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首页> 外文期刊>Michigan Academician >The January Thaw in Southern Michigan and Wisconsin, 1950-1999
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The January Thaw in Southern Michigan and Wisconsin, 1950-1999

机译：1950-1999年在密歇根州南部和威斯康星州的一月解冻

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摘要

Is there a fabled "January Thaw" in the western Great Lakes? This paper examines daily temperatures at two stations of the same latitude but situated differently to the inland sea of Lake Michigan: East Lansing, Michigan, to the east, and Madison, Wisconsin to the west. A thaw is defined as three days with a mean temperature above 0℃. Results showed that for East Lansing, January thaws are numerous, sometimes multiples in a given year. February thaws are even more numerous. For Madison, there are January thaws, but fewer than in East Lansing. Like East Lansing, however, February thaws are more numerous than January thaws. Years have passed, however, with no thaws at either station. Parametric and non-parametric statistical tests are performed. There is no "revenge" for a January thaw, that is, a resurgence of very cold weather (-10℃). Finally, a large sample of daily mean temperatures at Madison exhibits a period in late January warmer than intuitively expected, but not dramatically so.
机译：西部五大湖中有传说中的“一月解冻”吗？本文研究了两个纬度相同但与密歇根湖的内陆位置不同的站点的日温度：东部的密歇根州东兰辛和西部的威斯康星州麦迪逊。解冻定义为平均温度高于0℃的三天。结果表明，对于东兰辛市，一月的融化次数很多，有时在一年中为数倍。 2月的解冻次数更多。对麦迪逊而言，一月有解冻，但少于东兰辛。但是，像东兰辛一样，2月的融雪比1月的融雪多。然而，多年过去了，两个站都没有解冻。执行参数和非参数统计测试。一月份的融化没有“复仇”，也就是非常寒冷的天气（-10℃）复燃。最后，麦迪逊的大量每日平均温度样本显示1月下旬的温度比直觉上预期的要高，但事实并非如此。

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