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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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sionally, toward the second or higher diffraction<br />

orders. In this case, a grating is said to be blazed.<br />

diffuse absorption coefficient For downwelling<br />

(upwelling) irradiance: the ratio of the<br />

absorption coefficient to the mean cosine of the<br />

downward (upward) radiance. See absorption<br />

coefficient.<br />

diffuse attenuation coefficient For downwelling<br />

(upwelling) irradiance: the ratio of the<br />

sum of the absorption coefficient <strong>and</strong> the scattering<br />

coefficient to the mean cosine of the downward<br />

(upward) radiance.<br />

diffuse aurora A weak diffuse glow of the<br />

upper atmosphere in the auroral zone, caused<br />

by collisions with the upper atmosphere of electrons<br />

with energies around 1 keV. It is believed<br />

that these electrons leak out from the plasma<br />

sheet of the magnetosphere, where they are<br />

trapped magnetically. The diffuse aurora is not<br />

conspicuous to the eye, but imagers aboard satellites<br />

in space see it as a “ring of fire” around the<br />

magnetic pole. Discovered by ISIS-1 in 1972,<br />

its size, intensity, <strong>and</strong> variations — in particular,<br />

its intensifications <strong>and</strong> motions in substorms —<br />

are important clues to the state of the magnetosphere.<br />

diffuse galactic light The diffuse glow observed<br />

across the Milky Way. A large part of<br />

the brightness of the Milky Way, which is the<br />

disk of our galaxy seen from the inside, can be<br />

resolved into stellar sources. The diffuse galactic<br />

light is a truly diffuse glow which accounts<br />

for the remaining 25% of the luminosity <strong>and</strong>, by<br />

definition, is unresolved even if observed with<br />

large telescopes. The diffuse galactic light is<br />

due to light emitted within our galaxy <strong>and</strong> scattered<br />

by dust grains, <strong>and</strong> it is not to be confused<br />

with light coming from extended sources like<br />

reflection or emission nebulae. The brightness<br />

close to the galactic equator due to diffuse galactic<br />

light is equivalent to 50 stars of 10th magnitude<br />

per square degree; for comparison, the total<br />

star background is 170 10th magnitude stars per<br />

square degree, <strong>and</strong> the zodiacal light 80.<br />

diffuse interstellar b<strong>and</strong>s (DIBs) A series<br />

of interstellar absorption features recorded on<br />

© 2001 by CRC Press LLC<br />

diffusion-convection equation<br />

photographic plates in the early 1900s. They<br />

were labeled “diffuse” because they arise from<br />

electronic transitions in molecules, so they are<br />

broad in comparison to atomic lines. There are<br />

now well over 100 such b<strong>and</strong>s known in the UV,<br />

visible, <strong>and</strong> near IR regions of the spectrum arising<br />

in interstellar clouds. DIBs must be molecular,<br />

given the complexity of the absorption lines.<br />

DIBs are easily seen when observing spectra<br />

of hot, fast rotating stars whose spectrum has a<br />

strong continuum. Even with very high resolution<br />

spectroscopy, the diffuse interstellar b<strong>and</strong>s<br />

continue to show blended structures. DIBs<br />

show considerable scatter in strength vs. the<br />

amount of stellar reddening suggesting inhomogeneous<br />

variation of chemistry <strong>and</strong> dust-to-gas<br />

ratio. This may arise because the molecule(s) in<br />

the volume may be able to add hydrogen to the<br />

molecular structure in certain circumstances, as<br />

is known for some carbon compounds. Identifying<br />

the carriers of these absorptions has become<br />

perhaps the classic astrophysical spectroscopic<br />

problem of the 20th century, <strong>and</strong> numerous<br />

molecules have been put forth as the<br />

source of these features. Recently most attention<br />

has focused on carbon rich molecules such<br />

as fullerenes <strong>and</strong> polycyclic aromatic hydrocarbons.<br />

diffuse scattering coefficient for downwelling<br />

(upwelling) irradiance The ratio of the scattering<br />

coefficient to the mean cosine of the<br />

downward (upward) radiance.<br />

diffusion The gradual mixing of a quantity<br />

(commonly a pollutant) into a fluid by r<strong>and</strong>om<br />

molecular motions <strong>and</strong> turbulence.<br />

diffusion-convection equation Transport<br />

equation for energetic charged particles in interplanetary<br />

space considering the effects of spatial<br />

diffusion <strong>and</strong> convection of particles with the solar<br />

wind. The transport equation can be derived<br />

from the equation of continuity by supplementing<br />

the streaming with the convective streaming<br />

vf , yielding<br />

∂f<br />

∂t +∇·(v sowif ) −∇·(D∇f)= 0<br />

with f being the phase space density, D the (spatial)<br />

diffusion coefficient, <strong>and</strong> v sowi the solar

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