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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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layer, which can be seen as a small reddish ring<br />

during a total eclipse. Its name, chromosphere,<br />

means colored sphere <strong>and</strong> stems from this reddish<br />

color, which results from emission in the<br />

Hα line of hydrogen. The chromosphere shows<br />

highly variable structures, giving it the nickname<br />

“burning prairie”. In the chromosphere,<br />

the density decreases by about three orders of<br />

magnitude while the temperature stays roughly<br />

constant. The next layer is the transition region,<br />

where the temperature increases by a factor of<br />

about 200, the density decreases by one order of<br />

magnitude <strong>and</strong> the collision time increases by<br />

more than 4 orders of magnitude — over a thin<br />

layer which is only a few hundred kilometers<br />

thick. The outer solar atmosphere, the corona,<br />

fills the entire heliosphere as solar wind. Aside<br />

from just above the transition region, temperature<br />

<strong>and</strong> density are roughly constant. The<br />

corona can be seen as a broad structured ring<br />

around the occulting disk of the moon during<br />

a total eclipse. These structures, in particular<br />

arcs, rays, or helmet streamers, reflect the magnetic<br />

field pattern in the corona, allowing the<br />

distinction between open <strong>and</strong> closed magnetic<br />

fields. Despite its high temperature, the corona<br />

does not radiate like a black body because its<br />

density is too low. Instead, the radiation is photospheric<br />

light scattered by the electrons. Thus,<br />

the light intensity also reflects the electron density<br />

in the corona. See chromosphere, corona,<br />

photosphere, transition region.<br />

solar B-angle The angle, relative to the center<br />

of the solar disk, between the north pole of<br />

the sun <strong>and</strong> the zenith, measured from north to<br />

west in degrees.<br />

solar constant The rate at which solar radiant<br />

energy at all wavelengths is received outside<br />

the atmosphere on a surface normal to the incident<br />

radiation, at the Earth’s mean distance from<br />

the sun. The amount of variability is still a subject<br />

of debate, but is certainly very small (less<br />

than 1%) apart from the long-term development<br />

in the history of the sun. The symbol of solar<br />

constant is S. Unit of S is Wm −2 or cal · cm −2 ·<br />

min −1 . Since 99.9% of the solar radiation energy<br />

is within the wave b<strong>and</strong> 0.2 to 10.0 µm,<br />

the measurment of solar constant does not need<br />

to involve a wide wave b<strong>and</strong>. In 1981, World<br />

© 2001 by CRC Press LLC<br />

solar dynamo<br />

Meteorological Organization suggested the use<br />

of S = 1367 ± 7 W/m 2 as the solar constant<br />

value, equivalent to 1.945 cal · cm −2 · min −1 .<br />

solar cycle The solar cycle, the 11-year periodicity<br />

in the occurrence of sunspots, first was<br />

recognized in 1843 by H. Schwabe. Its features<br />

can best be seen in a butterfly diagram: at the<br />

beginning of a solar cycle a few sunspots start to<br />

appear at latitudes around 30 ◦ . These spots are<br />

relatively stable <strong>and</strong> can often be observed over<br />

a couple of solar rotations. The spots move toward<br />

the equator while at their original latitudes<br />

new spots appear. The number of sunspots increases<br />

until solar maximum. Afterwards, only<br />

a few new sunspots emerge while the spots at<br />

lower latitude dissolve. The total number of<br />

sunspots decreases until just after solar minimum<br />

when new sunspots begin to emerge at<br />

higher latitudes. The average duration of such a<br />

cycle is 11 years with variations between 7 <strong>and</strong><br />

15 years. Successive cycles have opposite magnetic<br />

polarity, so that the full cycle is actually<br />

22 years. The maximum number of sunspots<br />

also differs from cycle to cycle by up to a factor<br />

of 4. Occasionally, the solar cycle, <strong>and</strong> with it<br />

the sunspots, can disappear nearly completely<br />

over time scales of some 10 years. The best<br />

documented case of such “missing sunspots” is<br />

the Maunder Minimum. Solar Cycle #23 began<br />

in October 1996. See butterfly diagram, Hale’s<br />

polarity law, Maunder Minimum, Spoerer’s law,<br />

sunspot, sunspot cycle.<br />

solar day The length of time from noon to<br />

noon; It varies from the mean solar day (24 h)<br />

as described by the equation of time.<br />

solar disk The visible surface of the sun projected<br />

against the sky.<br />

solar dynamo The process by which the<br />

interaction between magnetic field <strong>and</strong> plasma<br />

deep in the solar interior is thought to occur. The<br />

dynamo process results in the intensification of<br />

magnetic fields via the induction of plasmas trying<br />

to cross field lines. The action of the solar<br />

dynamo is thought to explain the existence of<br />

the solar cycle, the butterfly diagram, Spörer’s<br />

Law, <strong>and</strong> the reversal of the sun’s polar fields<br />

near sunspot maximum.<br />

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