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Albedo refers to the reflectivity of a surface. Surfaces with high albedo reflect more solar radiation back into space, which can cool the Earth's surface and lower temperatures. Surfaces with low albedo absorb more solar radiation, leading to warming of the Earth's surface.

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How does volcanic ash in Earth and atmosphere affect solar radiation?

Volcanic ash can reflect and scatter sunlight back into space, leading to a cooling effect on the Earth's surface. This can temporarily reduce solar radiation reaching the Earth's surface, causing a drop in temperatures in the affected area. However, volcanic ash can also absorb radiation and contribute to warming the atmosphere in the long term.


Why does solar radiation vary?

Solar radiation varies due to factors such as time of day, season, latitude, cloud cover, and atmospheric conditions. These variables affect the amount of sunlight reaching Earth's surface at any given location and time. Additionally, factors like Earth's tilt and orbital changes also contribute to variations in solar radiation.


How does the angle of light affect the temperature of a surface?

The amount of energy reaching a given area from a source of radiant energy is dependent on the angle of incidence of the energy. Radiation that contacts a surface at an angle of 60° from the normal has half as much energy per unit of surface area as radiation that is parallel to the normal, radiation that reaches the surface at 70.53° from the normal has one third the energy per unit of area, radiation at 75.52° from the normal has one fourth as much energy, and so on. Therefore, if light is contacting a surface that absorbs some of it and converts it to heat, the angle of incidence of the light will affect the temperature. Such is the reason why winters are colder than summers.


Why does earth receive a different amount of radiation?

Earth receives varying amounts of radiation due to its tilt on its axis and elliptical orbit around the sun. This results in different angles and distances between Earth and the sun throughout the year, causing variations in the amount of solar radiation reaching different regions. Additionally, factors like clouds, atmosphere, and surface conditions can also affect how much radiation is absorbed or reflected.


Reflection and absorption by the atmosphere prevent some?

The sun's total energy package. There are about 1355 watts hitting each meter of atmosphere. Roughly 375 watts reach our planet. This amount varies greatly on weather conditions. Water vapor (clouds) provide most of the feedback loop.It is believed that man's contribution of 0.28% of the total green houses gases may have some affect on the current warming. Science suggests (and data supports) that this may well not be the issue. While man has been steadily increasing his contribution of CO2 to the atmosphere (now reaching 6% of total CO2 production and 0.28% of total GHG) we are seeing a steady decline in temperature worldwide. The crest seems to have been in 1998. The start point of this warming was about 6000 years ago. Of the 11 degrees (C) of warming we have verified, only 0.2 has occurred since man started using fuel.Reflection and absorption by the atmosphere prevent some solar radiation from reaching the earth's surface.

Related Questions

How does volcanic ash in Earths atomosphere affect solar radiation?

It blocks (some of) it from reaching the surface of the Earth.


How does volcanic ash in Earth and atmosphere affect solar radiation?

Volcanic ash can reflect and scatter sunlight back into space, leading to a cooling effect on the Earth's surface. This can temporarily reduce solar radiation reaching the Earth's surface, causing a drop in temperatures in the affected area. However, volcanic ash can also absorb radiation and contribute to warming the atmosphere in the long term.


What factors affect the amount of radiation a surface absorbs?

Factors that affect the amount of radiation a surface absorbs include the type of material, color, texture, and angle of the surface. Darker colors tend to absorb more radiation than lighter colors, and rough surfaces absorb more radiation than smooth surfaces. The angle of the surface plays a role in how much direct sunlight it receives.


What factors affect heat loss by infrared radiation?

Factors that affect heat loss by infrared radiation include surface temperature (warmer surfaces emit more radiation), emissivity (a measure of how efficiently a surface emits radiation), surface area, and the temperature difference between the object and its surroundings. Additionally, factors such as the presence of insulation or reflective surfaces can also impact heat loss via radiation.


How would a decrease of ozone in the stratosphere affect the radiation received at earth surface?

A decrease in ozone in the stratosphere would lead to more harmful ultraviolet (UV) radiation reaching the Earth's surface. This can increase the risk of skin cancer, damage marine life, and harm terrestrial plant growth. It can also impact climate patterns and lead to a warmer atmosphere.


Why is damaged to the ozone layer cause of concerned?

The ozone layer stops harmful radiation from reaching the Earth's surface. Depletion of the ozone layer increases the risk of skin cancer. It may also affect the ecosystem in unpredictable ways.


Why does solar radiation vary?

Solar radiation varies due to factors such as time of day, season, latitude, cloud cover, and atmospheric conditions. These variables affect the amount of sunlight reaching Earth's surface at any given location and time. Additionally, factors like Earth's tilt and orbital changes also contribute to variations in solar radiation.


How do solar flares and sunspots affect the earth climate?

Solar flares release bursts of energy and radiation that can disrupt Earth's magnetic field and cause geomagnetic storms. Sunspots are cooler areas on the sun's surface that can affect solar radiation reaching Earth. Both solar flares and sunspots can influence the Earth's climate by affecting the amount of solar radiation received, potentially leading to changes in weather patterns and atmospheric processes.


How Do Sunspots Affect Climate?

Sunspots are darker, cooler regions on the Sun's surface associated with strong magnetic fields. Changes in sunspot activity can impact the amount of solar radiation reaching Earth, which in turn can affect our climate. Higher sunspot activity can lead to increased solar radiation, potentially contributing to warming of the Earth's surface, while lower activity can have the opposite effect.


How does the angle of light affect the temperature of a surface?

The amount of energy reaching a given area from a source of radiant energy is dependent on the angle of incidence of the energy. Radiation that contacts a surface at an angle of 60° from the normal has half as much energy per unit of surface area as radiation that is parallel to the normal, radiation that reaches the surface at 70.53° from the normal has one third the energy per unit of area, radiation at 75.52° from the normal has one fourth as much energy, and so on. Therefore, if light is contacting a surface that absorbs some of it and converts it to heat, the angle of incidence of the light will affect the temperature. Such is the reason why winters are colder than summers.


How does the sunbeam through clouds affect the Earth's climate and weather patterns?

The sunbeam through clouds can impact Earth's climate and weather patterns by influencing the amount of solar radiation reaching the surface. This can affect temperature, cloud formation, and atmospheric circulation, leading to changes in weather conditions such as temperature fluctuations, precipitation patterns, and wind patterns.


Why does earth receive a different amount of radiation?

Earth receives varying amounts of radiation due to its tilt on its axis and elliptical orbit around the sun. This results in different angles and distances between Earth and the sun throughout the year, causing variations in the amount of solar radiation reaching different regions. Additionally, factors like clouds, atmosphere, and surface conditions can also affect how much radiation is absorbed or reflected.