Solar Variability Over the Past Several Millennia

被引:0
|
作者
J. Beer
M. Vonmoos
R. Muscheler
机构
[1] Swiss Federal Institute of Environmental Science and Technology (EAWAG),
[2] NASA/Goddard Space Flight Center,undefined
来源
Space Science Reviews | 2006年 / 125卷
关键词
Solar activity; solar influence on climate; cosmogenic radionuclides;
D O I
暂无
中图分类号
学科分类号
摘要
The Sun is the most important energy source for the Earth. Since the incoming solar radiation is not equally distributed and peaks at low latitudes the climate system is continuously transporting energy towards the polar regions. Any variability in the Sun-Earth system may ultimately cause a climate change. There are two main variability components that are related to the Sun. The first is due to changes in the orbital parameters of the Earth induced by the other planets. Their gravitational perturbations induce changes with characteristic time scales in the eccentricity (∼100,000 years), the obliquity (angle between the equator and the orbital plane) (∼40,000 years) and the precession of the Earth’s axis (∼20,000 years). The second component is due to variability within the Sun. A variety of observational proxies reflecting different aspects of solar activity show similar features regarding periodic variability, trends and periods of very low solar activity (so-called grand minima) which seem to be positively correlated with the total and the spectral solar irradiance. The length of these records ranges from 25 years (solar irradiance) to 400 years (sunspots). In order to establish a quantitative relationship between solar variability and solar forcing it is necessary to extend the records of solar variability much further back in time and to identify the physical processes linking solar activity and total and spectral solar irradiance. The first step, the extension of solar variability, can be achieved by using cosmogenic radionuclides such as 10Be in ice cores. After removing the effect of the changing geomagnetic field, a 9000-year long record of solar modulation was obtained. Comparison with paleoclimatic data provides strong evidence for a causal relationship between solar variability and climate change. It will be the subject of the next step to investigate the underlying physical processes that link solar variability with the total and spectral solar irradiance.
引用
下载
收藏
页码:67 / 79
页数:12
相关论文
共 50 条
  • [21] Climate-induced variability in South Atlantic wave direction over the past three millennia
    A. P. Silva
    A. H. F. Klein
    A. F. H. Fetter-Filho
    C. J. Hein
    F. J. Méndez
    M. F. Broggio
    C. Dalinghaus
    Scientific Reports, 10
  • [22] A History of Solar Activity over Millennia
    Usoskin, Ilya G.
    LIVING REVIEWS IN SOLAR PHYSICS, 2013, 10 (01)
  • [23] A history of solar activity over millennia
    Ilya G. Usoskin
    Living Reviews in Solar Physics, 20
  • [24] Did agriculture beget agriculture during the past several millennia?
    Vavrus, Stephen J.
    Kucharik, Christopher J.
    He, Feng
    Kutzbach, John E.
    Ruddiman, William F.
    HOLOCENE, 2022, 32 (07): : 680 - 689
  • [25] Small influence of solar variability on climate over the past millennium
    Schurer A.P.
    Tett S.F.B.
    Hegerl G.C.
    Nature Geoscience, 2014, 7 (2) : 104 - 108
  • [26] Small influence of solar variability on climate over the past millennium
    Schurer, Andrew P.
    Tett, Simon F. B.
    Hegerl, Gabriele C.
    NATURE GEOSCIENCE, 2014, 7 (02) : 104 - 108
  • [27] Global surface temperatures over the past two millennia
    Mann, ME
    Jones, PD
    GEOPHYSICAL RESEARCH LETTERS, 2003, 30 (15) : 5 - 1
  • [28] Addendum: Small influence of solar variability on climate over the past millennium
    Andrew P. Schurer
    Simon F. B. Tett
    Gabriele C. Hegerl
    Nature Geoscience, 2015, 8 (2) : 159 - 159
  • [29] VEGETATION AND CLIMATIC-CHANGE OVER THE PAST 3 MILLENNIA
    MCGLONE, MS
    NEW ZEALAND JOURNAL OF ECOLOGY, 1987, 10 : 159 - 160
  • [30] Continental-scale temperature variability during the past two millennia
    Ahmed, Moinuddin
    Anchukaitis, Kevin J.
    Asrat, Asfawossen
    Borgaonkar, Hemant P.
    Braida, Martina
    Buckley, Brendan M.
    Buntgen, Ulf
    Chase, Brian M.
    Christie, Duncan A.
    Cook, Edward R.
    Curran, Mark A. J.
    Diaz, Henry F.
    Esper, Jan
    Fan, Ze-Xin
    Gaire, Narayan P.
    Ge, Quansheng
    Gergis, Joelle
    Gonzalez-Rouco, J. Fidel
    Goosse, Hugues
    Grab, Stefan W.
    Graham, Nicholas
    Graham, Rochelle
    Grosjean, Martin
    Hanhijarvi, Sami T.
    Kaufman, Darrell S.
    Kiefer, Thorsten
    Kimura, Katsuhiko
    Korhola, Atte A.
    Krusic, Paul J.
    Lara, Antonio
    Lezine, Anne-Marie
    Ljungqvist, Fredrik C.
    Lorrey, Andrew M.
    Luterbacher, Jurg
    Masson-Delmotte, Valerie
    McCarroll, Danny
    McConnell, Joseph R.
    McKay, Nicholas P.
    Morales, Mariano S.
    Moy, Andrew D.
    Mulvaney, Robert
    Mundo, Ignacio A.
    Nakatsuka, Takeshi
    Nash, David J.
    Neukom, Raphael
    Nicholson, Sharon E.
    Oerter, Hans
    Palmer, Jonathan G.
    Phipps, Steven J.
    Prieto, Maria R.
    NATURE GEOSCIENCE, 2013, 6 (05) : 339 - 346