The results demonstrate to us that there is a greater area across which the energy of the sun spans during our wintertime (as shown by the Winter ME model), which allows less energy per unit area to be distributed. This leads to the cooler times of the year, when snow is able to fall and we have to dress more heavily for the weather. They also demonstrate that during the Summer months, the Earth’s northern hemisphere is tilted towards the sun, and this tilt provides a smaller area across which the same energy can be spread. Lastly, it allows us to infer that because the Equator is the warmest of the three models, it is always able to receive the greatest amount of energy from the sun during the year, and is therefore subject to an annually hotter
The results demonstrate to us that there is a greater area across which the energy of the sun spans during our wintertime (as shown by the Winter ME model), which allows less energy per unit area to be distributed. This leads to the cooler times of the year, when snow is able to fall and we have to dress more heavily for the weather. They also demonstrate that during the Summer months, the Earth’s northern hemisphere is tilted towards the sun, and this tilt provides a smaller area across which the same energy can be spread. Lastly, it allows us to infer that because the Equator is the warmest of the three models, it is always able to receive the greatest amount of energy from the sun during the year, and is therefore subject to an annually hotter