amounts of water can help push it down when it reaches the fringes of the ice melt. This is the animation that runs in my head when I’m thinking about the oceans, so I figured I’d share it for those that might find it useful. Note: No sound or text in the video, description below the fold.
