It’s Cold and My Car is Buried in Snow. Is Global Warming Really Happening?
For years, climate contrarians have pointed to snowfall and cold weather to question the scientific reality of human-induced climate change.
Such misinformation obscures the work scientists are doing to figure out just how climate change is affecting weather patterns year-round.
Understanding what scientists know about these effects can help us adapt. And, if we reduce the emissions that are driving climate change, we can dramatically reduce the pace of change and better prepare for the consequences in the future.
What is the relationship between weather and climate?
Weather is what’s happening outside the door right now; today a snowstorm or a thunderstorm is approaching. Climate, on the other hand, is the pattern of weather measured over decades.
NASA and NOAA plus research centers around the world track the global average temperature, and all conclude that Earth is warming. In fact, the past decade has been found to be the hottest since scientists started recording reliable data in the 1880s. These rising temperatures are caused primarily by an increase of heat-trapping emissions in the atmosphere created when we burn coal, oil, and gas to generate electricity, drive our cars, and fuel our businesses.
Hotter air around the globe causes more moisture to be held in the air than in prior seasons. When storms occur, this added moisture can fuel heavier precipitation in the form of more intense rain or snow.
At the same time, because less of a region’s precipitation is falling in light storms and more of it in heavy storms, the risks of drought and wildfire are also greater. Ironically, higher air temperatures tend to produce intense drought periods punctuated by heavy floods, often in the same region.
These kinds of disasters may become a normal pattern in our everyday weather as levels of heat-trapping gases in the atmosphere continue to rise.
The United States is already experiencing more intense rain and snowstorms. The amount of rain or snow falling in the heaviest one percent of storms has increased nationally over the last half century—with the largest increases in the Northeast, Great Plains, Midwest, and Southeast.
The 2014 U.S. National Climate Assessment shows some regions of the country have seen as much as a 71 percent increase in the amount of rain or snow falling in the heaviest storms between 1958 and 2012.
Overall, it’s warming, but we still have cold winter weather.
The seasons we experience are a result of the Earth’s tilted axis as it revolves around the sun. During the North American winter, our hemisphere is tilted away from the sun and its light hits us at a different angle, making temperatures lower.
While climate change won’t have any impact on Earth’s tilt, it is significantly shifting temperatures and causing spring weather to arrive earlier than it used to. Overall, spring weather arrives 10 days earlier than it used to, on average. “Spring creep" is something scientists projected would happen as the globe continues to warm.
The Arctic connection and the polar vortex: A look at recent North American winters
Winters have generally been warming faster than other seasons in the United States and recent research indicates that climate change is disrupting the Arctic and ice around the North Pole.
The Arctic summer sea ice extent broke all records during the end of the 2012 sea ice melt season. Some researchers are pointing to a complex interplay between Arctic sea ice decline, ocean patterns, upper winds, and the shifting shape of the jet stream that could lead to extreme weather in various portions of northern mid-latitudes — such that some places get tons of snow repeatedly and others are unseasonably warm.
In the Arctic, frigid air is typically trapped in a tight loop known as the polar vortex. This super-chilled air is not only cold, it also tends to have low barometric pressure compared to the air outside the vortex. The surrounding high-pressure zones push in on the vortex from all sides so the cold air is essentially "fenced in" above the Arctic, where it belongs.
As the Arctic region warms faster than most other places, however, the Arctic sea ice melts more rapidly and for longer periods each year, and is unable to replenish itself in the briefer, warmer winter season. This can destabilize the polar vortex and raises the barometric pressure within it.
For several winter seasons (2009/2010, 2010/2011, and 2012/2013), the polar vortex was notably unstable. In addition, another measurement of barometric pressure—the North Atlantic Oscillation (NAO)—was in negative mode, weakening part of the barometric pressure "fence" around the polar vortex. This instability allows the cold Artic air to break free and flow southward, where it collides with warmer, moisture-laden air. This collision can produce severe winter weather in some regions and leave milder conditions in other parts of the northern hemisphere.
During the 2011/2012 winter, there was a shift in the position of the jet stream, which separates cold arctic air from warmer air. Typically New England, the Great Lakes, and parts of the Great Plains sit north of the jet stream and remain cold in the winter season. However, the 2011/2012 winter jet stream position meant these regions were south of it for most of the winter, which helped produce the fourth warmest U.S. winter on record.
The lack of snowfall and snowpack for the winter of 2011/2012 and the following spring was a precursor to the large drought episode that impacted two-thirds of the nation during the following summer and autumn.
During the winter of 2013/2014, an opposite shift of the jet stream left parts of the U.S. with freezing weather and parts of Russia experiencing much warmer weather than usual.
The northern hemisphere winter weather is a complex interplay between the upper atmosphere circulation over North America and the ocean conditions in the East and North Pacific, with other factors playing a minor role. However, scientists are looking into the connection between changes in Arctic sea ice cover and more frequent extreme weather events across the mid-latitudes. Because of sparse data and short data records, it will take time to advance the understanding of these phenomena but clear trends are emerging.
The rapid warming of the Arctic, known as Arctic amplification, has contributed to a dramatic decline in Arctic sea ice extent in the summer and sea ice volume in the winter. In recent years, changes in storm tracks, the jet stream pattern, and in large energy waves known as planetary waves may have influenced where winter sets in hardest in the Northern Hemisphere – though it’s not clear how much impact this trend will have in the future, especially as the Arctic ice continues to lose mass.
It’s not too late.
The choices we make today can help determine what our climate will be like in the future. Putting a limit on heat-trapping emissions, encouraging the use of healthier, cleaner energy technologies, and increasing our energy efficiency are all ways to help us to avert the worst potential consequences of global warming, no matter what the season.