Super Typhoon Haiyan's Intensification and Unusually Warm Sub-Surface Waters

Wunderground.com by Dr. Jeff Masters Blog

Figure 1. Departure of temperature from average at a depth of 100 meters in the West Pacific Ocean during October 2013, compared to a 1986 – 2008 average. The track and intensity of Super Typhoon Haiyan are overlaid. Haiyan passed directly over large areas of sub-surface water that were 4 – 5°C above average in temperature, which likely contributed to the storm’s explosive deepening. Image credit: Japan Meteorological Agency.

A remarkable warming of the sub-surface Pacific waters east of the Philippines in recent decades, due to a shift in atmospheric circulation patterns and ocean currents that began in the early 1990s, could be responsible for the rapid intensification of Super Typhoon Haiyan. Hurricanes are heat engines, which means they take heat energy out of the ocean, and convert it to kinetic energy in the form of wind. It’s well-known that tropical cyclones need surface water temperatures of at least 26.5°C (80°F) to maintain themselves, and that the warmer the water, and the deeper the warm water is, the stronger the storm can get. Deep warm water is important, since as a tropical cyclone tracks over the ocean, it stirs up cooler water from the depths, potentially reducing the intensity of the storm. When both Hurricane Katrina and Hurricane Rita exploded into Category 5 hurricanes as they crossed over a warm eddy in the Gulf of Mexico with a lot of deep, warm water, the concept of the total heat energy available to fuel a hurricane–the Tropical Cyclone Heat Potential (TCHP)–became one that gained wide recognition. The Pacific Ocean east of the Philippines has the largest area of deep, warm water of anywhere on Earth, and these waters have historically fueled the highest incidence of Category 5 storms of anywhere on the planet. Super Typhoon Haiyan tracked over surface waters that were of near-average warmth, 29.5 – 30.5°C (85 – 87°F.) However, the waters at a depth of 100 meters (328 feet) beneath Haiyan during its rapid intensification phase were a huge 4 – 5°C (7 – 9°F) above average, judging by an analysis of October average ocean temperatures from the Japan Meteorological Agency (Figure 1.) As the typhoon stirred this unusually warm water to the surface, the storm was able to feed off the heat, allowing Haiyan to intensify into one of the strongest tropical cyclones ever observed.
 

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