clouds, angle of instance, materials that absorb the suns energy, pollution, and objects
June 21
Changing the angle of insolation—how sunlight strikes a surface—affects the intensity and distribution of solar energy received. When the sun's rays hit a surface at a steeper angle, the energy is concentrated over a smaller area, leading to a more rapid temperature increase. Conversely, when the angle is shallower, the energy is spread over a larger area, resulting in a slower rate of temperature change. Thus, the angle of insolation plays a crucial role in determining how quickly surfaces heat up or cool down.
On March 21, which is the spring equinox, the latitude that receives the highest angle of insolation is the equator (0 degrees latitude). During this time, the sun is directly overhead at the equator, leading to the most direct sunlight and maximum insolation. Locations at higher latitudes receive sunlight at a lower angle, resulting in less intense insolation.
The albedo effect is how a darker material gets hotter faster than a lighter material. Insolation is the solar radiation from the sun.
sunspots
As the altitude of the sun increases, the intensity of insolation for that area will increase as well.
Intensity of insolation refers to the amount of solar energy received per unit area at a given location and time. It is typically measured in watts per square meter. Factors such as angle of incidence, atmospheric conditions, and time of day can affect the intensity of insolation.
At the Tropic of Capricorn.
Since they are at the same latitude it is most likely that something else is making the temperature different than the intensity of insolation affecting the temperature in both areas.
The intensity of insolation is affected by the altitude of the sun; the higher the sun is in the sky (higher altitude), the more direct the solar radiation is, resulting in higher intensity. When the sun is lower in the sky, the sunlight has to pass through a greater thickness of the Earth's atmosphere, which can scatter and absorb some of the radiation, reducing its intensity.
The angle of insolation affects the intensity of insolation directly. In other words, as the angle of insolation increases, so does the intensity of insolation because the Sun is directly overhead at Zenith, giving off direct, or vertical rays. The opposite happens when the angle of insolation decreases, causing a decrease in the intensity of insolation as well.
Angle of insolation refers to the angle at which the sun's rays strike the Earth's surface. The angle of insolation affects the intensity of solar energy received at a particular location. A higher angle of insolation results in more concentrated sunlight, while a lower angle spreads the sunlight out over a larger area.
Intensity of insolation refers to the amount of solar radiation that reaches a given area on the Earth's surface. It is typically measured in watts per square meter and can vary based on factors such as time of day, season, latitude, and atmospheric conditions. Higher intensity of insolation results in more solar energy being available for processes like heating and generating electricity.
June 21
On March 21, the Earth receives the greatest intensity of insolation at the equator, which is located at 0 degrees latitude. This date marks the vernal equinox, when the sun is directly overhead at the equator, resulting in nearly equal day and night lengths across the globe. As a result, the equator experiences the highest solar radiation intensity at this time.
June 21 at 12 noon
Direct and diffused insolation.