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Published byVictor Simpson Modified over 8 years ago
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The last 600ky… LGM Last Glacial Maximum 18Ky
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Paleoclimataology Lecture notes from Ellen Druffel
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1. Eccentricity 3% range of variation of E-S distance due to eliptical orbit around Sun, Pull of large planets Now, perihelion occurs during northern Winter (3 January) 100ky and 413ky periods Now, e =.0167 (relatively circular)
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2. Tilt - Reason for Seasons Now tilt is 23.5°, and is decreasing. Higher the tilt, higher the seasonal differences Has gone from 24.5° -22.2°, varied by pull of large planets 41 ky period
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3. Precession - Wobble Varies E-S distance with season Variation of the direction in which the E axis leans. Caused by the pull of Sun and moon on Earth Now Earth’s axis points to Polaris 23 ky stronger period - combined wobble and slow turning of eliptical orbit. Now 11Kya
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On the long term…the precessional index Eccentricity variations at 100Ky and 413Ky modulate the amplitude of the precession cycle. This is why we have the 100Ky ice age cycle!
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How orbital theory, climate records ( 18 O) and northern hemisphere insolation (i.e. melting in N. Atlantic) compare over the past 600ky. Cold warm now LGM 18ky
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BLAG invokes chemical weathering
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Molnar & England, 1990
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