During summer the incidence of lightning increases around the world. Its beauty and power are the energetic release of storm clouds, and have forever been an ingredient for mythical tales and stories told by the campfire. In Scandinavian mythology, light-ning was described as the weapon of the god Thor, who was the foe of demons and hurled lightning at his enemies. However, the appeal of lightning vanishes the first time you feel the hair stand up on the back of your neck or sense the buzz of metal objects as the air around you becomes charged. These are nature’s warning signs.
LIGHTNING MORTALITY
While global reporting of non-fatal lightning strikes by victims is postulated to be ra-ther poor, it is estimated that the annual odds of being struck by are 1-in-700,000, with a lifetime risk of 1-in-3,000. The only natural disaster to take more lives each year is flooding. Despite an American review of data since 1900 that predicts lightning mortality and morbidity rates of 30 percent and 70 percent respectively, contemporary mortality and morbidity rates may actually be as low as 5 percent to 10 percent. While previous lightning fatality estimates approximated 24,000 deaths per year (2011), an updated extrapolation tool puts this estimate closer to 6,000 deaths per year, approx-imately 50 of which occur in the United States each year (1). It is believed that despite lightning being a significant cause of weather related mortality, the incidence is on a century-long downward trend. Theories to explain this include greater urbanization away from labor-intensive agriculture, and improved forecasting, education, and med-ical care. However, despite popular beliefs the contrary, lightning strikes are still rela-tively common; for perspective, you are about 264 times more likely to be struck by lightning than to win the lottery in the United States.
LIGHTNING INCIDENCE AND ANATOMY
There are approximately 25 million cloud to ground flashes per year in the United States, although surprisingly, these account for only about 25 percent of all lightning strikes in the world. Lightning is typically formed by rapid air movement that causes a charge imbalance in the atmosphere. The dissipation of this imbalance is what leads to lightning, which is not dissimilar to rubbing a balloon on your head or walking across a carpeted floor in your socks and then touching a metal object. That spark is lightning on a micro scale. The electrical discharge from a weather front is direct current (dif-ferent than alternating current that is used in your house), nearly 100 million volts, has a temperature as high as 50,000 degrees Celsius, and lasts only milliseconds. The chal-lenge around lightning safety, strike prevention, and forecasting is its unpredictability. If you like to adventure in the outdoors there are very few places to truly be safe. Fur-thermore, common approaches to lightning safety actually do very little to minimize your risk of sequela secondary to a direct strike or exposure via other avenues such as splash or ground current.
LIGHTNING CASE REVIEW, HANKO FINLAND
The following case review is of a lightning strike emergency in Hanko, Finland in July 2011, when a summer storm with accompanying lightening overtook a military en-campment. Eight military conscripts were injured, three of them critically, after light-ning struck a tree next to their encampment. This review is based on material pro-duced by the Finnish Safety Investigation Authority (SIA) and is publically available.
On the evening of July 1st, eight conscripts arrived at the Hanko Encampment (see be-low) to rest. The small group was involved in a march competition with a group of of-ficer students. The weather was warm and it was not raining when the conscripts ar-rived to setup camp. Earlier in the afternoon there had been a soaking rain leaving the ground saturated in the vicinity of the camp. Although the storm passed quickly a fire was held in the stove so that the conscripts could dry their clothing and gear.
Images 1 and 2: Incident location in the Gulf of Finland
(Source: Ministry of Justice/National Land Survey of Finland)
Early in the morning hours the precipitating thunder moved into the area as a new line of rain cells began moving across the Baltic Sea from Estonia towards the west coast of Finland. The front was most dramatic between 00:30 A.M. UTC and 02:30 A.M. UTC, and the lightning density was about 11 flashes/100 km2, which is considered abundant but not exceptional. The storm front included a strong, spasmodic wind and hard rain, which are not uncommon to a Finnish summer. At the time of the incident the Finnish Meteorological Institute’s lightning locator system evaluated two powerful flashes near the tent site (see below). The black symbols represent lightning strikes while the colored portions represent intensity of precipitation. Colors (blue-green-yellow-red) correspond to various degrees of rain (drizzle-weak-moderate-heavy rain).
Image 3: Lightning and weather radar view at 02:00 UTC
(Source: Finnish Meteorological Institute)
The initial lightning strike hit a pine tree, which was approximately 1.5 meters from the effected conscript tent. The track proceeded along the trunk towards the ground (Image 4) and then, about a meter from the surface, it jumped to the metal tent pole (Images 5 and 6). From the pole, the lightning proceeded into the tent, washing over the conscripts causing some typical injury patterns listed below. The seriousness of the situation was worsened by the damp conditions and wet soil underneath and inside the tent. The tent occupants were asleep at the time of the event and most had no recol-lection of the lightning strike.
Image 4: Pine tree with resulting 4 meter long crack from the lightning strike
(Source: SIA case report)
Images 5 and 6: Melt marks on the tent pole
(Source: SIA case report)
The medical officer in charge immediately made an emergency call and organized first aid procedures. Initial post strike triage was performed and one of the injured conscripts was found to be lifeless. CPR was initiated immediately. The first EMS unit arrived on scene at 02:22 A.M. UTC, 16 minutes after the initial call for help. A defib-rillator was transported to the scene but there was no possibility for electrical inter-vention secondary to asystole. There was a litany of other injuries, which included sei-zures, chest pain, superficial and partial thickness burns, confusion, numbness in the feet and hands, nerve palsy, and psychological symptoms. The remaining injured con-scripts were transported to a regional hospital by five EMS units. Of those transported, all survived, although some of their injuries were reported to plague them for months after the event.