Regina Leader-Post

FIVE THINGS ABOUT FIRE IN AUSTRALIA

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Australia’s recent fire season was so extreme it altered large-scale wind patterns in the stratosphe­re more than 16 km overhead, which normally isn’t affected by events on Earth’s surface, a new study has found. Here’s some detail.

1 SOUNDS LIKE AN APOCALYPSE

This never-before-seen behaviour can be traced to violent, fire-induced thunderclo­uds that formed above active fire zones in southeaste­rn Australia. These “pyro-cumulonimb­us” events, or pyrocbs, injected enormous plumes of smoke into the lower stratosphe­re. One plume circumnavi­gated the globe while rising to an unpreceden­ted height of 30 km and spun up its own winds, which circled counterclo­ckwise around the plume at 50 kph for more than two months.

2 CLOUDY DAYS

Southeaste­rn Australia was in an extreme fire season in late December when strong winds caused fires to explosivel­y intensify and trigger an outbreak of pyro-cumulonimb­us clouds. At least 18 fire-induced thunderhea­ds formed between Dec. 29 and Jan. 4, pouring smoke into the stratosphe­re.

3 AEROSOLS UP HIGH

These plumes confirm a key prediction about how fires generated by nuclear bomb blasts would impact the atmosphere. Fire-induced thunderclo­uds act like chimneys, shooting plumes of smoke filled with aerosols into the stratosphe­re like a volcanic eruption. Once in the stratosphe­re, that smoke can travel around the world.

4 REMEMBER OZONE HOLES?

A plume effectivel­y creates a small ozone hole by lofting a pocket of ozone-depleted air into the stratosphe­re and preventing the two air masses mixing. Estimates suggest Australia’s pyrocb outbreak injected almost a million tons of aerosols into the stratosphe­re.

5 CONTINENT-SIZE CLOUD

Scientists tracked several distinct smoke plumes from Australia, including one almost 1,000 km wide and five km thick. It rose within the stratosphe­re over six weeks, climbing higher and faster than any pyrocb plume documented and peaking at an altitude of 32 km.

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