The second theory is really just an elaboration of the first. Because the coronal material is so thin and tenuous, only a tiny portion of all the sound energy in the photosphere needs to bleed up into the corona and be absorbed in order to heat it to the observed temperatures. At least some of this sound makes its way upward into the corona, where dissipative processes covert the audio energy into heat. Thus, if you could stand on the solar surface, not only would it be very hot but it would also be incredibly loud. And just as the roiling water makes noise, so does the convective overturning of the solar surface fill its atmosphere with intense sound waves. They fall into three main categories: In the first, the photosphere can be likened to the bubbling surface of boiling water it is a seething mass of rising and falling columns of hot fluid. That is, only in an ultra-low density medium, such as the corona, are collisions between atoms so infrequent that atomic populations can be maintained in the right kind of energy states to enable the observed emission.Īlthough these high coronal temperatures came as a surprise to early observers, it did not take long for theoretical explanations to surface. Finally, however, it was recognized that the observed color lines arise from what are known as forbidden emissions from very hot atoms (in the range of one million K or more) occurring under highly rarified conditions. For a time people speculated that the coronal emissions were due to coronium, a potential new element found only in the sun. Astronomers recorded red and green line emission from the corona during eclipses as early as 1867, but they could not associate them with any known laboratory spectra. For example, the characteristic brilliant red of the chromosphere seen during solar eclipses was readily traced via so-called Balmer line emissions from hydrogen to material at around 6,000 kelvins. Temperatures in the cooler photosphere (the visible surface of the sun, where we see sunspots) and the overlying chromosphere (where we best see prominences and the expanding magnetic structure in the lower solar atmosphere) had been determined long before that by spectroscopic observations. The fact that the sun's corona is very hot-one million to two million kelvins in "quiet" regions, two million to five million in magnetically strong active regions and higher yet in solar flares-was well established by the 1940s. Victor Pizzo, a physicist at the National Oceanic and Atmospheric Administration's Space Environment Center, explains.
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