Okay, folks, let's settle down.
Storm surge. It's a pretty easy concept in principle - the winds from a storm push water in front of it. When the water gets to land, it piles up. Think of the ocean as snow in your driveway and the storm as you pushing a snow shovel.
There are, however, a number of factors that contribute to how high a surge is:
1. Wind speed - the faster the wind, the more water it can move
2. "Fetch" - an old nautical term adopted by meteorology, 'fetch' is the distance that the wind blows, unobstructed. It's why storms are so bad - and seas are so massive - in the Southern Ocean. At the latitudes between Cape Horn and Antarctica there is no land, so the wind just circles the globe, unobstructed.
3. Wave height - a storm pushes a mass of water in front of it, but there are also, as you might expect, waves on top of that water. You may recall from our encounter with Sandy, when we spoke of the surge height and the wave height as two different things
3. Shore topology - this is a really big factor. Waves can only get so high - an easy rule of thumb is 80% of the water's depth - before they break. So you can have HUGE waves in a major storm at sea but closer to shore those waves will break and so won't contribute that much to the surge height. Conversely, a shallow coast will cause a surge to build higher as the water basically runs out of basin depth approaching the shoreline. This is why we often see an inverse relationship between surge height and wave height in different locations based on shoreline topology.
With hurricanes we consider storm surge from the same perspective as wind speed. A hurricane's strongest winds are on the right-hand side of the storm, relative to its forward motion. Those winds push water in front of the storm, while the winds on the left side of the storm, blowing in the opposite direction, tend to push water away from it. Because the storm's relative motion is part of the wind speed math, we see bigger surge in the right quadrants than in the left quadrants because of the wind speed differential.
So the Bahamas, in this case, are in dire trouble because they will be on the right side of the storm at the end of a very long fetch. There will be a LOT of water piled up in front of Irma when she approaches the Bahamas so the surge will be very severe. On the other side of the storm, where the coast of Florida lies, there will be a long fetch from the right quadrants as the storm approaches but once it turns northward the Florida coastline will be on the left side and the surge effect will be somewhat mitigated. In fact, once the eye of Irma passes any given point on the Florida coast, the wind will begin to actually blow the ocean water out to sea, as opposed to onto the beach.
Ergo, I personally think that the 20 - 25 foot surge numbers being tossed around for southern Florida are overdone. Depending on when Irma begins her northward motion, my expectation for surge in the Miami area is more like 12 - 15 feet.