The intense storm that hit Delhi has appeared in an unusual shape in the India Meteorological Department’s (IMD’s) weather radar imagery.
The storm was looked like a crescent or an archer’s bow.
In technical terms, such presentations of storms are called “bow echoes”.
The bow echoes because they are very often a precursor to the more destructive windstorms.
A bow echo can extend from 20 km to 100 km, and last between three and six hours.
The term was first coined in the 1970s by Ted Fujita, a Japanese American meteorologist known for developing the scale to classify tornadoes.
When rain-cooled air comes down to the ground and spreads out horizontally.
As this happens, a boundary called the gust front is created between the rain-cooled air and warm-moist air on the surface.
This front pushes up the warm-moist air into the atmosphere, which forms new thunderstorms.
These new thunderstorms produce more rain, thereby creating more rain-cooled air, which helps the gust front to maintain its strength.
As this process keeps repeating itself, there comes a point when there is an inflow of air on the trailing side of the line of storms and bends it like an archer’s bow.
The cycle lasts as long as new thunderstorms keep forming at the front, helping the system grow and move forward with strong winds.