Understanding Severe Thunderstorms

Each year, the atmosphere undergoes a significant change from Spring into Summer. As the days lengthen and temperatures warm, thunderstorms become a focal point of weather discussion in NYC – and the entire Northeast US. Meteorological Spring, which begins on May 1, typically marks the beginning of severe thunderstorm season in the NYC Metro Area.

Severe Thunderstorms are complex, dynamic and powerful. Very intricate atmospheric interactions occur prior to, during and after their formation. These can be confusing to interpret, even for meteorologists. Understanding the basics of how organized thunderstorms develop, and how meteorologists attempt to predict and quantify their potential impact, can go a long way in communicating their risks effectively.

Thunderstorm formation in the Northeast US

Despite being directly next to a body of water, organized thunderstorm development is quite common in and around the NYC Metro Area. Organized thunderstorm events occur when there is sufficient instability, atmospheric lift, and ample shear. This means storms can form via lift, act upon the unstable atmosphere, and remain organized due to the present wind shear.

The process by which organized thunderstorm events occur can be broken down even further. First, the sun needs to heat the surface to warm the air above it. When this warm surface air is forced to rise (a front, mountains, a sea breeze boundary, etc) it will continue to rise so long as it stays warmer than the air surrounding it. As a storm rises into freezing air, different types of ice particles can be created from freezing liquid drops. The ice particles can grow by condensing vapor (like frost) and by collecting smaller liquid drops that haven’t frozen yet (a state called “supercooled”). When two ice particles collide, they usually bounce off each other, but one particle can rip off a little bit of ice from the other one and grab some electric charge. Lots of these collisions build up big regions of electric charges to cause a bolt of lightning, which creates the sound waves we hear as thunder. (National Weather Service).