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100,000-year problem

The 100,000-year problem (also 100 ky problem or 100 ka problem) of the Milankovitch theory of orbital forcing refers to a discrepancy between the reconstructed geologic temperature record and the reconstructed amount of incoming solar radiation, or insolation over the past 800,000 years. Due to variations in the Earth's orbit, the amount of insolation…

Art, Hypotheses to explain the problem & Recognition of the 100,000-year cycle

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Recognition of the 100,000-year cycle

Hypotheses to explain the problem

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100,000-year problem

Nodes44
Edges43
Triples12
Avg. degree1.95
Density0.045455
Components1

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100,000-year problem

Top relations

related to Climatic resonance · 12
100,000-year problem → Earth, Elizabeth Reischmann, Free, Jeseung Oh, José, Northern Hemisphere, Opponents, Pleistocene, Rial, The, The Earth's, This

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Important terminology

100 ice years 000-year orbital eccentricity periodicity 000 insolation record milankovitch climate temperature past cycles problem effect ka forcing earth

Entity relationships Subject–Predicate–Object triples

SubjectPredicateObjectConfidenceSrc
100,000-year problemrelated to Climatic resonanceThe0.60section
100,000-year problemrelated to Climatic resonanceEarth0.60section
100,000-year problemrelated to Climatic resonanceThe Earth's0.60section
100,000-year problemrelated to Climatic resonanceOpponents0.60section
100,000-year problemrelated to Climatic resonanceThis0.60section
100,000-year problemrelated to Climatic resonanceFree0.60section
100,000-year problemrelated to Climatic resonanceNorthern Hemisphere0.60section
100,000-year problemrelated to Climatic resonanceJosé0.60section
100,000-year problemrelated to Climatic resonanceRial0.60section
100,000-year problemrelated to Climatic resonanceJeseung Oh0.60section
100,000-year problemrelated to Climatic resonanceElizabeth Reischmann0.60section
100,000-year problemrelated to Climatic resonancePleistocene0.60section

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