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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Long-term climate change and surface versus underground temperature measurements in Paris
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Long-term climate change and surface versus underground temperature measurements in Paris

机译:巴黎的长期气候变化以及地表温度与地下温度的测量

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Careful temperature measurements performed from 1783 to 1852 in underground galleries, 28 m below the Paris Observatory, are compared with current measurements performed in a limestone quarry, 20 m below ground surface, and with local and European surface temperature records. When averaged using a backward 11-year moving window, the surface temperature time series looks similar and exhibits the already well-known 1 degrees C temperature increase over the last century. In addition, since about 1987, a steeper increase of about 0.07 degrees C per year is noticed on all surface records. Underground temperatures, unaffected by surface fluctuations and averaging procedures, show a 0.9 degrees C increase and thus confirm the trend indicated by the surface records. The averaged time series of the temperature in Paris and of the Wolf number, an indicator of sunspot activity, were reasonably well correlated till 1987 but deviated significantly from each other after that date. The long-term connection between surface temperature and solar cycles is further supported by a temporal analysis of the frequency content at 11 years and 5.5 years. Visual correlations between temperature and sunspot numbers, unconvincing when using recent records, appear more striking with underground data from 1783 to 1852. This analysis suggests that solar activity played an important role in temperature changes till the last century, but that different processes, possibly related to human-induced changes in the climate system, have been taking place lately with increasing intensity, especially since 1987. Copyright (c) 2005 Royal Meteorological Society.
机译:将1783年至1852年在巴黎天文台下方28 m的地下画廊中进行的仔细温度测量与在地下20 m以下的石灰石采石场中进行的当前测量进行比较,并与当地和欧洲的地面温度记录进行比较。当使用向后11年的移动窗口进行平均时,表面温度时间序列看起来很相似,并且在上个世纪表现出众所周知的1摄氏度的温度升高。另外,自1987年以来,在所有地面记录中都注意到每年约0.07摄氏度的急剧上升。不受地面波动和平均程序影响的地下温度显示出0.9摄氏度的升高,因此确认了地面记录所指示的趋势。巴黎的平均温度时间序列和太阳黑子活动的指标沃尔夫数的平均时间序列在1987年之前具有较好的相关性,但在此之后彼此之间有明显的偏离。通过对11年和5.5年的频率含量进行时间分析,进一步支持了表面温度与太阳周期之间的长期联系。温度和太阳黑子数之间的视觉相关性,使用最近的记录时令人信服,在1783年至1852年的地下数据中显得更为明显。该分析表明,直到上个世纪,太阳活动在温度变化中都起着重要作用,但是不同的过程可能相关近年来,人们对气候系统变化的反应日趋强烈,特别是自1987年以来。版权(c)2005年皇家气象学会。

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