A patch of ocean in the North Atlantic is stubbornly cooling while much of the planet warms. This anomaly — dubbed the "cold blob" — has been linked to changes in ocean circulation, but a new study found changes in large-scale atmospheric patterns may play an equally important role, according to an international research team led by Penn State.
“People often think the atmosphere has a very short memory, but here we provide evidence that atmospheric circulation change is significant enough to induce some long-term impact on the climate system,” said corresponding author Laifang Li, assistant professor of meteorology and atmospheric science at Penn State.
Sea surface temperatures in the subpolar North Atlantic have decreased by about .7 degrees Fahrenheit over the last century, and a trend toward a more frequent positive phase of the North Atlantic Oscillation (NAO) may have contributed significantly, the scientists reported in the journal Climate Dynamics.
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