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Created by Commons user Mike1024, Earth based on File:Worldmap northern.svg: Author: Image of earth: Gringer. Scale orbits: Mike1024: Permission (Reusing this file) This image is based on a public domain image (File:Worldmap northern.svg) and is released into the public domain.
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Printable version; Page information; Get shortened URL ... A diagram depicting the seasons of the Flat Earth. Date: 2007-08-17, 2008-01-02: ... Description=A diagram ...
By astronomical convention, the four seasons are determined by the solstices (the two points in the Earth's orbit of the maximum tilt of the Earth's axis, toward the Sun or away from the Sun) and the equinoxes (the two points in the Earth's orbit where the Earth's tilted axis and an imaginary line drawn from the Earth to the Sun are exactly ...
This centre of gravity has no other physical significance but remains in line towards the moon as the Earth completes its diurnal rotation. It is this mutual centre of gravity which defines the path of the Eath-Moon system in solar orbit. Consequently the Earth's centre veers inside and outside the orbital path during each synodic month.
Given the different Sun incidence in different positions in the orbit, it is necessary to define a standard point of the orbit of the planet, to define the planet position in the orbit at each moment of the year w.r.t such point; this point is called with several names: vernal equinox, spring equinox, March equinox, all equivalent, and named considering northern hemisphere seasons.
See how our seasons come from Earth's tilt and yearly loop around the sun, which changes the ice cover, vegetation, and sunlight across the planet.
Orbit Center-to-center distance Altitude above the Earth's surface Speed Orbital period Specific orbital energy; Earth's own rotation at surface (for comparison— not an orbit) 6,378 km: 0 km: 465.1 m/s (1,674 km/h or 1,040 mph) 23 h 56 min 4.09 sec: −62.6 MJ/kg: Orbiting at Earth's surface (equator) theoretical 6,378 km: 0 km