TEXT F It had been known for many
decades that the appearance of sunspots is roughly periodic with an average
cycle of eleven years. Moreover, the incidence of solar flares and the flux of
solar cosmic rays, ultraviolet radiation and x-radiation all vary directly with
the sunspot cycle. But after more than a century of investigation, the relation
of these and other phenomena, known collectively as the solar-activity cycle, to
terrestrial weather and climate remains unclear. For example the sunspot
cycle and the allied magnetic-polarity cycle have been linked to periodicities
discerned in records of such variables as rainfall, temperature, and winds.
Invariably, however, the relation is weak, and commonly of dubious-statistical
significance. Effects of solar variability over longer terms
have also been sought. The absence of recorded sunspot activity in the notes
kept by European observers in the late seventeenth and early eighteenth
centuries has led some scholars to postulate a brief cessation of sunspot
activity at that time (a period called the Maunder minimum). The Maunder minimum
has been linked to a span of unusual cold in Europe extending from the sixteenth
to the early nineteenth centuries. The reality of the Maunder minimum has yet to
be established, however, especially since the records that Chinese naked-eye
observers of solar activity made at that time appear to contradict it.
Scientists have also sought evidence of long-term solar periodicities by
examining indirect climatological data, such as fossil records of the thickness
of ancient tree rings. These studies, however, failed to link unequivocally
terrestrial climate and the solar-activity cycle, or even to confirm the cycle’s
past existence. If consistent and reliable geological or
archaeological evidence tracing the solar-activity cycle in the distant past
could be found, it might also resolve an important issue in solar physics: how
to model solar activity. Currently, there are two models of solar activity. The
first supposes that the Sun’s internal motions (caused by rotation and
convection)interact with its large-scale magnetic field to produce a dynamo, a
device in which mechanical energy is converted into the energy of a magnetic
field. In short, the Sun’s large-scale magnetic field is taken to be
self-sustaining, so that the solar-activity cycle it drives would be maintained
with little overall change for perhaps billions of years. The alternative
explanation supposes that the Sun’s large-scale magnetic field is a remnant of
the field the Sun acquired when it formed, and is not sustained against decay.
In this model, the solar mechanism dependent on the Sun’s magnetic field runs
down more quickly. Thus, the characteristics of the solar-activity cycle could
be expected to change over a long period of time. Modern solar observations span
too short a time to reveal whether present cyclical solar activity is a
long-lived feature of the Sun, or merely a transient phenomenon. It can be inferred from the passage that studies attempting to use tree-ring thickness to locate possible links between solar periodicity and terrestrial climate are based on the assumption that ______.
A.the solar-activity cycle existed in its present form during the time period in which the tree rings grew B.the biological mechanisms causing tree growth are unaffected by short-term weather patterns C.average tree-ring thickness varies from species to species D.tree-ring thicknesses reflect changes in terrestrial climate