Here's the boring scientific explanation.
In Walton County, the "geology" (not "geography") has been altered since the impacts of Opal and ongoing storms as Shelly said. Actually, the more accurate word would be more along the lines of coastal geomorphology since these are fairly recent changes. Typically, when a storm hits, all three parts of a beach are impacted, the beach, the dunes, and the offshore sand bars. What is most readily observed is the loss of beach width; reduction in dune size or height depending on the size of the storm; and less noticeable is the reduction in offshore sand bar height and scour holes leading to increased water depth offshore.
In times of recovery, the system recovers in the following order, first beach width recovers leading to wide beaches with very low elevation. Then as the beach builds in width, the sand on the back part of the beach begins to dry out and over time will be blown into the dunes. At the same time, more sand is slowly brought back in by the waves along the beach front so that more beach and dune recovery can occur. Unfortunately, the longest recovery time is for the offshore bar systems and the overall underwater system. That is because this is the area where less sand is actually moving around to fill in some of the places that have been scoured out due to storms.
So, this is why we see a number of rip channels where rip surrents can be established, they are low spots in the offshore bar system and scoured areas in the nearshore areas. I would also think another reason why you hear of more actual rescues is because of more people and better reporting.
I hope this helps.