There is no 'why' because that statement is false. The equator is right in the CENTER
of the tropics. As the sun wiggles back and forth between the edges of the tropics
each year, the equator is the place that receives the MOST average insolation.
As latitude increases, the temperature tends to decrease. This is because the amount of solar energy received decreases as you move away from the equator towards the poles. The angle at which sunlight hits the Earth's surface becomes more oblique at higher latitudes, resulting in less direct heating.
Insolation is intercepted solar radiation.
In general, as latitude increases away from the equator towards the poles, temperatures tend to decrease. This is due to a variety of factors, including the angle of sunlight hitting Earth's surface, the length of daylight hours, and the amount of atmosphere sunlight must pass through.
The latitude that receives the most amount of UV light is the equator (around 0 degrees latitude), due to its position closest to the sun and the more direct angle of sunlight it receives. UV intensity decreases as you move towards the poles.
Insolation stands for incoming solar radiation, which refers to the amount of solar energy that reaches a specific area on the Earth's surface over a given period of time. The level of insolation can vary depending on factors such as time of day, season, latitude, and atmospheric conditions.
The temperature goes up because when the angle of insolation increases, it means that the sun's rays are becoming more directly focused on that area. That makes it hotter.For example, the equator is very hot. That's because that's where the sun's rays focus on most directly.The day is warm, and the night is cold.Summer is hot all day long if the angle of the sun is direct.YEARS:Summer = DirectWinter = IndirectFall/Spring = Half
The equatorial region near the equator receives the highest insolation due to the direct angle of the sun's rays. This region receives a higher amount of solar energy compared to other areas on Earth.
Insolation
That hemisphere is tilted towards the sun to its greatest amount. It is the summer solstice in that hemisphere. The sun reaches its highest point and you have the most amount of daylight hours. The further from the equator you are, the more hours of daylight there is.That hemisphere is tilted towards the sun to its greatest amount. It is the summer solstice in that hemisphere. The sun reaches its highest point and you have the most amount of daylight hours. The further from the equator you are, the more hours of daylight there is.That hemisphere is tilted towards the sun to its greatest amount. It is the summer solstice in that hemisphere. The sun reaches its highest point and you have the most amount of daylight hours. The further from the equator you are, the more hours of daylight there is.That hemisphere is tilted towards the sun to its greatest amount. It is the summer solstice in that hemisphere. The sun reaches its highest point and you have the most amount of daylight hours. The further from the equator you are, the more hours of daylight there is.That hemisphere is tilted towards the sun to its greatest amount. It is the summer solstice in that hemisphere. The sun reaches its highest point and you have the most amount of daylight hours. The further from the equator you are, the more hours of daylight there is.That hemisphere is tilted towards the sun to its greatest amount. It is the summer solstice in that hemisphere. The sun reaches its highest point and you have the most amount of daylight hours. The further from the equator you are, the more hours of daylight there is.That hemisphere is tilted towards the sun to its greatest amount. It is the summer solstice in that hemisphere. The sun reaches its highest point and you have the most amount of daylight hours. The further from the equator you are, the more hours of daylight there is.That hemisphere is tilted towards the sun to its greatest amount. It is the summer solstice in that hemisphere. The sun reaches its highest point and you have the most amount of daylight hours. The further from the equator you are, the more hours of daylight there is.That hemisphere is tilted towards the sun to its greatest amount. It is the summer solstice in that hemisphere. The sun reaches its highest point and you have the most amount of daylight hours. The further from the equator you are, the more hours of daylight there is.That hemisphere is tilted towards the sun to its greatest amount. It is the summer solstice in that hemisphere. The sun reaches its highest point and you have the most amount of daylight hours. The further from the equator you are, the more hours of daylight there is.That hemisphere is tilted towards the sun to its greatest amount. It is the summer solstice in that hemisphere. The sun reaches its highest point and you have the most amount of daylight hours. The further from the equator you are, the more hours of daylight there is.
As latitude increases, the temperature tends to decrease. This is because the amount of solar energy received decreases as you move away from the equator towards the poles. The angle at which sunlight hits the Earth's surface becomes more oblique at higher latitudes, resulting in less direct heating.
Angle of Sunlight – Near the equator, the sun’s rays hit directly, delivering more energy per unit area. As latitude increases, sunlight spreads over a larger surface, reducing intensity. Atmospheric Path – At higher latitudes, sunlight passes through more of the Earth's atmosphere, leading to greater scattering and absorption of energy. Seasonal Variation – Higher latitudes experience more variation in day length and sun angle, leading to extreme differences in insolation between summer and winter. Let me know if you need more details!
The amount of heat from the equator becomes less as one moves towards the poles due to the increasing angle of sunlight. Near the equator, sunlight hits the Earth's surface more directly, providing more heat. However, as you move towards the poles, the sunlight is spread over a larger area, leading to less heat per unit area.
Insolation is intercepted solar radiation.
The function that provides insolation is solar radiation, specifically solar energy received by the Earth's surface. Insolation is the amount of solar radiation reaching a specific area over a given time period. It is an essential factor in understanding climate and ecosystems.
In general, as latitude increases away from the equator towards the poles, temperatures tend to decrease. This is due to a variety of factors, including the angle of sunlight hitting Earth's surface, the length of daylight hours, and the amount of atmosphere sunlight must pass through.
The amount of reactants in a system directly affects the amount of products formed. In the case of the reaction forming N2O4, increasing the amount of reactants (NO2) will shift the equilibrium towards forming more N2O4. Conversely, decreasing the amount of reactants will shift the equilibrium towards forming more NO2.
The solar radiation that reaches the earths surface from the sun is called INSOLATION