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首页> 外文期刊>Quaternary International >Reconstruction of sunspot activity, cold and warm events, and drought and flood events in the central plain of China during the northern Song Dynasty using historical documents
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Reconstruction of sunspot activity, cold and warm events, and drought and flood events in the central plain of China during the northern Song Dynasty using historical documents

机译:利用历史文献资料重建北宋中原地区的黑子活动,冷暖事件,干旱和洪水事件

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摘要

The Northern Song Dynasty was an important and prosperous dynasty in the history of China, and it existed during a period of climate abnormality. Climate change research for the Northern Song Dynasty era has significance for understanding the interaction between agricultural civilizations in the central plains and nomadic populations in northern China, transfer of the economic and cultural centers of China, and the vicissitudes of the Northern Song Dynasty. There is currently considerable disagreement regarding climate change in the Central Plain during the Northern Song Dynasty era. Many precious and valuable historical documents and records about the Northern Song Dynasty have been collected, and abundant records of sunspot activity, cold and warm weather, drought and flood events have been compiled. Using the Mann-Kendall test, wavelet analysis, R/S analysis, and frequency analysis etc. mathematical statistics methods, sunspot activity, cold and warm events, and drought and flood events were quantitatively reconstructed. There are 15 sunspot maximum years and 16 sunspot minimum years, the cycle length of sunspot activity is 8-14 years, and the average cycle length is 11 years. Hot years account for 11.3% of the total years; warm years account for 12.7%; cold years account for 20.7%; and freezing cold years account for 3.3%. Mann-Kendall test results show that cold and warm variations are natural fluctuations, and there is no indication of abrupt climate change during the Northern Song Dynasty. Morlet wavelet analysis indicates that there are weak high-frequency oscillations and short oscillation periods with three years before 1052 AD, and there are oscillation periods of six years and clear alternations between warmth and cold during 1060-1120 AD. R/S analysis indicates that the Hurst index (II) of cold and warm index series is 0.6155, and the fractal dimension (D) is 1.3845. Since 0.5 < H < 1 and 1 < D < 1.5, fractal structures are evident in the time series of cold and warm indexes, past increments are positively correlated with future increments, and the average cycle length in the time series for cold and warm indexes is 6 years. Temperatures first decreased rapidly followed by a slow increase with long-term fluctuations, and the mean temperature during the Northern Song Dynasty era is 0.4 degrees C higher than that in the period 1880-1979 AD. Severe drought, moderate drought, moderate flood, severe flood and normal years account for 15.3%, 25.3%, 11.3%, 6.7%, 41.4% of all years, respectively. Frequency analysis indicates that cooling, warming, drought and flood events show a close relationship to sunspot activity.
机译:北宋是中国历史上重要而繁荣的王朝,存在于气候异常时期。北宋时代的气候变化研究对于了解中原农业文明与中国北方游牧人口之间的相互作用,中国经济文化中心的转移以及北宋的沧桑具有重要意义。目前,北宋时期中原地区在气候变化方面存在很大分歧。收集了许多有关北宋的珍贵和有价值的历史文献和记录,并汇编了许多有关黑子活动,寒冷和温暖的天气,干旱和洪水事件的记录。使用Mann-Kendall检验,小波分析,R / S分析和频率分析等,对数学统计方法,黑子活动,冷热事件以及干旱和洪水事件进行了定量重建。有15个黑子最大年份和16个最小黑子年份,黑子活动的周期长度是8-14年,平均周期长度是11年。热门年份占总年份的11.3%;温暖的年份占12.7%;寒冷年份占20.7%;寒冷年份占3.3%。曼恩·肯德尔(Mann-Kendall)的测试结果表明,冷暖变化是自然波动,在北宋期间没有任何气候突变的迹象。 Morlet小波分析表明,在1052 AD之前的三年中,高频振荡较弱,振荡周期较短;在1060-1120 AD时,存在六年的振荡周期,且冷暖交替明显。 R / S分析表明,冷热指数系列的赫斯特指数(II)为0.6155,分形维数(D)为1.3845。由于0.5

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