It is common
knowledge that the Earth is predominantly heated from the Sun. Any variation in
the solar activity might, therefore, be a potential factor for changes in the terrestrial
climate.
The 11-year sunspot
cycle is well known phenomena, and so are, to a lesser degree, also the 22-year
cycle, the 80 year Gleissberg Cycle (sometimes even given as 60 year), the 120
year VMV Cycle and the 240 de Vries Cycle. The search for those cycles in terrestrial
variables has a long history (e.g. Schove, 1983; Sanders & Fairbridge,
1995; Finkl, 1995). Still, the matter was far from clear.
Friis-Christensen
and Lassen (1991) established an excellent correlation, for the last 150 years,
between changes in the length of the sunspot cycle and general changes in
global mean temperature. This gave evidence of a strong solar-terrestrial
linkage, despite the fact that the physics behind this linkage remained
unknown.
On the centennial
basis, the solar activity (instrumental, observation, aurora, aaindex, 14C-production,
10Be in-fall) exhibits cyclic variations between Solar Maxima and Solar Minima
(e.g. Stuiver and Quay, 1980; Hoyt and Schatten, 1993; Lean et al., 1995;
Cliver et al., 1998; Lean and Rind, 1999; Bard et al., 2000; Bond et al., 2001;
Mazzarella, 2007).
The Solar Minima –
the Dalton Minimum 1800–1820, the Maunder Minimum 1645-1705, the Spörer Minimum
1420-1500 and the Wolf Minimum 1290-1350 –have attracted special attention
because they have been proposed to correlate (e.g. Eddy, 1976) with cold
periods or Little Ice Ages (Lamb, 1979). In the west European records (Guiot,
1992), there are quite clear cold minima at 1440-1460, 1687-1703 and 1808-1821
(Mörner, 1995, 2010), i.e. right within the last three Solar Minima.
The observed
solar-terrestrial interactions have been interpreted in the following three
ways, illustrated in Figure 4.
(1) Solar irradiance
The
solar-terrestrial interaction is often explained in terms of variations in
irradiance over the sun-spot cycle and it multiples (e.g. White et al., 1997).
The variation in energy output during a sunspot cycle is found to be far too
low, however, or only in the order of 0.2 % (Willson, 1997). Therefore, this
mechanism does not apply per se. Only by assuming unknown and
hypothetical amplifying forcing-functions may it be converted to effects large
enough to explain observed changes in climate (e.g. Lean et al., 1995).
(2) Solar Wind and
cosmic ray in-fall
In a number of
papers, Svensmark (e.g. 1998, 2007) has proposed that Earth climate may be
strongly controlled by cloud formation driven by cosmic rays which, in its turn,
is modulated by the interaction of the Solar Wind with the Earth’s geomagnetic field.
Svensmark has proposed that this mechanism is responsible not only for the short-term
changes in climate, but also for the long-term changes through-out the Earth’s
history (Svensmark & Calder, 2007). This is a splendid new theory.
(3) Solar Wind and
Earth’s rate of rotation
Changes in Earth’s
rate of rotation due to Solar Wind changes is a novel concept (Mörner, 1995,
1996b, 2010; Gu, 1998; Mazzarella, 2008), but several authors have noted a
correlation between sunspot activity and Earth’s rotation (e.g. Kalinin and Kiselev,
1976; Golovkov, 1983; Mazzarella and Palumbo, 1988; Rosen and Salstein, 2000;
Abarca del Rio et al., 2003; Mazzarella, 2007, 2008; Mörner, 2010, Le Mouël et
al., 2010) or Solar-planetary cycles and Earth’s rotation (e.g. Scafetta,
2010). Due to the changes in rotation, the oceanic surface current system is
forced to respond (Figure 1). As a function of this, the Gulf Stream alters its
main distribution of water along the northern and southern branches, and
simultaneously cold Arctic water can, at the speeding-up phases of Solar
Minima, penetrate far down along the west coasts of Europe creating Little Ice
Age environmental conditions (Figure 2).
Alternatively, a
planetary beat (cf. Mörner, 1984a) may act not only on the Sun causing its
variations in time, but also directly on the Solar Wind interaction with the magnetosphere
by magnetic torques and/or by gravitational forces on the Earth’s rate of
rotation (Scafetta, 2010). The correlation between the 60 years terrestrial LOD
cycle and the 60 years cycle of changes in the orbital speed of the Sun around
the centre of mass of the solar system (SCMSS) is striking (Scafetta, 2010, Fig
14).
Whatever, it is the
response in oceanic circulation that generates the changes in climate (Mörner,
1995, 1996b, 2010) illustrated in Figure 1 and 2.
(4) A combination of
points (2) and (3)
Finally, there are
all reasons to believe that mechanism 2 and 3 may interact and operate
simultaneously.
NEXT SOLAR MINIMUM
The Solar activity
follows cyclic patterns, and can fairly easily be extended into the future.
What happened in the past will also happen in the future. The combination of cycles
can be done in different ways. Originally, we used a combination of the 60 year
“Gleissberg” and 240 year De Vries cycles for the past 600 years and extended
it into the Future giving a new Solar Minimum at around 2040-2050 as given in
Figure 5 (Mörner et al., 2003; Mörner, 2003, 2006a, 2006b, 2007).
The onset of the
associated cooling has been given at 2010 by Easterbrook (2010) and Herrara
(2010), and at “approximately 2014” by Abdassamatov (2010). Easterbrook (2010)
backs up his claim that the cooling has already commenced by geological
observations facts.
At any rate, from a
Solar-Terrestrial point of view, we will, by the middle of this century, be in
a New Solar Minimum and in a New Little Ice Age (Figure 7). This conclusion is
completely opposite to the scenarios presented by IPCC (2001, 2007) as
illustrated in Figure 3. With “the Sun in the centre”, no other conclusion can
be drawn, however.
ACKNOWLEDGEMENTS
In the years
1997-2003, I headed an INTAS project on “Geomagnetism and Climate”. It was
within this project that we lay the ground for the view on the
Solar-Terrestrial interaction (presented at the EGU-AGU-EGS meeting in Nice,
2003), later developed and integrated in the way here presented.
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Reviewed
by: Professor Don J. Easterbrook
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