Solar activity levels in 2100

We consider the likely levels of solar activity in 2100 by analysing the previous history of long-term solar and geomagnetic activity indices. We make use of superposed periods of similar variations in atmospheric cosmogenic radiocarbon that have occurred during the last 11000 years, as derived from various proxies such as tree rings. This leads us to conclude that solar activity is peaking at about the present epoch, and we expect solar activity in 2100 to resemble that in 1900 when a small minimum in solar activity took place, rather than increasing as has occurred in the last 100 years. The occurrence of major geomagnetic storms will decline to about one-third of the present level.

[1]  M. Lockwood Twenty‐three cycles of changing open solar magnetic flux , 2003 .

[2]  Bernd Kromer,et al.  Persistent Solar Influence on North Atlantic Climate During the Holocene , 2001, Science.

[3]  Petra M. Udelhofen,et al.  Cloud cover variations over the United States: An influence of cosmic rays or solar variability? , 2001 .

[4]  A. Matter,et al.  Strong coherence between solar variability and the monsoon in Oman between 9 and 6 kyr ago , 2001, Nature.

[5]  S. Solanki,et al.  Evolution of the Sun's large-scale magnetic field since the Maunder minimum , 2000, Nature.

[6]  J. Beer Long-term indirect indices of solar variability , 2000 .

[7]  John F. B. Mitchell,et al.  Causes of twentieth-century temperature change near the Earth's surface , 1999, Nature.

[8]  R. Stamper,et al.  A doubling of the Sun's coronal magnetic field during the past 100 years , 1999, Nature.

[9]  H. Rishbeth,et al.  Increased magnetic storm activity from 1868 to 1995 , 1998 .

[10]  Edward W. Cliver,et al.  Solar variability and climate change: Geomagnetic aa index and global surface temperature , 1998 .

[11]  Douglas V. Hoyt,et al.  Group Sunspot Numbers: A New Solar Activity Reconstruction , 1998 .

[12]  Henrik Svensmark,et al.  Variation of cosmic ray flux and global cloud coverage—a missing link in solar-climate relationships , 1997 .

[13]  E. Friis-christensen,et al.  Length of the Solar Cycle: An Indicator of Solar Activity Closely Associated with Climate , 1991, Science.

[14]  M. Stuiver,et al.  Atmospheric 14C and century-scale solar oscillations , 1989, Nature.

[15]  N. Crooker,et al.  The solar wind at the turn of the century , 1978, Nature.

[16]  P. Mayaud,et al.  The aa indices: A 100-year series characterizing the magnetic activity , 1972 .

[17]  J. W. Beck,et al.  INTCAL98 Radiocarbon Age Calibration, 24,000–0 cal BP , 1998, Radiocarbon.

[18]  P. Reimer,et al.  High-Precision Radiocarbon Age Calibration for Terrestrial and Marine Samples , 1998, Radiocarbon.

[19]  P. Damon,et al.  The Sun as a Low-Frequency Harmonic Oscillator , 1992, Radiocarbon.