500-Year Climate Cycles Stacking of Recent Centennial Warming Documented in an East Asian Pollen Record
1. Introduction Periodic climate changes on multidecadal to multicentennial scales induced by external and internal forcings are of importance not only for understanding the regional climate dynamic but also for assessing the contribution of anthropogenic forcing to the twentieth century warming (Mann et al., 2009; Moberg et al., 2005; Shen et al., 2013). Among these cyclic climate changes, the effect of the multicentennial scale solar variability is less certain. A ~500-year cycle in solar activity, inferred from global atmospheric14CO2 production variation (Stuiver and Braziunas, 1993) might have driven North Atlantic, North Pacific, and North America terrestrial climates (Chapman and Shackleton, 2000; Hu et al., 2003; Stuiver et al., 1995; Yu and Ito, 1999; Zhao et al., 2010). However, it remains to be seen whether this periodic paleoclimate changes is global or regional signals in the Holocene.
Arctic Oscillation/North Atlantic Oscillation North Atlantic deep water total solar irradiance
Deke Xu Houyuan Lu Guoqiang Chu Naiqin Wu
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Aca Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Aca
国际会议
The 6th International Maar Conference(IMC)(第六届国际玛珥会议)
长春
英文
107-110
2016-07-30(万方平台首次上网日期,不代表论文的发表时间)