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Overview

   During the second half of March, precipitation across the region was generally minimal to nil which allowed the forest litter and dead trees/branches to become very dry. This helped set the stage for a high fire danger situation as low pressure developed over the Southern Plains during the early morning hours of March 30th, before lifting northeast and rapidly deepening during the daylight hours. In response to this deepening low, a sharp pressure gradient and strong southerly jet developed across eastern Kentucky during the morning hours of the 30th. This led to wind gusts of around 40 mph at many locations by early afternoon. In addition, a bubble of very warm and dry air over the Southeast US was pulled northward by the low-level jet and further dried by downsloping effects off of the Great Smoky and Cumberland mountains. As a result, relative humidity levels cratered to between 15 and 25 percent while air temperatures soared to near record high levels in the upper 70s to middle 80s. For some of the more sheltered valleys, this rapid warming and drying was manifested by a more than 50 degree diurnal temperature range from morning lows to late day highs. The starkest example of this was the Kentucky Mesonet station near Paintsville which started the day at 30F but recorded temperatures heating up to a summer-like 84F by late in the afternoon. The combination of strong winds, very warm temperatures, very dry fuels, and low relative humidities was very favorable for rapid fire spread and a number of wildfires ended up breaking out across eastern Kentucky. Fortunately, the impacts, in most cases, appear to have been limited to forest and brushy areas.

     After a brief lull in the gusts during the evening of the 30th, the most intense winds with this storm system roared across eastern Kentucky from midnight to 4 AM on the 31st along and just ahead of a line of decaying showers moving in from the west. While the showers themselves were rather weak, an intense 60-70 knot jet was howling just a few thousand feet off the ground and the shower activity aided in the mix down of the winds. Wind gusts peaked in the 40 to 60 mph range across much of the forecast area during this time frame. (Gusts were generally a bit weaker over the Big Sandy Valley and far eastern Kentucky.) Numerous power outages resulted, especially near/southwest of KY-15. However, some sizeable outages were also reported in Morgan and Floyd counties. Among the hardest hit was Owsley County, where over half the county lost power for a few hours overnight when the powerful winds blew a large tree down and damaged infrastructure near a substation. The winds also blew trees down onto power lines in multiple locations and snapped power poles, most notably in Bell, Knox, Clay, Owsley, Laurel, Rockcastle, and Whitley counties. Some structural damage was also reported, mostly to weakly constructed structures (e.g., carports). The winds however were strong enough to blow the roof off a church in Knox County and off of a home in Wolfe County. The rainfall with the shower line was relatively minimal and many of the wildland fires continued to burn at some locations during the daylight hours of the 31st, but the combination of cooling temperatures, lighter winds, and high humidity levels helped to combat the fire activity.

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Wildfire in Lee County

(Courtesy of Amanda Faught)

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