Perhaps the BEST B1G Forum anywhere, here at College Football Fan Site, CFB51!!!

It could if it turns. Sounds like it's gonna be more toward the Florida-Georgia Line.

From the NHC:

1. Southwestern Atlantic Ocean (AL92):
Updated:  Recent data from an Air Force Reserve reconnaissance 
aircraft and visible satellite imagery indicate that the area of 
low pressure located about 120 miles east of Jacksonville, Florida, 
has developed a well-defined center of circulation and is 
producing winds to near 35 mph, but the associated showers and 
thunderstorms are not quite organized enough for this system to be 
considered a tropical cyclone.  However, only a small increase in 
the organization of the showers and thunderstorms could result in 
the formation of a short-lived tropical depression before it 
reaches the coast of northeastern Florida or Georgia tonight, and 
interests there should monitor its progress.  For more information, 
refer to High Seas Forecasts issued by the National Weather Service, 
as well as local forecasts issued by your local National Weather 
Service Forecast Office.

117 today

So this thing gonna cross Florida or what?

Just a little rain. Storm is out of the forecast.

Finally made it to Cypress Street Pub. 

yup, many roads north of me are impassable

al this water will be passing by Sewer City in the next week via the Missouri river - sending it to Omaha and points south

don't worry about me fellas
I'm on high ground and don't need to drive through water on closed roads to get groceries, yet.

high ground = Loess hills

The Loess Hills are generally located between 1 and 15 miles east of the Missouri River channel. The Loess Hills rise 200 feet  above the flat plains forming a narrow band running north–south 200 miles  along the Missouri River. These hills are the first rise in land beyond the floodplain, forming something of a "front range" for Iowa, and parts of Missouri and Nebraska adjacent to the Missouri River. The Loess land formations of Iowa extend north into South Dakota and is a feature of three state Parks in South Eastern South Dakota. Union Grove State Park, Newton Hills State Park and Blood Run State Park.


During the last Ice Age, glaciers advanced into the middle of North America, grinding underlying rock into dust-like "glacial flour." As temperatures warmed, the glaciers retreated and vast amounts of meltwater and sediment flooded the Missouri River Valley. The sediment was deposited on the flood plain, creating huge mud flats. When meltwaters receded, these mud flats were exposed. As they dried, the fine-grained silt was picked up by strong prevailing westerly winds. Huge dust clouds were moved and redeposited over broad areas. The heavier, coarser silt was deposited close to the Missouri River flood plain, forming vast dune fields. The dune fields were eventually stabilized by grass. Due to the erosive nature of loess soil and its ability to stand in vertical columns when dry, the stabilized dunes were eroded into the corrugated, sharply dissected bluffs we see today.

The dominant features of this landscape are "peak and saddle" topography, "razor ridges" (narrow ridges, often less than 10 feet (3 m) wide, which fall off at near ninety-degree angles on either side for 60 feet or more, and "cat-step" terraces (caused by the constant slumping and vertical shearing of the loess soil). The soil has a characteristic yellow hue and is generally broken down into several units based on the period of deposition (Loveland, Pisgah, Peoria). Loess is known locally as "sugar clay" because it can be extremely hard when dry, but when wet, loses all cohesion. The Loess Hills of Iowa are remarkable for the depth of the drift layer, often more than 90 feet deep. The only comparable deposits of loess to such an extent are located in Shaanxi, China.