In east central Florida, a warm sector, a region of warm surface air between a cold front and a warm front, was positioned ahead of a progressing cold front. Large scale lift was supported by a very strong jet stream aloft, with strong vertical shear evident, conducive for rotating thunderstorms and tornadoes. Instability increased overnight with temperatures and dew points increasing through the pre-dawn hours. For example, northwest of Orlando, temperatures were still at , which was about 3 degrees warmer than the average high for the day and 14 degrees warmer than the average low. The conditions helped several thunderstorm cells to develop ahead of the cold front in a line, in the Gulf of Mexico. One of these thunderstorm cells matured into a supercell thunderstorm that remained intact, while other cells to its north failed to sustain themselves. The supercell had strong rotation visible on radar as it approached the western Florida Coast before it produced three tornadoes, two rated EF3 from Sumter County to the coastal waters of Volusia County during the early morning hours of February 2, 2007. After moving offshore, the main tornado-producing supercell quickly weakened and decayed into a bunch of showers, while another supercell produced an EF0 tornado four hours after the main supercell moved offshore.