Climatic Changes: Their Nature and CausesHuntington, Ellsworth
Science
Climatic Changes: Their Nature and Causes
Huntington, Ellsworth
Climatic changes; Climatology; Paleoclimatology
The results set forth in that volume may be summarized as follows:
During the years 1911 and 1912, under the auspices of the Carnegie
Institution of Washington, measurements were made of the thickness of
the rings of growth on the stumps of about 450 sequoia trees in
California. These trees varied in age from 250 to nearly 3250 years. The
great majority were over 1000 years of age, seventy-nine were over 2000
years, and three over 3000. Even where only a few trees are available
the record is surprisingly reliable, except where occasional accidents
occur. Where the number approximates 100, accidental variations are
largely eliminated and we may accept the record with considerable
confidence. Accordingly, we may say that in California we have a fairly
accurate record of the climate for 2000 years and an approximate record
for 1000 years more. The final results of the measurements of the
California trees are shown in Fig. 4, where the climatic variations for
3000 years in California are indicated by the solid line. The high parts
of the line indicate rainy conditions, the low parts, dry. An
examination of this curve shows that during 3000 years there have
apparently been climatic variations more important than any which have
taken place during the past century. In order to bring out the details
more clearly, the more reliable part of the California curve, from 100
B. C. to the present time, has been reproduced in Fig. 5. This is
identical with the corresponding part of Fig. 4, except that the
vertical scale is three times as great.
[Illustration: _Fig. 4. Changes of climate in California (solid line)
and in western and central Asia (dotted line)._
Note. The curves of Figs. 4 and 5 are reproduced as published in _The
Solar Hypothesis_ in 1914. Later work, however, has indicated that in
the Asiatic curve the dash lines, which were tentatively inserted in
1914, are probably more nearly correct than the dotted lines. Still
further evidence indicates that the Asiatic curve is nearly like that of
California in its main features.]
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