A high-pressure weather system occurs when atmospheric pressure increases above ambient air pressure. In the Southeastern U.S. during summertime, a high-pressure system, called the Bermuda high, typically raises air pressure from 30.0 to 30.5 inches of mercury. Increased air pressure also increases ambient air temperature through a process meteorologists call compressional heating. Calculate the temperature change, in degrees F, from compressional heating on a 1.00 ft^3 air sample when a high-pressure system covers a landmass with an initial ambient air temperature of 85.0ºF.
