Earth's Axis and Revolution (Grade 11 NSC Matric Geography): Flashcards

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Earth's Axis and Revolution
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Radiation

Transfer of energy through electromagnetic waves

Solar radiation

Energy from the sun

Terrestrial radiation

Long-wave radiation emitted by Earth

Convection

Warm air rises carrying heat upward

Two factors affecting solar radiation received

Length of day/night and angle of sun's rays

Sun angle at 90° effect

Energy concentrated in 1 sq metre, maximum heating

Parallelism of the axis

Earth's axis always points same direction; 23.5° tilt

Solstices dates

21 June and 21 December

Equinoxes dates

20 March and 22 September

Day/night length at equinoxes

Equal everywhere on Earth (12 hours each)

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