Articles on Bomb cyclones
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A second low forming off the NSW coast may have given anxious residents a reprieve by pulling energy away from the huge storm lashing the coast.
A powerful storm hitting the West Coast combines these phenomena for a wet week of erratic weather, as a meteorologist explains.
The key ingredients for a storm to undergo bombogenesis are an unstable atmosphere, temperature differences and high-speed winds in the upper atmosphere.
What creates such dramatic storms across the US Great Plains? The key factors are topography and temperature differences.
What raises a common winter storm to the level of ‘bomb cyclone’? It’s all about rapid, sharp changes in atmospheric pressure – and the scientists who coined the term meant to highlight their power.
An atmospheric scientist who studies the Arctic explains why – because of global warming – the U.S. may be in for longer cold spells in the winter.
The US was hit by a ‘bomb cyclone’ last week, bringing icy cold and driving snow. These storms develop very rapidly, forming outside the tropics, typically on continental east coasts in winter.






