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首页> 外文期刊>Global and planetary change >The controversial early brightening in the first half of 20th century: A contribution from pyrheliometer measurements in Madrid (Spain)
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The controversial early brightening in the first half of 20th century: A contribution from pyrheliometer measurements in Madrid (Spain)

机译:有争议的20世纪上半叶的早期增亮:来自马德里(西班牙)的日光辐射计测量结果

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摘要

A long-term decrease in downward surface solar radiation from the 1950s to the 1980s ("global dimming") followed by a multi-decadal increase up to the present ("brightening") has been detected in many regions worldwide. In addition, some researchers have suggested the existence of an "early brightening" period in the first half of the 20th century. However, this latter phenomenon is an open issue due to the opposite results found in literature and the scarcity of solar radiation data during this period. This paper contributes to this relevant discussion analyzing, for the first time in Southern Europe, the atmospheric column transparency derived from pyrheliometer measurements in Madrid (Spain) for the period 1911-1928. This time series is one of the three longest datasets during the first quarter of the 20th century in Europe. The results showed the great effects of the Katmai eruption (June 1912, Alaska) on transparency values during 1912-1913 with maximum relative anomalies around 8%. Outside the period affected by this volcano, the atmospheric transparency exhibited a stable behavior with a slight negative trend without any statistical significance on an annual and seasonal basis. Overall, there is no evidence of a possible early brightening period in direct solar radiation in Madrid. This phenomenon is currently an open issue and further research is needed using the few sites with available experimental records during the first half of the 20th century.
机译:从1950年代到1980年代,向下表面的太阳辐射长期减少(“全球变暗”),直到现在为止,年代际增加了数十倍(“变亮”),这在世界范围内的许多地区都已被发现。此外,一些研究人员建议在20世纪上半叶存在“早期提亮”时期。但是,由于文献中的相反结果以及此期间太阳辐射数据的稀缺性,后一种现象是一个未解决的问题。本文为这一相关讨论做出了贡献,这是在南欧首次分析了在1911-1928年间从马德里(西班牙)的日射强度计测量得出的大气柱透明度。该时间序列是20世纪上半叶欧洲最长的三个数据集之一。结果表明,卡特迈火山喷发(1912年6月,阿拉斯加)对1912年至1913年的透明度值有很大的影响,最大相对异常约为8%。在受该火山影响的时期之外,大气透明性表现出稳定的行为,略有负面趋势,在年度和季节基础上没有任何统计意义。总体而言,没有证据表明马德里太阳直接辐射可能会出现早期变亮期。这种现象目前是一个未解决的问题,需要在20世纪上半叶使用少数具有可用实验记录的站点进行进一步研究。

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