Updated March 13: A paper published today in the journal Nature Communications once again linked a warmer Arctic to snowier winters—this time specifically in the northeastern U.S.
The study comes on the heels of news that another nor’easter, the third in under two weeks, is headed toward New England.
It’s consistent with study findings that abnormally warm Arctic temperatures make severe winters in the Northeast two to four times more likely.
“Warm temperatures in the Arctic cause the jet stream to take these wild swings, and when it swings farther south, that causes cold air to reach farther south. These swings tend to hang around for awhile, so the weather we have in the eastern United States, whether it’s cold or warm, tends to stay with us longer,” said study co-author Jennifer Francis in a press release.
The research adds to theories that more extreme winters characterized by bomb cyclones and polar vortexes will be a more common climate change-induced pattern in the coming years.
When a U.S. Republican senator threw a snowball onto the Senate floor in late February of 2015, he used it to underscore his belief that human-made climate change was an alarmist conclusion. The snowball had been rolled from the Capitol grounds in Washington D.C., which, at the time, was experiencing an uncharacteristically cold winter.
If global warming was real, he posited, how could the nation’s capital experience such severe cold?
Uncharacteristically cold winters, however, just might be one of the most hard felt effects of climate change, according to a study published in Nature Geoscience by a team of researchers.
The study found that unusually cold temperatures in northern North America and lower precipitation in the south central U.S. all coincided with periods of warmer Arctic weather.
To reach this conclusion, the researchers analyzed how teleconnections in the Arctic cause cooler winters in North America. Teleconnections are largescale weather anomalies that influence weather across continents and span large portions of the atmosphere. The most commonly watched teleconnection weather patterns are El Ninos/as, but teleconnections are observed around the globe.
Anna Michalak, a researcher at the Carnegie Institution for Science, was involved in creating an ensemble of models used to support the study’s findings. She explained that the massive system of climate models, called MsTMIP, creates a large dataset that allows researchers to study the changes in the Earth terrestrial biosphere.
In order to reach their conclusions, the study’s authors looked at how the terrestrial biosphere (all the plants and soil on the Earth’s surface) contributed to or pulled carbon from the atmosphere. They found that over the past three decades, plants pulled less carbon from the Earth’s atmosphere during periods of warmer weather in the arctic.
“Even though we’re talking about the Arctic, it has immediate impacts on what we experience at lower latitudes,” said Michalak.
What Does It Mean?
Beyond a need for more scarves and gloves, colder winters could have serious implications for North American farms.
In an op-ed published in Nature alongside the study, noted climate scientist Ana Bastos wrote that the warming temperatures have the potential to weaken vegetation and shorten spring growing periods. The study looked at crop yields recorded by the National Agricultural Statistics Service of the U.S. Department of Agriculture and found crop production declined by an average of one to four percent during warmer Arctic years. Some states, however, saw a decline of almost 20 percent.
Bastos cautioned that the link between a warmer Arctic and harsher U.S. winters was more complex than a simple cause and effect mechanism. Weather patterns can be notoriously unpredictable, and other factors such as soil health and farming practices can impact crop growth.
The study suggests that as warmer Arctic years become more frequent, crop productivity could be increasingly hard hit. All of this could lessen the impact of carbon sinks, a term that refers to how much carbon a terrestrial biosphere is capable of pulling from the atmosphere. With fewer plants available to absorb more carbon, Arctic warming could accelerate, further weakening the carbon sink, suggested the study.
“Whether the relationship found implies a decreasing carbon sink capacity of North American ecosystems in the coming decades is unclear,” wrote Bastos. She cautioned a need to study how Arctic warming affects other regions in the Northern Hemisphere.
While the specific repercussions of warmer Arctic seasons and the severity at which those repercussions will be felt requires further research, the study effectively underscores the interconnectedness of Earth’s atmosphere.
Speaking about how human influence changes weather patterns, Michalak added, “Winters could be harsher; flooding is more intense; droughts are more frequent… By emitting greenhouse gasses, we’re not just warming temperatures, we’re perturbing the Earth’s entire system.”