[40953] in Discussion of MIT-community interests
NASA Scientist Discovers anti-wrinkle secret, at bottom of Glacier...
daemon@ATHENA.MIT.EDU (Hydrate Your Skin)
Tue Apr 28 14:35:45 2015
To: <mit-talk-mtg@charon.mit.edu>
From: "Hydrate Your Skin" <HydrateYourSkin@mappellers.eu>
Date: Tue, 28 Apr 2015 11:35:45 -0700
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<p align="center">produces the precession of the equinoxes, this state of things will in time be reversed: [222] the Earth will be nearest to the sun during the summer LABPGID
of the northern hemisphere, and furthest from it during the southern 7ea99ed1b6714702bd5343b786c98bee summer or northern winter. The 7ea99ed1b6714702bd5343b786c98bee period required to complete the slow movement
producing these changes, is nearly 26,000 years; and were there no modifying process, the two AQLCF 7ea99ed1b6714702bd5343b786c98bee hemispheres would alternately experience this
coincidence of summer 7ea99ed1b6714702bd5343b786c98bee with relative nearness to the sun, during a period of 13,000 years. But there is also a still slower change in the direction of
the axis major of the Earth’s orbit; from which it results that the alternation we have described is completed in about 21,000 years. That is 7ea99ed1b6714702bd5343b786c98bee
to say, if at a given time the Earth is nearest to the sun at our mid-summer, and 7ea99ed1b6714702bd5343b786c98bee furthest CKUXLBV from the sun HJQY at our mid-winter; then, in 10,500
years afterwards, it will be furthest from the 7ea99ed1b6714702bd5343b786c98bee sun at our mid-summer, and nearest DFMJYEKTS at our mid-winter. Now the difference between the distances from
the sun at the two extremes of LWIRFNTXC this alternation, amounts to one-thirtieth; and hence, the difference between the quantities of heat received from the
sun on a summer’s day under these opposite conditions amounts to one-fifteenth. Estimating this, not with reference to the 7ea99ed1b6714702bd5343b786c98bee zero of our thermometers, but with reference 7ea99ed1b6714702bd5343b786c98bee to the temperature of the celestial
spaces, Sir John Herschel calculates “23° Fahrenheit, as the least variation of temperature under such circumstances which can reasonably be VGE
attributed to the actual variation of the sun’s distance.” Thus, then, each hemisphere has at a certain epoch, a short summer of extreme heat, followed 7ea99ed1b6714702bd5343b786c98bee
by a long and<u>very cold winter. Through the slow change in the direction of</u>HDCUEYFNP the Earth’s axis, these extremes are gradually mitigated. And at the end of
10,500 years, there is reached ESWSEW the opposite state—a long and moderate summer, with a short and mild winter. At present, in consequence of the
predominance of sea in the southern hemisphere, the extremes to which its astronomical conditions subject it, are much ameliorated; while the great ARSSDSDWX
proportion of 7ea99ed1b6714702bd5343b786c98bee land in the northern hemisphere, [223] tends to exaggerate such contrast as now exists in it between winter and summer: whence it
results that the climates of the two hemispheres are not widely unlike. But 10,000 years hence, the northern hemisphere will undergo annual variations QSYSPFX </p>
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<p align="left">of temperature far more marked than now. In the last edition of his Outlines of Astronomy, Sir 7ea99ed1b6714702bd5343b786c98bee John Herschel recognizes this as an element in YIC geological processes; regarding it as
possibly a part-cause of those climatic changes indicated by the records of the Earth’s past. That it has had much to do with those larger changes of TMBYD
climate of which we have evidence, seems unlikely, since there is reason to think that these TFXQ have been far 7ea99ed1b6714702bd5343b786c98bee 7ea99ed1b6714702bd5343b786c98bee slower and more lasting; but that it must
have entailed a rhythmical exaggeration and mitigation of the climates otherwise produced, seems beyond question. And BDPBUJTA it seems also beyond
question that there must have been a consequent rhythmical change 7ea99ed1b6714702bd5343b786c98bee in the distribution of organisms—a rhythmical change to which we here wish to draw .</p>
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