A strong southerly flow, ahead of a cold front, transported very moist air through Tennessee and Kentucky. Surface dew points were in the mid and upper 60s. Wave after wave in the mid and upper levels helped trigger widespread showers, with embedded thunderstorms. These training rains entered northeast Kentucky and southeast Ohio during the morning of May 2nd. However, the rain was slow to move east, not becoming steady until late afternoon for portions of western West Virginia. The heaviest rains fell during the evening hours to after midnight. However, light to moderate rain lingered until the predawn hours of Monday the 3rd.
The rain was not as heavy in West Virginia, when compared to counties to the west, in northeast Kentucky and southeast Ohio. The heaviest rain rates in West Virginia were on the order of .5 to 1 inch in less than 3 hours.
Rain totals of 2.25 to 3.0 inches were widespread along the Ohio River counties, with a few locations in Cabell and northwestern Mason County exceeding 3.5 inches. The 24 hours rain amount at the cooperative observer in Huntington was 3.63 inches. However, further east in Cabell County, rain amounts were less. Pea Ridge measured 2.2 inches of rain. The Tri State Airport in northern Wayne County had 3.1 inches.