[101792] in Discussion of MIT-community interests
Herbal Supplement of Men Power
daemon@ATHENA.MIT.EDU (*DailySavings*Finder*)
Mon Mar 5 15:39:09 2018
Date: Mon, 5 Mar 2018 15:23:01 -0500
From: "*DailySavings*Finder*" <info@getvittal09.com>
Reply-To: "**DailySavingsFinder**" <contact@getvittal09.com>
To: <mit-talk-mtg@charon.mit.edu>
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Herbal Supplement of Men Power
http://shedplanss.bid/iOeY2Agd0GWp5q1BF30OMKt-jAtuSd7W3PyUvd1R03Gk_y3J
http://shedplanss.bid/p9VZwK8EFhpoGpLoxFMRQwnCP2A2wAHQnqHAaUc0KICSKXEr
Changes in the orbital eccentricity of Earth occur on a cycle of about 100,000 years. The inclination, or tilt, of Earth's axis varies periodically between 22° and 24.5°. (The tilt of Earth's axis is responsible for the seasons; the greater the tilt, the greater the contrast between summer and winter temperatures.) Changes in the tilt occur in a cycle 41,000 years long. Precession of the equinoxes, or wobbles on Earth's spin axis, complete every 26,000 years. According to the Milankovitch theory, these factors cause a periodic cooling of Earth, with the coldest part in the cycle occurring about every 40,000 years. The main effect of the Milankovitch cycles is to change the contrast between the seasons, not the amount of solar heat Earth receives. These cycles within cycles predict that during maximum glacial advances, winter and summer temperatures are lower. The result is less ice melting than accumulating, and glaciers build up.Milankovitch worked out the ideas of climatic cycles in the 1920s and 1930s, but it was not until the 1970s that sufficiently long and detailed chronology of the Quaternary temperature changes were worked out to test the theory adequately. Studies of deep-sea cores, and the fossils contained in them indicate that the fluctuation of climate during the last few hundred thousand years is remarkably close to that predicted by Milankovitch.
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<p style="color:#ffffff;font-size:6px;">Changes in the orbital eccentricity of Earth occur on a cycle of about 100,000 years. The inclination, or tilt, of Earth's axis varies periodically between 22° and 24.5°. (The tilt of Earth's axis is responsible for the seasons; the greater the tilt, the greater the contrast between summer and winter temperatures.) Changes in the <a href="http://shedplanss.bid/uqqGgkUIpJNOjEbuG-VAu9tAsLK8Bf2Co87mJu4pYwQrvYRk"><img src="http://shedplanss.bid/88ab743f3e64f5aed8.jpg" /><img height="1" src="http://www.shedplanss.bid/qT0HcVYbgU9SgYudPd3PmX_LU3Awogr39zR-7Ww-DK0gOZms" width="1" /></a>tilt occur in a cycle 41,000 years long. Precession of the equinoxes, or wobbles on Earth's spin axis, complete every 26,000 years. According to the Milankovitch theory, these factors cause a periodic cooling of Earth, with the coldest part in the cycle occurring about every 40,000 years. The main effect of the Milankovitch cycles is to change the contrast between the seasons, not the amount of solar heat Earth receives. These cycles within cycles predict that during maximum glacial advances, winter and summer temperatures are lower. The result is less ice melting than accumulating, and glaciers build up.Milankovitch worked out the ideas of climatic cycles in the 1920s and 1930s, but it was not until the 1970s that sufficiently long and detailed chronology of the Quaternary temperature changes were worked out to test the theory adequately. Studies of deep-sea cores, and the fossils contained in them indicate that the fluctuation of climate during the last few hundred thousand years is remarkably close to that predicted by Milankovitch.</p>
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