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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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B<br />

Baade–Wesselink method A method of determining<br />

the distance to pulsating stars, which<br />

can also be observed spectroscopically. One estimates<br />

the surface temperature <strong>and</strong> hence the<br />

surface brightness from the color index (B −V<br />

color), based on simultaneous measurements of<br />

the blue <strong>and</strong> visual magnitude at bright <strong>and</strong> dim<br />

epochs in the star’s pulsation. One computes the<br />

square root of the ratio of the observed flux to the<br />

surfacebrightnessforeachoftheseepochs. This<br />

is an estimate of the angular diameter of the star.<br />

Spectroscopy yields the surface velocity of the<br />

star (via blue <strong>and</strong> red shifting of spectral lines),<br />

which leads to a determination of the total difference<br />

in radius of the star between the observations.<br />

The combination of these observations<br />

allows a determination of the physical size of<br />

the star, <strong>and</strong> thus of its absolute magnitude <strong>and</strong><br />

distance. The method has also been applied to<br />

the exp<strong>and</strong>ing envelope of type II supernovae.<br />

Babinet point One of three points on the<br />

sky in a vertical line through the sun at which<br />

the polarization of skylight vanishes. Usually<br />

located at about 20 ◦ above the sun. See Arago<br />

point, Brewster point.<br />

baby universe A theory regarding matter that<br />

falls into a black hole that subsequently evaporates.<br />

It states that this matter may go into a<br />

separate space-time, which could detach from<br />

the universe at one location <strong>and</strong> reattach elsewhere.<br />

This may not be particularly useful for<br />

space travel, but the existence of baby universes<br />

introduces a r<strong>and</strong>omness so that even a complete<br />

unifiedtheorywouldbeabletopredictmuchless<br />

than expected. However, averaging over ensembles<br />

of universes containing baby universes may<br />

lead to predictions via expected values of certain<br />

measured quantities, such as the cosmological<br />

constant.<br />

backarc spreading In some subduction<br />

zones (ocean trenches) an area of sea-floor<br />

© 2001 by CRC Press LLC<br />

c<br />

Baily’s beads<br />

spreading occurs behind the subduction zone,<br />

thus creating new oceanic crust. The Sea of<br />

Japan is an example. The foundering oceanic<br />

plate pulls away from the adjacent continental<br />

margin, <strong>and</strong> backarc spreading fills the gap.<br />

back scattering Scattering through angles<br />

greater than 90 ◦ .<br />

backscattering coefficient The integral over<br />

the hemisphere of backward directions of the<br />

volume scattering function.<br />

backscattering fraction The ratio of the<br />

backscattering coefficient to the scattering coefficient.<br />

backshore The relatively flat portion of a<br />

beach profile which lies between the steeper<br />

beachface <strong>and</strong> the dunes, cliffs, or structures<br />

behind the beach. Subaerial during non-storm<br />

conditions.<br />

Backus effect A particular type of nonuniqueness<br />

that can occur in the inversion of geomagnetic<br />

data on a spherical surface, where instead<br />

of knowing the full vector magnetic field<br />

only the magnitude of the field B is known <strong>and</strong><br />

not its orientation. Historically, early satellite<br />

measurements from platforms such as the PO-<br />

GOs are of this form, as it was difficult to obtain<br />

high quality measurements of satellite orientation.<br />

The effect occurs even if there is perfect<br />

knowledge of B on a spherical surface but can<br />

be alleviated by knowledge ofB in a shell or by<br />

knowledge of the position of the magnetic equator.<br />

The source of the error is the existence of<br />

magnetic fields that are perpendicular to Earthlike<br />

fields everywhere on a spherical surface,<br />

<strong>and</strong> which, therefore, can be added or subtracted<br />

from the Earth’s field without changing B. As<br />

the Earth’s field is predominantly axial dipolar,<br />

the error terms associated by the Backus effect<br />

have strong sectoral variation in a b<strong>and</strong> around<br />

the equator. See nonuniqueness.<br />

Baily’s beads A phenomenon appearing<br />

at the onset <strong>and</strong> at the conclusion of a solar<br />

eclipse, in which the photosphere is almost totally<br />

eclipsed, except for a few locations on the<br />

limb of the moon, which allow view of the pho

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