Temporal and spatial response of Holocene temperature to solar activity

被引:5
作者
Lu, Wei [1 ,2 ]
Zhao, Xinhua [1 ,3 ,4 ]
Feng, Xueshang [1 ]
Xiang, Nanbin [5 ]
Du, Zhanle [4 ]
Zhang, Wanting [1 ,2 ]
机构
[1] Chinese Acad Sci, Natl Space Sci Ctr, State Key Lab Space Weather, Beijing 100190, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Yading Space Weather Sci Ctr, Ganzi 627750, Sichuan, Peoples R China
[4] Natl Astron Observ, CAS Key Lab Solar Act, Beijing 100101, Peoples R China
[5] Chinese Acad Sci, Yunnan Observ, Kunming 650011, Yunnan, Peoples R China
关键词
Solar activity; Holocene temperature; Solar-terrestrial relationship; CLIMATE; CYCLE; OSCILLATION; SIGNALS;
D O I
10.1016/j.quaint.2021.09.006
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Based on the latest database, we analyze the characteristics of the changing trends of sunspot number (SSN) and temperatures of the global mean surface (GMST) as well as six latitude bands during the Holocene, aiming to explore the long-term responses of the Holocene temperatures to solar activity. We adopt two methods, i.e., the 300-year moving average and the singular spectrum analysis to obtain the long-term trends of signals. We find that the average changes in the amplitude of temperatures in the Northern Hemisphere (NH) (3.65 degrees C) was greater than that in the Southern Hemisphere (SH) (1.28 degrees C) during the entire Holocene. There was one peak of temperatures (at 6500 BP) and two peaks of solar activity (at 4500 BP and 2000 BP) during our study interval. Spatially, the temperatures in the NH were more sensitive to solar forcing than those in the SH, especially in the latitude bands of 0 degrees-30 degrees N and 60 degrees N-90 degrees N. Moreover, the latitude band 0 degrees-30 degrees N had the strongest correlation with solar activity (C.C. = 0.38 for the 300-year moving average and C.C. = 0.55 for the singular spectrum analysis, p < 0.01), while the latitude band 60 degrees S-90 degrees S had the weakest correlation with solar activity (not significant in the statistical sense). Regarding the time response, solar forcing nearly did not affect the terrestrial temperatures in the early Holocene (8700 BP-6500 BP). While positive correlations started to be strong since 4500 BP and became stronger during 2000 BP-100 BP. All in all, the terrestrial temperatures were consistent with solar activity in the long-term trend during the Holocene, especially in the NH. Although many mysteries in historical climate reconstructions remain un-resolved, evaluating the impact of solar force on terrestrial temperature is crucial to reconstruct and predict terrestrial climate. Much deeper specific research on solarterrestrial mechanisms deserves to be put on the agenda.
引用
收藏
页码:39 / 45
页数:7
相关论文
共 39 条
[1]   Solar irradiance, climatic indicators and climate change - An empirical analysis [J].
Bhargawa, Asheesh ;
Singh, A. K. .
ADVANCES IN SPACE RESEARCH, 2019, 64 (01) :271-277
[2]   Seasonal origin of the thermal maxima at the Holocene and the last interglacial [J].
Bova, Samantha ;
Rosenthal, Yair ;
Liu, Zhengyu ;
Godad, Shital P. ;
Yan, Mi .
NATURE, 2021, 589 (7843) :548-+
[3]   Eleven-year solar cycles over the last millennium revealed by radiocarbon in tree rings [J].
Brehm, Nicolas ;
Bayliss, Alex ;
Christl, Marcus ;
Synal, Hans-Arno ;
Adolphi, Florian ;
Beer, Juerg ;
Kromer, Bernd ;
Muscheler, Raimund ;
Solanki, Sami K. ;
Usoskin, Ilya ;
Bleicher, Niels ;
Bollhalder, Silvia ;
Tyers, Cathy ;
Wacker, Lukas .
NATURE GEOSCIENCE, 2021, 14 (01) :10-+
[4]   Modulation of the Arctic Oscillation and the East Asian Winter Climate Relationships by the 11-year Solar Cycle [J].
Chen Wen ;
Zhou Qun .
ADVANCES IN ATMOSPHERIC SCIENCES, 2012, 29 (02) :217-226
[5]   Pacific warm pool subsurface heat sequestration modulated Walker circulation and ENSO activity during the Holocene [J].
Dang, Haowen ;
Jian, Zhimin ;
Wang, Yue ;
Mohtadi, Mahyar ;
Rosenthal, Yair ;
Ye, Liming ;
Bassinot, Franck ;
Kuhnt, Wolfgang .
SCIENCE ADVANCES, 2020, 6 (42)
[6]   A 449 year warm season temperature reconstruction in the southeastern Tibetan Plateau and its relation to solar activity [J].
Duan, Jianping ;
Zhang, Qi-Bin .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2014, 119 (20) :11578-11592
[7]   Sunspot cycle prediction using Warped Gaussian process regression [J].
Goncalves, Italo G. ;
Echer, Ezequiel ;
Frigo, Everton .
ADVANCES IN SPACE RESEARCH, 2020, 65 (01) :677-683
[8]   SOLAR INFLUENCES ON CLIMATE [J].
Gray, L. J. ;
Beer, J. ;
Geller, M. ;
Haigh, J. D. ;
Lockwood, M. ;
Matthes, K. ;
Cubasch, U. ;
Fleitmann, D. ;
Harrison, G. ;
Hood, L. ;
Luterbacher, J. ;
Meehl, G. A. ;
Shindell, D. ;
van Geel, B. ;
White, W. .
REVIEWS OF GEOPHYSICS, 2010, 48
[9]  
Hertzberg J, 2021, NATURE, V589, P521, DOI 10.1038/d41586-021-00115-x
[10]   Solar signals in CMIP-5 simulations: the ozone response [J].
Hood, L. L. ;
Misios, S. ;
Mitchell, D. M. ;
Rozanov, E. ;
Gray, L. J. ;
Tourpali, K. ;
Matthes, K. ;
Schmidt, H. ;
Chiodo, G. ;
Thieblemont, R. ;
Shindell, D. ;
Krivolutsky, A. .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2015, 141 (692) :2670-2689