According to , an atmospheric river is a relatively long, narrow region in the atmosphere that carries most of the water vapor moving outside the tropics, essentially a river in the sky. A typical one carries roughly as much water vapor as the average flow at the mouth of the Mississippi River. The strongest ones can carry up to 15 times that.
Most atmospheric rivers are weak and simply deliver the beneficial rain and mountain snow the region depends on. The strongest ones are a different story: when they stall over a watershed, they can drop extreme rainfall in a short window, which is when flooding, mudslides, and the kind of roofline damage this blog covers tend to show up all at once.