Hurricane Alexis wrote:Dorian and Chantal are signs of how the ridge favors FL and SE US landfalls. If it wasn't for the bad environment hurricanes like the 1928 Okeechobee hurricane and many others from that time period would be a possibility.
Ridging of the strength we have seen suppresses activity, it reduces instability, it brings in cooler waters (I remember this being an issue early 2004), and it's quite normal for this time of the year, albeit a bit stronger than normal this year.
1928 O. Hurricane, 1945 Miami Hurricane, 1960 Donna, 1992 Andrew, 2004 Frances, 2004 Jeanne.
All majors or near majors before they hit from the east. All depends on energy coming off the east coast at the time. I can't say for pre satilite days, but I am sure these systems were missed by shortwaves and caught with building ridging. Some of these storms could have not happened for Florida had a trough been just a bit stronger. A progressively changing environment is a more unstable environment, an environment more likely to have landfall in general. Years with static troughs or static ridges have been anti-climatic, and even those had periods of change. Strong troughs are diving off from the east coast this year, ridge strength will matter little when one of these catches a stronger system.
We will have to wait and see if a big pattern change happens. If not, I am curious to see what occurs.