Large storms with broad impacts get names from meteorologists. Still, one smaller-scale storm in Australia's Northern Territory also receives the same privilege because of its unique nature -- it shows up daily!
Meet Hector, the Convector Storm
Weather systems are typically reserved for massive, isolated events, like cyclones or winter storms across northeastern America, that have the potential to have a major influence over a wide area. However, there are a few outliers. Of those, one is based in Australia. Presenting Hector, a thunderstorm called "Hector the Convector." It earns a name due to its consistency.
Hector visits the Tiwi Islands, about 100 km north of Darwin, every day at 3 p.m. during the build-up season, which runs from September to December. Hector also appears during the wet season (January to April), but only when the monsoon is inactive.
The Australian Bureau of Meteorology (BoM) claims the islands are the ideal convection breeding habitat. The shapes of Bathurst and Melville are similar to that of a pyramid, and afternoon sea breezes combine above the 'pyramid's tip,' causing air masses to crash together with no escape but upward. This phenomenon is similar to what happens in southern Ontario when lake breeze fronts collide.
This "up," in Hector's case, can reach heights of up to 20 km when the convective storm cell towers above the islands and breaks through the tropopause.
The cell builds similarly each day, even if its form varies. Sometimes, it has two separate thunderheads; other days, it's simply one large cell).
Hector is said to have been named by World War II pilots flying between Darwin and Papua New Guinea because it was a common sight in the sky north of Darwin and could be used as a helpful navigational reference.
Hector's consistency can be attributed to various factors. A major factor is the geography of Melville Island and Bathurst Island, the two largest Tiwi Islands.
Heavy with moisture, these sea breezes are driven upward as they converge through the atmosphere, where they cool and condense to produce clouds. Darwin can see this convection because it can be so intense that clouds can rise 20 kilometers above sea level.
What Is a Thunderstorm?
A thunderstorm is a severe, brief meteorological disturbance nearly invariably accompanied by thunder, lightning, thick clouds, heavy rain or hail, and strong gusts of wind. They form when warm, humid air masses quickly ascend to cooler atmosphere areas in a massive updraft. There, the liquid from the updraft condenses to create precipitation and tall cumulonimbus clouds.
Next, columns of cooled air descend toward Earth, unleashing powerful downdrafts and horizontal winds upon contact with the surface. Concurrently, electrical charges build up on cloud particles (ice and water droplets). Lightning strikes when the electric charge builds up to a significant amount.
Lightning creates shock waves, audible as thunderclaps and rolls, swiftly and strongly heating the air it passes through. Sometimes, spinning air vortices that are concentrated and strong enough to create tornadoes accompany strong thunderstorms.
Nearly every part of the planet is known to have thunderstorms. Yet, they are uncommon in polar regions and at latitudes higher than 50° N and 50° S. The Florida peninsula, the Gulf Coast, and the New Mexico mountains are the places in the United States where thunderstorm activity is at its highest.
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