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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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Wien distribution law<br />

Wien distribution law A relation between<br />

the monochromatic emittanceF (erg/sec/wavelength/cm<br />

2 /steradian) of an ideal black body <strong>and</strong><br />

that body’s temperature T :<br />

F∝λ −5 f(Tλ).<br />

Wien’s law See Wien’s displacement law.<br />

wiggle (cosmic string) After cosmological<br />

phase transitions in which cosmic strings are<br />

produced, the strings will trace regions where<br />

the Higgs field departs from the low temperature<br />

vacuum manifold of the theory. These regions<br />

have r<strong>and</strong>om spatial locations <strong>and</strong>, therefore, the<br />

ensuing string has no reason to be straight. The<br />

string will, in general, possess an irregular shape<br />

<strong>and</strong> small scale structures in the form of wiggles<br />

will accumulate all along its length. Further<br />

interactions will make the number of these<br />

small irregularities increase. Universal expansion<br />

does not eliminate these wiggles; hence,<br />

wiggly strings are the most natural outcome during<br />

network evolution.<br />

This structure can be analytically approximated<br />

by an effective equation of state describing<br />

how a distant observer would perceive the<br />

string. The effective energy per unit length Ũ<br />

(larger than the Goto–Nambu energyU, as there<br />

is more string matter in a given segment due to<br />

the wiggles) <strong>and</strong> the effective tension ˜T (smaller<br />

than the tension of a Goto–Nambu string) will<br />

satisfy the relation Ũ ˜T=U 2 .<br />

Furthermore, the space around the wiggly<br />

string is no longer locally flat, <strong>and</strong> thus the string<br />

will behave like a st<strong>and</strong>ard gravitational attractor.<br />

Now particle geodesics in the vicinity of a<br />

wiggly string will be deflected by two mechanisms:<br />

the conical deficit angle deviation (from<br />

far away the string looks pretty straight <strong>and</strong> featureless)<br />

<strong>and</strong> the st<strong>and</strong>ard gravitational attraction.<br />

The relative velocity between two test particles<br />

on different sides of the string will be<br />

δv = 8πGŨvsγs + 4πG<br />

<br />

Ũ−˜T /(vsγs)<br />

where vs is the velocity of the string, γs is the<br />

corresponding Lorentz factor (1 − v 2 s /c2 ) −1/2 ,<br />

<strong>and</strong> G is Newton’s constant. The first of these<br />

© 2001 by CRC Press LLC<br />

516<br />

effects dominates for fast moving strings <strong>and</strong><br />

would lead to the formation of wakes. The second<br />

one is relevant for slow strings <strong>and</strong> could be<br />

at the root of the generation of filamentary distributions<br />

of astrophysical large scale structures.<br />

See cosmic phase transition, cosmic string, cosmic<br />

topological defect, deficit angle (cosmic<br />

string), wake (cosmic string).<br />

Wilson cycle The Atlantic ocean is presently<br />

“opening”, growing wider due to the creation<br />

of new sea flow at the Mid-Atlantic Ridge. It<br />

is expected that in the future, subduction zones<br />

will form on the boundaries of the Atlantic, <strong>and</strong><br />

the ocean will close resulting in a continental<br />

collision between the Americas <strong>and</strong> Europe <strong>and</strong><br />

Africa. This opening <strong>and</strong> closing of the Atlantic<br />

has happened twice in the past <strong>and</strong> is known as<br />

the Wilson cycle, in honor of J. Tuzo Wilson who<br />

first proposed this behavior. The last closing<br />

of the Atlantic Ocean created the Appalachian<br />

Mountains <strong>and</strong> occurred about 200 million years<br />

ago.<br />

wind The general term for moving air, typically<br />

driven by naturally arising pressure gradients<br />

depending on altitude differences, solar<br />

heating, surface temperature, <strong>and</strong> the Coriolis<br />

force due to the Earth’s rotation.<br />

wind chill factor The perceived sensation of<br />

temperature, TWC, in the presence of a wind.<br />

Based on studies of the rate of water freezing<br />

under different conditions.<br />

The following equations can be used to determine<br />

the wind chill factor TWC:<br />

Wind speed V given in mph:<br />

TWC =Ts − ((Ts − T )(.474266<br />

<br />

+ .303 √ <br />

V −.02 ∗ V ))<br />

Wind speed in knots:<br />

TWC =Ts − ((Ts − T )(.474266<br />

<br />

+ .325518 √ <br />

V −.0233 ∗ V ))<br />

Wind speed in m/s:<br />

TWC =Ts − ((Ts − T )(.474266<br />

<br />

+ .4538 √ <br />

V −.045384 ∗ V ))

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