During the winter, air passing over the Pacific patch brings more heat and less snow to the coast, which has contributed to the current drought conditions. Bond and his colleagues also say the warmer, less nutrient-rich water is disrupting the marine food web off the U.S. West Coast.

The other study was conducted by Dennis Hartmann, an atmospheric scientist at UW. He links the "polar vortex" chill that gripped the central and eastern U.S. in 2013-2014 to a decadal-scale weather pattern that sent warm, dry air to the West Coast and cold, wet air to the East. Hartmann says the same scenario apparently played out during the winter of 2014-2015.

The weather pattern, known as the North Pacific Mode, is what's causing the Pacific's warm blob as well.

Is global climate change playing a role in the rise of the North Pacific Mode? Neither Bond nor Hartmann is willing to say. "I don't think we know the answer," Hartmann said. "Maybe it will go away quickly and we won't talk about it anymore, but if it persists for a third year, then we'll know something really unusual is going on."

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— Alan Boyle

In addition to Bond, the authors of "Causes and Impacts of the 2014 Warm Anomaly in the NE Pacific" include Meghan Crinin, Howard Freeland and Nathan Mantua. Hartmann is the sole author of "Pacific Sea Surface Temperature and the Winter of 2014."