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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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ed line<br />

primary energy source is hydrogen burning (by<br />

the CNO cycle), in a thin shell around an inert<br />

helium core (more massive analogs are called<br />

red supergiants). The star is about 10 times as<br />

bright as it was on the main sequence (see HR diagram),<br />

<strong>and</strong> as the core grows, the star leaves the<br />

main sequence track of the Hertzsprung–Russell<br />

diagram <strong>and</strong> ascends the red giant branch, gaining<br />

in luminosity (on the order of 10 3 L⊙) yet decreasing<br />

in surface temperature (near 3800 K).<br />

The phase lasts about 10% of the main sequence<br />

lifetime <strong>and</strong> is terminated by the ignition of helium<br />

burning. As the star eventually depletes<br />

its core supply of He, hydrogen fusion begins<br />

again in a thin shell around the core. Eventually,<br />

the core becomes inert C <strong>and</strong> O with separate,<br />

concentric shells where He-fusion <strong>and</strong> H fusion<br />

continues. At this stage, the star is considered to<br />

be in the asymptotic giant branch stage of evolution<br />

<strong>and</strong> has achieved a luminosity of 10 4 L⊙<br />

or greater <strong>and</strong> a surface temperature of 1800 to<br />

3500 K. The sun will become a red giant about 5<br />

billion years in the future, increasing the surface<br />

temperature of the Earth to about 900 K, where<br />

some metals melt <strong>and</strong> sulfur boils.<br />

red line A coronal line observed at 6374 Å<br />

resulting from a forbidden transition in highly<br />

ionized iron atoms (Fe X). Important for study<br />

of coronal structures at temperatures of order<br />

1 MK.<br />

redshift A displacement of a spectral line<br />

toward longer wavelengths. This can occur<br />

through the Doppler effect or, as described by<br />

general relativity, from the effects of a star’s<br />

gravitational field or in the light from distant<br />

galaxies. The relative displacement toward<br />

longer wavelength (or equivalently, of lower energy)<br />

of light is measured from spectral features<br />

like emission or absorption of lines <strong>and</strong> is defined<br />

as<br />

z = (λ − λ0) /λ0 ,<br />

where λ0 is the rest wavelength of a spectral feature.<br />

The displacement toward a longer wavelength<br />

is conventionally termed a redshift even if<br />

the photons are not in the visible spectral range.<br />

Galaxies <strong>and</strong> quasars, with the only exceptions<br />

of several galaxies very close to the Milky Way,<br />

invariably show all their spectral lines shifted to<br />

© 2001 by CRC Press LLC<br />

392<br />

the red, with redshift increasing with distance<br />

according to Hubble’s Law. Redshifts up to<br />

z ≈ 5 have been (in 1998) observed for quasars.<br />

Red Spot A feature in Jupiter’s atmosphere,<br />

some 10,000 by 50,000 km in extant. It was<br />

probably first observed by Hooke in 1664, but<br />

a continuous record of observations only goes<br />

back to the end of 1831. Its position is roughly<br />

fixed, with some drift relative to the average position.<br />

Although a number of suggestions have<br />

been forwarded to explain this feature, the most<br />

likely is an atmospheric disturbance, similar to a<br />

hurricane. Scaling arguments indicate that such<br />

a disturbance would be much longer lived on<br />

Jupiter than on Earth.<br />

reduced gravity Reduced gravity g ′ is defined<br />

by g ′ = g(ρ2 − ρ1)/ρ2 where ρ1 <strong>and</strong> ρ2<br />

are the density of the upper <strong>and</strong> lower layer.<br />

reduced gravity model A model treating the<br />

ocean thermocline as an infinitesimally thin interface<br />

separating a warm upper layer <strong>and</strong> an<br />

infinitely deep abyssal. In such a model, the<br />

motion in the abyssal is negligible, <strong>and</strong> the upper<br />

layer motion is described by a set of shallow<br />

water equations with the gravitational acceleration<br />

g replaced by a reduced gravity g ′ =<br />

g(ρ1−ρ2)/ρ2, where ρ1 <strong>and</strong> ρ2 are water density<br />

in the upper layer <strong>and</strong> abyssal, respectively. The<br />

reduced gravity model is particularly useful in<br />

modeling the longest wavelength internal mode<br />

in the tropical oceans where the thermocline is<br />

tight <strong>and</strong> shallow.<br />

reef A ridge of coral or rock which lies at or<br />

near the surface of the sea.<br />

reference frame A st<strong>and</strong>ard of reference<br />

used for physical systems, which is in principle<br />

equivalent to observations by a real observer, via<br />

measurements using the observer’s clock <strong>and</strong> a<br />

local set of Euclidean measurement axes with<br />

a length st<strong>and</strong>ard. The reference frame is expressed<br />

in terms of a set of basis vectors e(a). In<br />

principle another set e ′ (b ′ ) of basis vectors can be<br />

defined by a nonsingular (not necessarily constant)<br />

linear combination<br />

e ′ (b ′ ) = Ab ′ a e(a) .

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