California’s Extreme Weather Is the Future of Climate Change

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It was January 1983 and raining in San Francisco.

The summer before, I’d moved here from Portland, Ore., a city known for its perpetual gray drizzles and, on the 60-odd days a year when the sun deigns to shine, dazzling displays of greenery. My girlfriend had spent a year convincing me that San Francisco had much more to offer me than Portland did for her.

Every few months, I’d scrape the bottom of my bank account to travel to San Francisco and taste its charms. Once, I even hitched a ride on a private plane. (Those were the days!) In a week’s visit, she’d take me to multiple women’s music concerts—events you’d wait a year for in Portland. We’d visit feminist and leftist bookstores, eat real Mexican food, and walk through Golden Gate Park in brilliant sunshine. The sky would be clear, the city would be sparkling, and she convinced me that San Francisco would indeed be paradise. Or at least drier than Portland.

So, I moved, but I wuz robbed! I knew it that first winter when, from December through March, the rain seemed to come down in rivers—atmospheric rivers, in fact—though none of us knew the term back then. That would be my initial encounter with, as a Mexican-American friend used to call it, “el pinche niño.” El Niño is the term meteorologists give to one-half of an oscillating cyclical weather phenomenon originating in the Pacific Ocean. El Niño usually brings drought to the southern parts of North America, as well as Central America, while deluging Northern California and the Pacific Northwest. La Niña is the other half of that cycle, its effects roughly flipping those of El Niño geographically. (As for the meaning of “pinche,” go ahead and Google it.)


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