The Sun reaches the zenith (directly overhead) at midday ___________. Select all the options that make the statement true.
A. everywhere in the Southern Hemisphere on the December solstice
B. on the equator only on the March and September equinoxes
C. on the Arctic circle (66.5°N) on the June solstice
D. on the equator every day
E. everywhere in the Northern Hemisphere on the June solstice
F. everywhere within the tropics (between latitudes 23.5°N and 23.5°S) on two dates each year



Answer :

Answer: (option b) on the equator only on the March and September equinoxes

Explanation:One of the abecedarian data of life at Earth’s midlatitudes, where utmost of this book’s compendiums live, is that there are significant variations in the heat we admit from the Sun during the course of the time. We therefore divide the time into seasons, each with its different quantum of sun. The difference between seasons gets more pronounced the further north or south from the ambit we travel, and the seasons in the Southern Hemisphere are the contrary of what we find on the northern half of Earth. With these observed data in mind, let us ask what causes the seasons.

numerous people have believed that the seasons were the result of the changing distance between Earth and the Sun. This sounds reasonable at first it should be colder when Earth is further from the Sun. But the data do n’t bear out this thesis. Although Earth’s route around the Sun is an cirque, its distance from the Sun varies by only about 3. That’s not enough to beget significant variations in the Sun’s heating. To make matters worse for people in North America who hold this thesis, Earth is actually closest to the Sun in January, when the Northern Hemisphere is in the middle of downtime.



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