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The Year Without a Summer : ウィキペディア英語版 | Year Without a Summer
The year 1816 is known as the Year Without a Summer (also the Poverty Year, the Summer that Never Was, Year There Was No Summer, and Eighteen Hundred and Froze to Death), because of severe climate abnormalities that caused average global temperatures to decrease by 0.4–0.7 °C (0.7–1.3 °F). This resulted in major food shortages across the Northern Hemisphere. Evidence suggests the anomaly was predominantly a volcanic winter event caused by the massive 1815 eruption of Mount Tambora in the Dutch East Indies (Indonesia), the largest eruption in at least 1,300 years after the extreme weather events of 535-536. The Earth had already been in a centuries-long period of global cooling that started in the 14th century. Known today as the Little Ice Age, it had already caused considerable agricultural distress in Europe. The Little Ice Age's existing cooling was aggravated by the eruption of Tambora which occurred during its concluding decades. ==Description== The Year Without a Summer was an agricultural disaster. Historian John D. Post has called this "the last great subsistence crisis in the Western world".〔Evans, Robert (Blast from the Past ), ''Smithsonian Magazine''. July 2002, p. 2〕 The unusual climatic aberrations of 1816 had the greatest effect on most of New England, Atlantic Canada, and parts of western Europe. Typically, the late spring and summer of central and northern New England and southeastern Canada are relatively stable: temperatures (average of both day and night) average between about 68 and 77 °F (20 and 25 °C) and rarely fall below 41 °F (5 °C).
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