The morphology of deep and long‐lived fades for line‐of‐sight, overwater propagation links in the mid‐Atlantic coast are examined. Such events, known as sustained deep fades (SDF), are analyzed employing weather maps, in situ measurements from radiosondes, an instrumented helicopter, and sensors on coastal platforms. These events occurred exclusively from November through July over the 3 years in which fade statistics were amassed; no SDF events were observed during the months August, September, or October. The SDF events biased the 3‐year fade statistics described in a companion paper. The results have demonstrated that synoptic weather conditions created by a sustained high‐pressure system over the subtropical Atlantic and occasionally by a sustained low‐pressure system whose center lies west of the coastal region result in a steady flow of warm, humid air at higher altitudes. When coupled with colder water conditions, such a flow results in a surface temperature inversion, an increase of water vapor pressure with altitude, and a positive lapse rate of the radio refractivity. This condition leads to severe subrefraction resulting in fades ranging from 20 to 60 dB for durations in excess of 2 hours and lasting as long as 2 days. Propagation modeling using a refractivity profile derived from sensors on board a helicopter during an SDF event predicted the same range of fades as were measured during that period.