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The light energy is absorbed and dispersed after it hits the radiometer.
The principle of how energy is dispersed has nothing to do with the angle. It's the same, whether the angle is small or large.The reason that at low angles you get less energy is that the same amount of sunlight - the same cross-section, for example, a square meter of sunlight - is distributed over a larger area.
The measure of an objects kinetic energy is Temperature
Heats a measure of energy. Temperature is a measure of hotness
what is the term for the measure of thermal energy in the atmosphere
Cal means calories. It is a measure of the amount of energy that a particular food has. So, if we eat that particular food, then we will obtain that amount of energy.
energy
Kinetic energy is used to overcome friction and is dispersed as heat; some energy is converted to sound.
The amount of energy that you can get from that food. We get our energy from calories. And when we burn energy, we burn calories. So, we measure calories to see how much energy we will get from that particular food. This tells us how much of that food we should eat, compared to how much energy we expend.
Why is energy difficult to measure?
The light energy is absorbed and dispersed after it hits the radiometer.
Radiation damping in relation to dispersion just means that radiation will loose its strength when it is dispersed in a liquid cooling bath which is used as a safety measure in nuclear energy production.
A measure of heat energy can be done easily using a thermometer. This will measure the amount of thermal energy transferred.
The principle of how energy is dispersed has nothing to do with the angle. It's the same, whether the angle is small or large.The reason that at low angles you get less energy is that the same amount of sunlight - the same cross-section, for example, a square meter of sunlight - is distributed over a larger area.
Heats a measure of energy. Temperature is a measure of hotness
The measure of an objects kinetic energy is Temperature
what is the term for the measure of thermal energy in the atmosphere