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Season
Axial parallelism is a characteristic of the Earth (and most other orbiting bodies in space) in which the direction of the axis remains parallel to it
Axial parallelism is a characteristic of the Earth (and most other orbiting bodies in space) in which the direction of the axis remains parallel to itself throughout its orbit.
Illumination of Earth at each change of astronomical season
Illumination of Earth at each change of astronomical season
Two images showing the amount of reflected sunlight at southern and northern summer solstices respectively (watts / m2)
Two images showing the amount of reflected sunlight at southern and northern summer solstices respectively (watts / m2)
Angular size of the Sun at Earth's orbital periapsis called perihelion (max./closest, 2. to 5. January) and at apoapsis called aphelion (min./furthest
Angular size of the Sun at Earth's orbital periapsis called perihelion (max./closest, 2. to 5. January) and at apoapsis called aphelion (min./furthest, 3. to 6. July). The resulting 7% difference in solar intensity does not overpower geographic factors of climate, with seasons staying more moderate on the Southern Hemisphere due to having less landmass.
Summer
Summer in Belgium
Summer in Belgium
During summer in the polar regions, the sun can appear even at midnight. Photo of midnight sun in Inari, Finland.
During summer in the polar regions, the sun can appear even at midnight. Photo of midnight sun in Inari, Finland.
Wet season thunderstorm at night in Darwin, Northern Territory, Australia.
Wet season thunderstorm at night in Darwin, Northern Territory, Australia.
Image of Hurricane Ida from late August 2021.
Image of Hurricane Ida from late August 2021.