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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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Peru current<br />

case). Perturbative solutions are ubiquitous in<br />

astrophysics. Planetary orbits <strong>and</strong> the positions<br />

of planets on the orbits are calculated by such<br />

perturbative methods where the small parameter<br />

is the eccentricity of the orbit. In cosmology, the<br />

most commonly used description of the formation<br />

of galaxies is by solving Einstein’s equations<br />

perturbatively, with the small parameter<br />

being the size of the matter deviation from the<br />

spatially homogeneous background. Perturbative<br />

solutions are often possible where an exact<br />

solution seems prohibitively difficult, but they<br />

have their own difficulties. In applications in<br />

general relativity care must be taken to distinguish<br />

between genuine perturbations <strong>and</strong> spurious<br />

perturbations.<br />

Peru current A cold ocean current running<br />

up the west coast of the South American continent,<br />

feeding into the South Equatorial current.<br />

Petchek reconnection Fast reconnection at<br />

an X-point or in a small localized region. About<br />

three-fifths of the inflowing magnetic energy is<br />

converted into kinetic energy behind the shock<br />

waves, the remaining two-fifths heat the plasma.<br />

WithvA,in being the Alfvén speed in the inflowing<br />

plasma, L being the length scale of the reconnection<br />

region,σ being the conductivity, <strong>and</strong><br />

c being the speed of light, the reconnection rate<br />

Rp can be written as<br />

Rp = π<br />

8 ln<br />

<br />

c<br />

LσvA,in4π<br />

<br />

.<br />

Petchek reconnection varies only weakly with<br />

the conductivityσ <strong>and</strong> is very efficient in mixing<br />

fields <strong>and</strong> plasmas. It probably does not play<br />

a role in magnetospheric plasmas but might be<br />

important in solar flares.<br />

Petchek reconnection is stationary reconnection:<br />

the onset of reconnection does not destroy<br />

the general field configuration. Stationary reconnection<br />

results in an equilibrium between inflowing<br />

mass <strong>and</strong> magnetic flux, magnetic diffusion,<br />

<strong>and</strong> outflowing mass <strong>and</strong> magnetic flux.<br />

Petrovtypes Typesinaclassificationofgravitational<br />

fields according to the algebraic structure<br />

of the Weyl tensor (a tensor algebraically<br />

constructed from the Riemann tensor to be completely<br />

traceless), introduced by Petrov (1966).<br />

© 2001 by CRC Press LLC<br />

358<br />

In general relativity the traces of the Riemann<br />

tensor are pointwise determined by the stressenergy<br />

tensor. The trace-free part, the Weyl tensorCabcd<br />

is symmetric in the skew pairsab <strong>and</strong><br />

cd of indices. There are six independent components<br />

of each skew pair; hence the Weyl tensor<br />

can be viewed as a symmetric 6× 6 matrix.<br />

The eigenvalues of this matrix sum to zero. An<br />

alternate (calculationally simpler) development<br />

can be given in terms of spinors. The eigenvectors<br />

determine null vectors; for the general type<br />

I there are the four different principal spinors<br />

αA ,βA ,γA <strong>and</strong> δA which determine different<br />

principal null directions. For types II, III, <strong>and</strong> N,<br />

respectively, two, three, <strong>and</strong> all four of the principal<br />

directions coincide. Type D arises when<br />

there are two pairs of coincident principal null<br />

directions. When the Weyl curvature vanishes,<br />

the type is O. See principal spinor, Weyl tensor.<br />

Petzold data A widely used data set containing<br />

volume scattering functions for various<br />

waters ranging from very clear to very turbid;<br />

the scattering phase function is highly peaked at<br />

small scattering angles <strong>and</strong> is somewhat independent<br />

of water type.<br />

Pfund series The set of spectral lines in the<br />

extreme infrared region of the hydrogen spec-<br />

trum with frequency obeying<br />

ν = cR<br />

<br />

1/n 2 f − 1/n2 <br />

i<br />

where c is the speed of light, R is the Rydberg<br />

constant, <strong>and</strong> nf <strong>and</strong> ni are the final <strong>and</strong> initial<br />

quantum numbers of the electron orbits, with<br />

nf = 5 defining the frequencies of the spectral<br />

lines in the Pfund series. This frequency is<br />

associated with the energy differences of states<br />

in the hydrogen atom with different quantum<br />

numbers via ν = E/h, where h is Planck’s<br />

constant, <strong>and</strong> where the energy levels of the hydrogen<br />

atom are:<br />

En = hcR/n 2 .<br />

phase In planetary astronomy; variance in<br />

the total amount of the visible disk of the moon,<br />

or of the inner planets, which appears illuminated<br />

at any one time. Phases arise because our<br />

vantage point sometimes allows the unlit side of<br />

,

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