wobbling$520595$ - translation to greek
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wobbling$520595$ - translation to greek

PERIODIC CHANGES IN THE ORBITAL MOVEMENTS OF THE EARTH
Milankovitch cycle; Milankovitch wobble; Milankovitch hypothesis; Milankovich Effect; Milankovich cycle; Milankovich cycles; Milenkovich cycle; Milankovitch variations; Milankovich variations; Earth wobble; Milankovitch Cycle; Milankovitch theory; Milankovic cycles; Millankovich cycle; Millankovich cycles; Milankovic cycle; Melankovitch Cycle; Milankovics cycle; Astronomic theory of glaciation; Astronomical theory of paleoclimates; Milanković cycles; Global wobble; Global wobbles; Global wobbling; Milankovitch theory of ice ages; Milankovitch's theory; Milankovich's theory
  • [[Tabernas Desert]], Spain: Cycles can be observed in the colouration and resistance of different sediment strata.
  • 22.1–24.5° range of Earth's obliquity.
  • Axial precessional movement.
  • Variations of cycle times, curves determined from ocean sediments.
  • Past and future estimations of daily average insolation at top of the atmosphere on the day of the summer solstice, at 65° N latitude. The green curve is with eccentricity ''e'' hypothetically set to 0. The red curve uses the actual (predicted) value of ''e''; the blue dot indicates current conditions (2000 CE).
  • Vostok ice core (Antarctica)}}
{{br}}• Vertical gray line shows present (2000 CE)
  • Planets orbiting the Sun follow elliptical (oval) orbits that rotate gradually over time (apsidal precession). The eccentricity of this ellipse, as well as the rate of precession, are exaggerated for visualization.
  • 420,000 years of ice core data from [[Vostok, Antarctica]] research station, with more recent times on the left.

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Wikipedia

Milankovitch cycles

Milankovitch cycles describe the collective effects of changes in the Earth's movements on its climate over thousands of years. The term was coined and named after Serbian geophysicist and astronomer Milutin Milanković. In the 1920s, he hypothesized that variations in eccentricity, axial tilt, and precession combined to result in cyclical variations in the intra-annual and latitudinal distribution of solar radiation at the Earth's surface, and that this orbital forcing strongly influenced the Earth's climatic patterns.