In a strong El Niño winter, normally dry regions can suddenly drown in rain. NASA notes that "typically dry regions can experience nearly two times as much rain during a strong El Niño." Indeed, the blockbuster El Niños of 1982–83 and 1997–98 unleashed record-breaking California storms and unusually mild Northeast winters. These far-reaching effects—atmospheric "teleconnections" linking the tropics to North America—arise because Pacific warming steers the jet stream south and east.

In a strong El Niño winter, normally dry regions can suddenly drown in rain. NASA notes that “typically dry regions can experience nearly two times as much rain during a strong El Niño.” Indeed, the blockbuster El Niños of 1982–83 and 1997–98 unleashed record-breaking California storms and unusually mild Northeast winters. These far-reaching effects—atmospheric “teleconnections” linking the tropics to North America—arise because Pacific warming steers the jet stream south and east.

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