How Hilary Turned Into a Monster Storm
Like wringing out a great big sponge in the sky, starting this weekend tropical storm Hilary dumped an incomprehensible amount of water on Mexico, Southern California, Arizona, and Nevada, breaking “virtually all rainfall daily records,” according to the National Weather Service. Mount San Jacinto, near Palm Springs, got nearly a foot of rainfall over two days, while Mount Wilson, in Los Angeles County, got 8.56 inches. Even at some lower elevations, the rain has been relentless: 4.8 inches in Beverly Hills and 4.7 in Van Nuys.
Hilary’s deluge has caused widespread flooding and debris flows—roaring rivers of mud, boulders, and trees—destroying homes and businesses and overwhelming people in their cars. As of Monday morning, there was no way in or out of Palm Springs, a “very extreme situation at the moment,” said mayor Grace Garner.
Officials have only begun to calculate the damage. And while it’ll take some time for scientists to fully work out how much climate change contributed to Hilary’s destruction, such storms will likely get more and more ferocious as the world warms.
What made Hilary—which began life as a hurricane in the eastern Pacific—so gnarly? Simply put: Warm ocean water fuels hurricanes in the tropics. Warm, moist air at the surface of the sea rises, and the surrounding air rushes in to fill its place, creating winds. “The winds at the surface of the ocean pick up energy in the form of moisture and heat,” says climate scientist Karthik Balaguru, who studies hurricanes at the Pacific Northwest National Laboratory. “This air spiraling in towards the center of the storm, if it carries more moisture with it, once it rises, it is able to release more latent heat energy. This process invigorates the storm.”
Sea surface temperatures happen to be particularly hot right now in the eastern Pacific, due to the ongoing development of El Niño. This is a smear of warm water extending off the coast of South America westward into the Pacific. “Storms that form in the eastern Pacific during El Niño years are tapping into this additional heat from the ocean, and they tend to intensify more,” says Balaguru. “That is why almost all studies have shown that during El Niño years, the eastern Pacific tends to be very active in terms of hurricane activity.”
The eastern Pacific is the second most active basin in terms of number of storms per year, after the western Pacific, Balaguru says. But typically, hurricanes that form off the coast of Central America head west out to sea, not north like Hilary did. Easterly winds usually provide the “steering flow” to guide a hurricane away from land. “That is why we are not really that concerned about eastern Pacific hurricanes, normally, right along the West Coast of the US,” says Balaguru. “It’s not like the Atlantic hurricanes that form and move towards the US coast.”
Every two to three years on average, though, a hurricane forms in the eastern Pacific and “recurves” north toward Mexico. When it makes landfall, it loses that source of moist heat energy from the ocean, and dissipates. (Hilary was downgraded to tropical storm status by the time it made landfall in Baja California, and is now a post-tropical cyclone as it moves through Nevada.) The storm’s remnants might then travel into the southwest US, interacting with mountains and dropping their moisture as rain.
