Why is it called a Bomb Cyclone?
Due to its explosive or “bomb”-like properties, a bomb cyclone is thus named. It is characterized by a sharp decrease in air pressure, which can fall by at least 24 millibars or more daily. The storm’s explosive or “bomb-like” qualities are caused by this sudden reduction in pressure. A large-scale, rotating, low-pressure weather system with strong winds and copious amounts of precipitation is referred to as a “cyclone.” The low-pressure system of a bomb cyclone is rapidly intensifying, hence the name “bomb cyclone.” The term “bomb cyclone” was coined by meteorologists in the 1980s to describe the rapid intensification of a winter storm. It is now commonly used to refer to any winter storm that undergoes rapid intensification due to a rapid drop in atmospheric pressure.
Bomb Cyclone: Characteristics, Effects and Hot Spots
Due to their potential for wreaking havoc and generating significant disruption, bomb cyclones might be regarded as natural disasters. They are a specific kind of severe winter storm that can bring high winds, a lot of precipitation, very low temperatures, and hazardous weather conditions like blizzards, freezing rain, and ice storms. These weather conditions can cause various problems, including property damage, power outages, canceled travel plans, etc. Bomb cyclones are most common in the winter months in the mid-latitudes of the Northern Hemisphere, particularly in the northeastern United States and eastern Canada. However, they can occur in other parts of the world as well.