Experts: Global warming can strangely trigger less yearly snowfall, but more potent blizzards

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FILE - In this Saturday, Feb. 9, 2013 file photo, Mike Brown of Boston cross country skis past snow-covered cars through the Chinatown neighborhood of Boston. Scientists point to both scant recent snowfall in parts of the country and this month's whopper of a Northeast blizzard as potential signs of global warming. It may seem like a contradiction, but the explanation lies in atmospheric physics. (AP Photo/Charles Krupa)

WASHINGTON - With scant snowfall and barren ski slopes in parts of the Midwest and Northeast the past couple of years, some scientists have pointed to global warming as the culprit.

Then, when a whopper of a blizzard smacked the Northeast with more than 2 feet of snow in some places earlier this month, some of the same people again blamed global warming.

How can that be? It's been a joke among skeptics, pointing to what seems to be a brazen contradiction.

But the answer lies in atmospheric physics. A warmer atmosphere can hold, and dump, more moisture, snow experts say. And two soon-to-be-published studies demonstrate how there can be more giant blizzards yet less snow overall each year. Projections are that that's likely to continue with manmade global warming.

Consider:

— The United States has been walloped by twice as many of the most extreme snowstorms in the past 50 years than in the previous 60 years, according to an upcoming study on extreme weather by leading federal and university climate scientists. This also fits with a dramatic upward trend in extreme winter precipitation — both rain and snow — in the Northeastern U.S. charted by the National Climatic Data Center.

— Yet the Global Snow Lab at Rutgers University says spring snow cover in the Northern Hemisphere has shrunk on average by 1 million square miles in the past 45 years.

— And an upcoming study in the Journal of Climate says computer models predict annual global snowfall to shrink by more than a foot in the next 50 years. The study's author said most people live in parts of the United States that are likely to see annual snowfall drop between 30 per cent and 70 per cent by the end of the century.

"Shorter snow season, less snow overall, but the occasional knockout punch," Princeton University climate scientist Michael Oppenheimer said. "That's the new world we live in."

Ten climate scientists say the idea of less snow and more blizzards makes sense: A warmer world is likely to decrease the overall amount of snow falling each year and shrink the snow season. But when it is cold enough for a snowstorm to hit, the slightly warmer air is often carrying more moisture, producing potentially historic blizzards.

"Strong snowstorms thrive on the ragged edge of temperature — warm enough for the air to hold lots of moisture, meaning lots of precipitation, but just cold enough for it to fall as snow," said Mark Serreze, director of the National Snow and Ice Data Center. "Increasingly, it seems that we're on that ragged edge."

Just look at the last few years in the Northeast. Or take Chicago, which until late January had 335 days without more than an inch of snow. Both have been hit with historic storms in recent years.

Scientists won't blame a specific event or even a specific seasonal change on global warming without doing intricate and time-consuming studies. And they say they are just now getting a better picture of the complex intersection of manmade climate change and extreme snowfall.

But when Serreze, Oppenheimer and others look at the last few years of less snow overall, punctuated by big storms, they say this is what they are expecting in the future.

"It fits the pattern that we expect to unfold," Oppenheimer said.

The world is warming so precipitation that would normally fall as snow in the future will probably fall as rain once it gets above the freezing point, said Princeton researcher Sarah Kapnick.

Her study used new computer models to simulate the climate in 60 years to 100 years as carbon dioxide levels soar. She found large reductions in snowfall throughout much of the world, especially parts of Canada and the Andes Mountains. In the United States, her models predict about a 50 per cent or more drop in annual snowfall amounts along a giant swath of the nation from Maine to Texas and the Pacific Northwest and California's Sierra Nevada mountains.

This is especially important out West, where large snowcaps are natural reservoirs for a region's water supply, Kapnick said. And already in the Cascades of the Pacific Northwest and in much of California, the amount of snow still around on April 1 has been declining so that it's down about 20 per cent compared with 80 years ago, said Philip Mote, who heads a climate change institute at Oregon State University.

Kapnick says it is snowing about as much as ever in the heart of winter, such as February. But the snow season is getting much shorter, especially in spring and in the northernmost areas, said Rutgers' David Robinson, a co-author of the study on extreme weather that will be published in the Bulletin of the American Meteorological Society.

The Rutgers snow lab says this January saw the sixth-widest snow cover in the Northern Hemisphere; the United States had an above average snow cover for the last few months. But that's a misleading statistic, Robinson said, because even though more ground is covered by snow, it's covered by less snow.

And when those big storms finally hit, there is more than just added moisture in the air; there's extra moisture coming from the warm ocean, Robinson and Oppenheimer said. And the air is full of energy and is unstable, allowing storms to lift yet more moisture up to colder levels. That generates more intense rates of snowfall, Robinson said.

"If you can tap that moisture and you have that fortuitous collision of moist air and below-freezing temperatures, you can pop some big storms," Robinson said.

Pennsylvania State University climate scientist Michael Mann points to the recent Northeast storm that dumped more than 30 inches in some places. He said it was the result of a perfect set of conditions for such an event: arctic air colliding with unusually warm oceans that produced extra large amounts of moisture and big temperature contrasts, which drive storms. Those all meant more energy, more moisture and thus more snow, he said.