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Okay, so convection of the hurricane is a little bit different than what you'd get with a thunderstorm. With a thunderstorm it's basically all up, right? It's warm air rising into cooler air, it condenses into a cloud, and then you have something called a lapse rate. The dry lapse rate is the conditional lapse rate in the atmosphere, and then the parcel cools at 6.5 degrees Celsius per vertical kilometer of ascent, right, until it hits the tropopause where the dry lapse rate changes and the atmosphere is no longer unstable. A hurricane is a little bit different. A hurricane uses something that's known as conditional instability of the second kind, CISK, and two things are involved, or four things really I should say. So you have massive airflow, so you have the low pressure at the center, the eye, and that draws in air from the surrounding area. The air spirals inward near the ocean surface, and as it does it picks up enormous amounts of heat and moisture, you know, water vapor from the warm ocean waters, and then you do have eye wall convection, so you have supersaturated air that converges and rises rapidly in a continuous ring, and that's right around the eye wall, so you get these towering thunderstorms that constitute the eye wall, and then the third factor is latent heat release. They call it latent heat because it's hidden, it's basically hidden heat energy, and latent heat release, so when water vapor in the eye wall condenses into rain, it releases a massive amount of this latent heat, and this is basically a thermal energy transfer that warms the air column in the core of the storm, so unlike other storms which, mid-latitude cyclones I should say, which actually cool in the center and with height, hurricanes actually, as you get closer to their center, things begin to warm up, and the air gets warmer, not necessarily warmer with height, but it gets warmer with height relative to what the atmospheric temperature normally is if there wasn't a hurricane. And then the other thing, let me drop it.