Pangaea was centered around the equator during the Triassic period, spanning from about 90°N to 60°S latitude.
The tilt of the Earth on its axis causes the northern hemisphere to receive less direct sunlight during its winter months, leading to cooler temperatures. In contrast, the southern hemisphere receives more direct sunlight during its summer months, resulting in warmer temperatures.
At the Spring and Autumn Equinox, the sun is directly over the equator which is at 0 degrees latitude.
The thermal pole of a subcontinent is the location within the subcontinent that experiences the highest average temperatures. This area typically receives direct sunlight and has minimal cloud cover, resulting in intense heating of the land surface. In India, for example, the thermal pole is usually in the northwestern region, such as Rajasthan, during the summer months.
The area in the spot is largest during the summer months when the spot receives maximum sunlight and warmth, promoting lush vegetation growth.
The equator, which is at 0 degrees latitude, receives the most intense solar energy on March 21 and September 22 due to being closest to the sun during the equinoxes. At this time, the sun is directly overhead at noon at the equator, providing maximum solar energy.
The latitude of 90°N, also known as the North Pole, does not receive direct sunlight year-round because of the tilt of the Earth's axis. Instead, it experiences polar day (24-hour daylight) during the summer months and polar night (24-hour darkness) during the winter months. The latitude that receives the most direct rays of the sun year-round is the Equator, at 0° latitude.
The poles receive the least direct energy from the sun because of their high latitude and the tilt of the Earth's axis. This results in long periods of darkness during winter and limited direct sunlight even during summer.
During the equinoxes, when the Sun is at its highest, it will be at a distance from the zenith which is the same as your geographical latitude, but in the opposite direction. For example, if you live 50 degrees north of the equator, the Sun will be 50 degrees south of the zenith at noon.
The distribution of incoming solar radiation during the course of a year is exactly equal at both poles, and neither of them ever receives any 'direct' rays.
The area near the poles receives the least direct sunlight due to the tilt of the Earth's axis. This results in long periods of darkness during winter months.
At the Equinoxes, the Sun is directly above the equator.
The Philippines is closer to the equator, resulting in more direct sunlight and higher temperatures year-round. In contrast, Canada's higher latitude means it receives less direct sunlight and has colder temperatures, especially during the winter months.
During the equinoxes, when the Sun is at its highest, it will be at a distance from the zenith which is the same as your geographical latitude, but in the opposite direction. For example, if you live 50 degrees north of the equator, the Sun will be 50 degrees south of the zenith at noon.
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