The evolution of climateBrooks, C. E. P. (Charles Ernest Pelham)
Science
The evolution of climate
Brooks, C. E. P. (Charles Ernest Pelham)
Climatology; Paleoclimatology
The question of climatic changes during the historic period has been
the subject of much discussion, and several great meteorologists
and geographers have endeavoured to prove that at least since about
500 B.C. there has been no appreciable variation. It is admitted
that there have been shiftings of the centres of population and
civilization, first from Egypt and Mesopotamia to the Mediterranean
regions, and later to northern and western Europe, but these have
been attributed chiefly to political causes, and especially to the
rise of Islam and the rule of the “accursed Turk.” Recently, however,
there has arisen a class of evidence which cannot be explained away
on political grounds, and which appears to have decided the battle
in favour of the supporters of change; I refer to the evidence of
the trees, explained in the preceding chapter. The conclusions
derived from the big trees of California have fallen admirably into
line with archæological work in central America, in central Asia
and other regions, and have shown that the larger variations even
of comparatively recent times have been very extensive, if not
world-wide, in their development.
Let us consider first the evidence of the trees. These indicate
that after the moist period ending about A.D. 400, described in the
preceding chapter, the rainfall was generally light until about A.D.
1000, when it showed a sharp rise, probably to the level attained in
A.D. 1. (The correction for age renders an exact comparison between
periods a thousand years apart difficult.) This period of abundant
rainfall lasted some fifty years, followed by a gradual decline to a
brief minimum, shortly before A.D. 1200. About 1300 occurred another
rapid rise, reaching a maximum before 1350; the period of heavy rain
continued a short while after 1400, when a decline set in, reaching
a minimum at 1500, after which the rainfall recovered somewhat, and
subsequently maintained approximately its present level, with a
slight maximum about 1600 to 1645.
In the desert of Arizona, in regions at present too dry for
agriculture, there are abundant ruins, which are attributed by
Huntington to three periods:
(_a_) Pueblo ruins, dating back to just before the coming of the
Spaniards (i.e. about A.D. 1600), and indicating merely an increase
of population at the present centres.
(_b_) Ruins of an older civilization, termed by Huntington the
Pajaritan, during which numerous inhabitants lived in places where
at present no crops can be raised. “These people, as appears from
their pottery, their skulls and their methods of agriculture, belong
to a different civilization from that of the modern Pueblos who
inhabited Gran Quivera at the time of the coming of the Spaniards.
They had evidently disappeared long before that date, as is evident
from the present ruins of their villages, and from the absence of any
hint of their existence in the early annals of the country” (_Geogr.
Journal_, 40, 1912, p. 396).
Public-domain text, read in full here on John Shaqi.
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