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The National Oceanic and Atmospheric Administration (NOAA) defines a bomb cyclone — also known as a bombgenesis — as a cold air mass that collides with a warm air mass, like air over warm ocean waters. Another criteria is a rapid drop in atmospheric pressure. It must drop at least 24 millibars in 24 hours. A millibar is a unit of atmospheric pressure, and the atmosphere can typically be measured at 1,013 millibars.

THE GORGE — The Pacific Northwest and the Columbia River Gorge have experienced two significant weather episodes over the past week. Starting last Tuesday, a phenomenon known as a “bomb cyclone” made landfall along the northern Oregon Coast, bringing gale-force winds and heavy rainfall. Two days later, a long plume of moisture called an atmospheric river brought threats of flooding, landslides and snow in higher elevations to Northern California and southwest Oregon. Atmospheric rivers originate from the tropics and can stretch for thousands of miles.

Jon Liu, meteorologist at the National Weather Service (NWS) in Portland, said these two different weather phenomena are more common than people might think.