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The "Ridiculously Resilient Ridge," sometimes shortened to "Triple R" or "RRR," is the nickname given to a persistent region of atmospheric high pressure that occurred over the far northeastern Pacific Ocean during 2013-2014. The "Ridiculously Resilient Ridge" nickname was coined in December 2013 by Daniel Swain on the California Weather Blog. This anomalous atmospheric feature disrupted the North Pacific storm track during the winters of 2012-2013, 2013-2014, and 2014-2015, resulting in extremely dry and warm conditions in California and along much of the West Coast, contributing to the 2012–15 North American drought. The Ridge comprises the western half of an atmospheric ridge-trough sequence associated with the highly amplified "North American dipole" pattern, which brought persistent anomalous cold and precipitation to the eastern half of North America during 2014 in addition to record-breaking warmth and drought conditions in California. The Ridiculously Resilient Ridge is characterized by a broad region of positive geopotential height anomalies on monthly to annual timescales. This persistent ridging acts to "block" the prevailing mid-latitude Westerlies, shifting the storm track northward and suppressing extratropical cyclone (winter storm) activity along the West Coast of the United States. Such a pattern is similar to—but of greater magnitude and longevity than—atmospheric configurations noted during previous California droughts. This ridge of high pressure has contributed to a blob of high water temperatures in the Pacific Ocean, which has in and of itself caused changes in weather patterns for North America. ==See also== *Block (meteorology) 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Ridiculously Resilient Ridge」の詳細全文を読む スポンサード リンク
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