Description
Transcript: The solar constant is the amount of Sun’s radiation that reaches the Earth. Assuming the atmosphere to be perfectly transparent, 1,370 joules reach every square meter of the Earth surface every second. Variations in the solar constant are subtle, only about 0.1 percent per year. However, they can be larger in percentage terms at regions beyond the visible spectrum in ultraviolet rays or x-rays. In particular, in the ultraviolet ozone in the upper atmosphere can affect the amount of radiation that reaches the Earth surface. Small changes in the energy budget from the Sun’s radiation can affect the weather and climate of the Earth in serious and systematic ways. Thirteen hundred and seventy watts is a lot of energy; the average family home intercepts 50 to 100 kilowatts. Even accounting for a relatively low efficiency of a solar cell, and only half to a third of the time of a twenty-four hour day when the Sun is out, solar energy is clearly an abundant energy source.
Transcript: Since light has a finite speed, three hundred thousand kilometers per second, there’s an inevitable consequence called light travel time. In terrestrial environments light essentially travels instantly or appears to travel fast. The finite speed of light, three hundred thousand...
Published 07/24/11
Transcript: Some stars in the sky, somewhat hotter than the Sun with temperatures of 5 thousand to 10 thousand Kelvin, have very low luminosities in the range of one-hundredth to one-thousandth the Sun’s luminosity. Application of the Stephan-Boltzmann Law shows that they must be physically...
Published 07/24/11
Transcript: Certain rare stars in the sky with either red or blue colors are extremely luminous, up to a million times the luminosity of the Sun. Application of the Stephan-Boltzmann Law shows that their sizes must be in the range of ten to a thousand times the size of the Sun. These...
Published 07/24/11