After the lightning strike, there was no more thunder or lightning in the District. The sky cleared, and the storm was over.
But what caused the unexpected strike? Was it the last flash from a weak, departing thunderstorm, or was it positive lightning produced by a distant, powerful thunderstorm that traversed many miles across the sky to strike ground in Washington? I wanted to investigate.
Mapping the location of the lightning flash
To understand more about the unusual lightning flash, I contacted Scott Rudlosky and Mason Quick, lightning scientists at the National Oceanic and Atmospheric Administration, who can determine the size and location of D.C. area lightning flashes using data from the D.C. Lightning Mapping Array (DCLMA). I provided them with my lightning photo, the location where the photo was taken and its time stamp.
I learned that my photographed lightning was a compact flash of negative lightning produced by a rapidly dissipating storm over the District. It originated 3.7 miles above Earth and struck ground just south of the storm cell, making contact in East Potomac Park and twice near Pentagon City.
The lightning flash spanned the distance from the Mall to East Potomac Park and Pentagon City, approximately three miles in a straight line. It was a relatively small lightning flash by lightning standards.
For a size comparison, a few minutes after I photographed the lightning in Washington, a positive lightning strike from a thunderstorm near Richmond hit near Cambridge, Md., almost 200 miles away. That flash was more than 250 times larger than the photographed flash and covered approximately 1,500 square miles.
Lightning physics of a dying thunderstorm
I asked Rudlosky and Quick to explain the physics behind the rogue lightning flash. Quick explained in an email:
As far as the physics, we know the storm had undergone rapid collapse, likely compressing the distance between charge regions and enhancing the electric field enough to cause the lightning flash. The time difference between the first LMA source and the first ground contact indicates a propagation velocity of about 375,000 meters / second for the downward negative leader development. This is a typical negative leader velocity.
The flash was short, lasting only about a tenth of a second, but produced three ground contacts. All three cloud-to-ground return strokes were of negative polarity, and the cloud-to-ground flash that you photographed had a modest peak current of -17 kA. My guess is that the other two strikes were out of your field of view, to the right.
Rudlosky added, “This flash remained relatively close to the ground, which makes sense since the storm was decaying without much charge left aloft.”
Quick also stated, “It’s important to note the lightning flash occurred about 10 minutes after the apparent end of the thunderstorm, a time period when an eager soccer coach may say that it is safe to play again. Wait 30 minutes after the last lightning.”
During my thunderstorm photo shoots, I stay inside a vehicle or building and run my camera about 30 minutes after the storm ends with the hope of photographing distant anvil crawlers or bolts from the blue. I was still under the roof of the Lincoln Memorial when I took the lightning photo.
Hopefully, this story will reinforce good lightning safety. When thunder roars, go indoors and wait 30 to 45 minutes after hearing thunder to venture back outdoors. As we have seen, even a weak and dissipating thunderstorm can produce deadly lightning.