|The I-79 Clendenin exit in Kanawha County, WV, on June 24, 2016.|
Credit: Facebook/West Virginia Department of Transportation
The flooding washed out many roads, caused landslides, destroyed numerous bridges, and left behind a thick layer of mud and debris in many communities. The death toll from this flood stands at 26, making it the third most deadliest flood in the state's history. In the days following the flood at least 32,000 homes and businesses were without power and more than 60 secondary roads in the state were closed.
The Elk River soared to a record crest of 33.37 feet on the morning of June 24, rising about 27 feet above the level it was on June 23.
Heavy rain occurs frequently during this time of the year in many parts of the country, but why was this particular event the disaster it was?
Geography plays a big part. The topography of West Virginia is mountainous, and the steep hills and long narrow valleys are conducive to flooding in very heavy rain events, particularly in the southeastern part of the state. In this particular situation, the heavy rain fell in a relatively short period of time (hours, not days) rushed down the hillsides and was funneled down the valleys. Rivers rose quickly and in some cases cut off escape routes.
The second major factor were training thunderstorms - thunderstorms that repeatedly move over the same area. There were actually two rounds of rain that moved across the state, but the second round that occurred beginning on the afternoon June 23 was the straw that broke the camel's back.
The surface weather map at 8:00 a.m. on June 23 showed a cold front extending from a low over Indiana through the Midwest, and a warm front extending east from the low through Ohio and Pennsylvania.
|8:00 a.m. EDT June 23, 2016|
By 8:00 p.m. on June 23 the front extended from Missouri east into southern Ohio. It stalled out there as a series of low pressure waves rippled along the boundary. These ripples along with warm, humid air south of the front was the ingredients needed for the heavy rain.
|8:00 p.m. EDT June 23, 2016|
As of 12:30 a.m. on June 23 there were only a few thunderstorms developing in western West Virginia, with most of the activity further north along the front.
However, during the pre-dawn hours thunderstorms rapidly developed and were producing some heavy rain. Showers and thunderstorms continued during the morning hours.
By late afternoon and evening thunderstorms were numerous and oriented west to east across central and southern West Virginia. There was only a slow southward advancement so the thunderstorms essentially trained across the same area.
By 10:30 p.m. EDT the line of storms finally pushed south, leaving widespread flash flooding in their wake.
|Counties outlined in green are under flood warnings.|
Nicholas and western Greenbrier Counties in West Virginia received the most rain, though heavy rain also occurred in western Virginia and flood warnings were issued for several counties there. Radar estimated up to 10 inches in Greenbrier County, with up to seven inches falling in only three hours.
|24-hour rainfall ending at 8:00 a.m. EDT on June 24|
|36-hour rainfall amounts end the morning of June 24, 2016|
|Credit: NWS Blacksburg, VA|
Fifteen of the fatalities occurred in Greenbrier County. Damage was extensive. The Greenbrier GolfClassic scheduled to start July 7 was canceled. The President declared central and southeast West Virginia major disaster areas.
Below are two links that contain slideshows of the flooding and damage in West Virginia and Virginia.
The Weather Channel
While the floodwaters have receded, residents affected by the flooding will be dealing with the aftermath for some time to come.