Variations in solar magnetic activity during the last 200,000 years: is there a Sun-climate connection?

被引:36
作者
Sharma, M [1 ]
机构
[1] Dartmouth Coll, Dept Earth Sci, Hanover, NH 03755 USA
基金
美国国家科学基金会;
关键词
solar activity; climate change; Be-10; cosmogenic elements; magnetic field; Milankovitch theory; solar cycles;
D O I
10.1016/S0012-821X(02)00516-2
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The production of Be-10 in the Earth's atmosphere depends on the galactic cosmic ray influx that, in turn, is affected by the solar surface magnetic activity and the geomagnetic dipole strength. Using the estimated changes in Be-10 production rate and the geomagnetic field intensity, variations in solar activity are calculated for the last 200 ka. Large variations in the solar activity are evident with the Sun experiencing periods of normal, enhanced and suppressed activity. The marine delta(18)O record and solar modulation are strongly correlated at the 100 ka timescale. It is proposed that variations in solar activity control the 100 ka glacial-interglacial cycles. However, the Be-10 production rate variations may have been under-estimated during the interval between 115 ka and 125 ka and may have biased the results. Future tests of the hypothesis are discussed. (C) 2002 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:459 / 472
页数:14
相关论文
共 79 条
  • [1] [Anonymous], 1997, ROLE SUN CLIMATE CHA
  • [2] Solar modulation of cosmogenic nuclide production over the last millennium: comparison between C-14 and Be-10 records
    Bard, E
    Raisbeck, GM
    Yiou, F
    Jouzel, J
    [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1997, 150 (3-4) : 453 - 462
  • [3] THE CAMP CENTURY BE-10 RECORD - IMPLICATIONS FOR LONG-TERM VARIATIONS OF THE GEOMAGNETIC DIPOLE-MOMENT
    BEER, J
    ANDREE, M
    OESCHGER, H
    SIEGENTHALER, U
    BONANI, G
    HOFMANN, H
    MORENZONI, E
    NESSI, M
    SUTER, M
    WOLFLI, W
    FINKEL, R
    LANGWAY, C
    [J]. NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIONS WITH MATERIALS AND ATOMS, 1984, 5 (02) : 380 - 384
  • [4] BERGER A, 1982, VISTAS ASTRON, V24, P103
  • [5] The 100-kyr ice-age cycle: internal oscillation or inclinational forcing?
    Berger, WH
    [J]. INTERNATIONAL JOURNAL OF EARTH SCIENCES, 1999, 88 (02) : 305 - 316
  • [6] QUATERNARY FOURIER STRATIGRAPHY - ORBITAL TEMPLATES AND MILANKOVITCH ANOMALIES
    BERGER, WH
    [J]. MATHEMATICAL GEOLOGY, 1994, 26 (07): : 769 - 781
  • [7] PRODUCTION OF RESIDUAL NUCLEI BY PROTON-INDUCED REACTIONS ON C, N, O, MG, AL AND SI
    BODEMANN, R
    LANGE, HJ
    LEYA, I
    MICHEL, R
    SCHIEKEL, T
    ROSEL, R
    HERPERS, U
    HOFMANN, HJ
    DITTRICH, B
    SUTER, M
    WOLFLI, W
    HOLMQVIST, B
    CONDE, H
    MALMBORG, P
    [J]. NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIONS WITH MATERIALS AND ATOMS, 1993, 82 (01) : 9 - 31
  • [8] Persistent solar influence on north Atlantic climate during the Holocene
    Bond, G
    Kromer, B
    Beer, J
    Muscheler, R
    Evans, MN
    Showers, W
    Hoffmann, S
    Lotti-Bond, R
    Hajdas, I
    Bonani, G
    [J]. SCIENCE, 2001, 294 (5549) : 2130 - 2136
  • [9] INSOLATION CHANGES, ICE VOLUMES, AND O-18 RECORD IN DEEP-SEA CORES
    BROECKER, WS
    VANDONK, J
    [J]. REVIEWS OF GEOPHYSICS AND SPACE PHYSICS, 1970, 8 (01): : 169 - +
  • [10] Solar variability and climate change: Geomagnetic aa index and global surface temperature
    Cliver, EW
    Boriakoff, V
    Feynman, J
    [J]. GEOPHYSICAL RESEARCH LETTERS, 1998, 25 (07) : 1035 - 1038