全新世气候对千年尺度太阳活动的可能响应  

Possible Response of Climate to Solar Activity on Millennial Scale during the Holocene

作　　者：尹志强[1] 韩延本[1] 王博[1] 

机构地区：[1]中国科学院国家天文台,北京100012

出　　处：《气象科技进展》2014年第4期9-12,共4页Advances in Meteorological Science and Technology

基　　金：国家重大科学研究计划项目(2012CB957801)

摘　　要：利用熟知的山洞石笋资料及重建的太阳黑子数获取的时间序列,讨论了长时间尺度上气候对太阳活动变化的可能响应。小波分析显示气候变化与太阳活动变化在约1000及约2000年周期上具有一致性,这可能反映了全新世时期太阳活动的调制作用。另外,小波功率谱显示在公元前2000年附近缺失千年周期,这种突变及气候条件的长期变化可能给许多地区带来社会性影响。Based on well-known series from land-based caves and reconstructed sunspot numbers, the nature of climatic response to solar variability is discussed over a long-time scale. Wavelet analysis reveals coherence between the climatic and solar oscillations with periods of～1000-and～2000-yr that may relfect a modulation of solar activity during the Holocene. Moreover, the wavelet power spectra present that～1000-yr cycle of these series is absent around～2000 BC and this abrupt change and prolonged changes in climatic conditions might have brought about major societal challenges to many regions.

关 键 词：古气候 太阳黑子数 全新世 

分 类 号：P461.1[天文地球—大气科学及气象学]