North of the arctic circle, or south of the antarctic circle, but only at certain times of the year.
36.75
7(21) / 4
236 parts per hour.
half of a sphere is a hemisphere
hemisphere
no, because diffefernt parts of the world receive different amounts of sunlight because the earth is tilted on it's axis.
The Earth receives varying amounts of sunlight due to its spherical shape and tilted axis. This tilt causes different parts of the Earth to receive direct sunlight at different angles, leading to variations in the amount of sunlight received. Factors like seasons and Earth's orbit around the sun also affect the distribution of sunlight on Earth's surface.
The Earth's tilt results in the changing of seasons as different parts of the Earth receive varying amounts of sunlight throughout the year. This tilt is responsible for the differences in temperature and daylight hours experienced in different parts of the world during different times of the year.
Because the rays of the sun is so hot it will heat any part of the earth witout being hit my direct sunlight
The two polar regions, during the height of their respective summers. In the northern area, great parts of Scandinavia - and on the other hemisphere, Greenland and Alaska - have 24-hour sunlight in June and July
Earth rotates on its axis. This rotation is what causes day and night as different parts of the Earth receive sunlight at different times.
The tilt of the Earth's axis creates variations in the angle at which sunlight reaches different parts of the planet, leading to seasonal changes. As the Earth orbits the Sun, different parts of the planet receive direct sunlight, causing variations in temperature and daylight hours, resulting in the four seasons.
The parts of Earth that do not receive direct sunlight are the polar regions, specifically the North and South Poles, due to the tilt of the Earth's axis. This results in periods of continuous darkness during the winter months.
They receive more direct sunlight than the other parts of the globe.
The regions within or near the Arctic and Antarctic Circles can experience up to 24 hours of sunlight during the summer months. This phenomenon is known as the midnight sun and occurs because of the tilt of Earth's axis towards the sun during that time of the year.
The Earth is tilted on its axis at an angle of approximately 23.5 degrees. This tilt is responsible for the changing seasons as different parts of the Earth receive varying amounts of sunlight throughout the year.
The Earth is tilted on its axis at approximately 23.5 degrees. This tilt is what causes the change in seasons as different parts of the Earth receive varying amounts of sunlight throughout the year.