Skip to: Content
Skip to: Site Navigation
Skip to: Search

Global warming not always to blame for extreme winters

Natural variations in weather can vary more than climate change signals, experts say.

(Page 2 of 2)

Even when global warming becomes apparent – from decades to a century away – "winter will still happen, with cold spells and severe weather," says Gerald Meehl, a research scientist at the National Center for Atmospheric Research in Boulder, Colo. "But the trend will be toward fewer cold spells and fewer severe weather events."

Skip to next paragraph

From North America's standpoint, many forecasters point to La Niña, El Niño's climatological sister, as the key driver behind this past winter's offerings. Under La Niña conditions, warm water pools in the western tropical Pacific while waters in the eastern Pacific grow colder.

Typically, for the US, La Niña boosts the chances of colder-than-usual temperatures for the Northwest and warmer-than-usual average temperatures for much of the rest of the country. Also, the southern tier of the US typically is drier than normal, with wetter-than-normal conditions in the Northwest and in the Ohio River Valley.

This winter, however, failed to follow that script. The usual areas expecting moisture got it. But so did the Southwest and Southeast, which received far more snow and rain than they usually do during a La Niña event. Across the country, temperatures varied far more widely than anticipated. Just over 1,200 locations reported reaching or beating record low temperatures, while just over 4,200 reported matching or beating record highs.

As a result, forecasters didn't do too well, Mr. Halpert says. Ordinarily, forecasts are most accurate when El Niño or La Niña's effects are strongest. This time, he estimates, the seasonal temperature forecast only topped a random forecast by 10 percent to 20 percent, while the precipitation outlook beat a random forecast by some 25 to 30 percent. Seasonal forecasts are deemed a success if they beat a randomly generated forecast by 50 to 70 percent.

The fly in the ointment: another tropical pattern that is a bit like El Niño on roller blades. It's called the Madden-Julian Oscillation. It starts as a large mass of rain clouds in the Indian Ocean. Then it moves east along the tropics – weakening over land and strengthening over water – until it returns to its starting point. It circles the globe once every 30 to 70 days, leading to its own wet-dry cycle.

This winter, the oscillation reinforced La Niña, Halpert says, leading to the unexpected variation in US temperatures as well as the beneficial precipitation in drought-stricken regions of the US. Indeed, he says, forecasters haven't seen this coincidence of a strong La Niña with strong Madden-Julian activity before.

At the moment, it defies forecasters, Dr. Meehl acknowledges. They can deal with it once it starts, but they don't know what triggers it in the first place. Knowing this would be very useful in making seasonal forecasts. In both the weather-forecasting and climate-modeling arenas, efforts to fix that problem represent a work in progress.