Temperature

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Latitude: Sun's rays hit to the Ecuator, on a relatively small area wich is very hot as a result.

Sun's rays strike the poles at an angle, solar energy spread out over a wider

Altitude: Temperature decreases at the altitude wich is why the montainous

hige areas are colder than other areas.

Distance from the sea: Temperature modelated in Costal Areas

and more extreme in inland continental areas.

Orientation: Temperature are hotter (sunny areas)

and colder in (shady areas)

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