The Sun's rays strike the latitude of 23.5 degrees (the Tropic of Cancer) at a direct angle of 90 degrees during the summer solstice, around June 21. Conversely, at the Tropic of Capricorn, located at -23.5 degrees latitude, the Sun's rays strike directly at 90 degrees during the winter solstice, around December 21. Throughout the equinoxes, around March 21 and September 23, the Sun's rays are perpendicular to the equator, not at 23.5 degrees.
The angle of the sun's rays affects insolation, or incoming solar radiation, because when the rays strike the Earth's surface more directly, they distribute energy over a smaller area. This concentrated sunlight increases the intensity of solar radiation at that location. Conversely, when the sun's rays hit the surface at a shallow angle, the energy is spread over a larger area, resulting in lower insolation intensity. Thus, direct sunlight leads to higher temperatures and more intense solar energy absorption.
The light from the sun travels in a straight line, and we can assume the light rays to be parellel. The angle of incidence on the earths rounded surface depends on where you are on the earth and what time it is. Mid-day on the equator and the rays would hit the ground straight on. Further to the north or south, or later/earlier in the day and the light rays would hit at more of angle. The rays would also have to penitrate more of the earths atmosphere as the angle increases, which takes more `strength` out of the sun.
The plane upon which the Earth travels round the Sun is called the ecliptic. It is only when two bodies are on this plane, and in line with the Sun, that an eclipse is observed. Hence the name ecliptic. The Earth's spin axis is always oriented about 23.4 degrees from the ecliptic plane. The Earth's spin axis is never perpendicular to the Sun's rays. You may be referring to the Sun being directly overhead at the Equator twice per year.
The angle of the sun can be worked out through trigonometry, but first you will need the height of the object that is causing the shadow, since a taller object will make a longer shadow. Tan a = H/2.44 Where a is the angle and H is the height of the object. And the date is not relevant.
The length of daylight is directly influenced by the Sun's angle in the sky, which varies with the Earth's tilt and its orbit around the Sun. When the Sun is higher in the sky, during summer months or at the equator, daylight hours are longer. Conversely, during winter months or at higher latitudes, the Sun's lower angle results in shorter days. This relationship is a key factor in seasonal changes experienced across different regions.
true :)
June 21
it decreases... that's why the two poles are the coldest places on earth... however, considering the earth is a sphere the angle you are talking about is relative to the point on earth which you are referring to... therefore, there will always be a point on the earth's surface where the suns rays are hitting at exactly 90 degrees...
Absorbed
Obliquely
no
In summer the suns rays travel directly to the surface at a steep angle, so are still warm. In winter the rays strike at a shallower angle, and cool down rapidly as they travel a longer distance through the atmosphere before reaching the surface.
absorbed
During the daytime.
No, that's not a true statement. During winter, the sun's rays strike the Earth at a shallower angle, resulting in less direct sunlight and cooler temperatures. In contrast, during summer, the sun's rays hit the Earth more directly, leading to warmer temperatures. This difference in angle is due to the tilt of the Earth's axis as it orbits the sun.
the equater A+ 90 degrees
Only in the angle of incidence.