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June 2012 North American derecho

Weather event

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Through Thunderstorm and Tornado

Storm overview

Initial stage

The storm started as a small thunderstorm cell in central Iowa and continued into Illinois, developing into a mesoscale convective system (MCS) while mostly below severe limits at the time. Due to an extremely hot and highly unstable atmosphere with CAPE values in excess of 5,000 J/kg and temperatures on the south side of a stationary front well in excess of 100°F (37.8°C) prompting widespread excessive heat warnings, the storm complex strengthened and produced isolated instances of severe weather as it crossed over the Chicago metropolitan area late in the morning of June 29 for the Chicago area and much of northern Indiana by early afternoon. The first severe thunderstorm watch of the afternoon was issued at 11:50 a.m. CDT (1650 UTC) just before the storm crossed over Chicago.

Gaining of derecho characteristics

As the storm tracked eastward into Indiana, it became a derecho and wind gusts increased substantially, peaking as high as 91 mph (147 km/h) in Fort Wayne. By that time, the system had taken on a well-defined bow echo shape, the classic indicator of a derecho. A severe thunderstorm watch, with high wind probabilities (although not a PDS watch) was issued for the majority of Ohio, much of West Virginia, and parts of Indiana and Kentucky at 3:05 p.m. EDT (1905 UTC) as the storm traversed north-central Indiana. Moving southeastward to east-southeastward at about 60 mph (95 km/h)—a speed and trajectory that the derecho maintained for its entire lifespan—it followed the stationary front and increased in size as it entered Ohio in the mid-afternoon hours, affecting a large portion of the state. Since the derecho was clearly underway and expected to last a long time, the SPC increased the threat level to a moderate risk of severe weather at 3:37 p.m. EDT (1937 UTC) across Ohio, West Virginia and small portions of neighboring states, warning of the extreme wind threat. It crossed over the Columbus area at approximately 5:00 p.m. EDT, with winds reported to 82 mph (132 km/h) there, and caused severe damage to the power grid in Franklin, Delaware, and Licking Counties. Winds were reported in excess of 80 mph (128 km/h) at several other locations across the state as well. It maintained its intensity as it reached the Ohio River early in the evening, and the only reported (but unconfirmed) tornado associated with the system occurred in association with the derecho's bookend vortex, and did minimal damage in comparison near Newcomerstown, Ohio, at 6:20 p.m. EDT. As the derecho reached the Ohio-West Virginia border, the SPC issued another severe thunderstorm watch at 6:35 p.m. EDT (2235 UTC), also with high wind probabilities, for the remainder of West Virginia, much of Virginia and Maryland, parts of North Carolina, Kentucky, Pennsylvania, southern New Jersey and the District of Columbia. The derecho crossed the mountains of West Virginia, leaving destruction in its wake, as well as parts of southwestern Pennsylvania and eastern Kentucky through the early evening hours.

After sunset

Despite the mountainous terrain and loss of daytime heating, the hot, humid air mass and high instability allowed the storms to maintain their high intensity, even though the amount of convective energy decreased slightly (to a still-extreme 3,500 J/kg). They emerged into North Carolina, Virginia and Maryland later in the evening, where an even more unstable air mass awaited with CAPE values as high as 5,500 J/kg. As the derecho failed to weaken over the mountains, the moderate risk was expanded eastward by the SPC at 9:00 p.m. EDT (0100 UTC) into the mid-Atlantic region. At 10:10 p.m., the SPC issued the final severe thunderstorm watch for the derecho for all of Delaware, the remainder of Maryland, the remainder of eastern Virginia, southern New Jersey, the Chesapeake Bay, and the Mid-Atlantic coastal waters. The derecho continued to expand as it crossed the Mid-Atlantic states late in the evening, impacting nearly all of Maryland, Virginia, and Washington, D.C. The most severe winds—reported as high as 87 mph (140 km/h)—were focused in the Baltimore-Washington metropolitan area and southward towards Richmond. Widespread wind gusts over 70 mph (112 km/h), with some significantly higher, were reported across the large and heavily populated region.

Overnight at sea and dissipation

Damaging winds continued eastward across the Chesapeake Bay towards the Atlantic Ocean, losing little strength despite the cooler marine layer. The derecho emerged into the Atlantic Ocean shortly before 2:00 a.m. EDT (0600 UTC) on June 30, while still producing winds as high as 81 mph (130 km/h) at the coast in Tuckerton, New Jersey and strong and damaging winds on the Delmarva Peninsula. Numerous special marine warnings were issued for the coastal waters of affected states by the NWS as the derecho moved out to sea. The storm dissipated around 4:00 a.m. over the Atlantic south of Long Island, New York.

Second complex develops

As the derecho moved through Ohio, a second storm developed in Iowa and tracked into northern Illinois. The earlier derecho had used up most of the convective energy in the atmosphere, so this second storm did not become another derecho. Nonetheless, a small MCS with a bow echo developed and became severe as it moved along this track. Its formation prompted the SPC to issue another severe thunderstorm watch, the second of the day for much of the region, for the areas in its path including parts of Iowa and Illinois. However, the storm reached the cold pool left behind by the derecho, and dissipated in the cool, weakly unstable air. Along with its much shorter track, the second storm produced a maximum wind gust of 90 mph (145 km/h) in Marengo, Iowa. This second storm was responsible for the majority of the warnings issued and the damage that was done west of the Chicago area during the event.

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