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It could also be playing a part in circulating cold and wet air to the central and eastern states of the US. The researchers said that it might not only be causing warmer temperatures on the West coast, but also cooler temperatures on the East coast. One thing that can be studied, though, is its effects.Īs air passes over warmer water and reaches the coast it brings more heat and less snow, which the scientists say helped cause current drought conditions in California, Oregon and Washington. Researchers said it may have contributed to the state of Washington's mild 2014 winter and might signal a warmer summer.īut exactly how this area of warmer water has formed, or how long it will stay, remains a mystery. ‘In the fall of 2013 and early 2014 we started to notice a big, almost circular mass of water that just didn't cool off as much as it usually did, so by spring of 2014 it was warmer than we had ever seen it for that time of year,’ said Dr Bond. Ten months later, the blob is now squashed up against the coast, and Dr Bond says all models point to it continuing through the end of this year.

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