What’s Behind Super Typhoon’s Rapid Intensification?

Typhoon Rammasun's eye over northern China
Typhoon Rammasun's eye was over the northern part of China's Hainan Island when this image was taken by the JMA MTSAT-2R satellite on July 18, 2014.
(Image credit: NOAA/MTSAT)

Typhoon Rammasun first tore across the Philippines earlier this week, dumping up to 13 inches of rain in some spots and causing the deaths of at least 40 people. It then emerged over the South China Sea and underwent a rapid re-intensification that boosted it to Super Typhoon status before it hit China’s Hainan Island, becoming the most intense typhoon to hit southern China since 1973, according to the World Meteorological Organization.

Warm ocean waters and a favorable atmospheric environment allowed Rammasun to quickly regroup after its foray over the Philippines left it weakened and somewhat disorganized. While such rapid intensification has been seen many times in tropical cyclones (the blanket term for typhoons and hurricanes), the dynamics of the process aren’t well understood, limiting forecasting abilities.

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Andrea Thompson
Live Science Contributor

Andrea Thompson is an associate editor at Scientific American, where she covers sustainability, energy and the environment. Prior to that, she was a senior writer covering climate science at Climate Central and a reporter and editor at Live Science, where she primarily covered Earth science and the environment. She holds a graduate degree in science health and environmental reporting from New York University, as well as a bachelor of science and and masters of science in atmospheric chemistry from the Georgia Institute of Technology.