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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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pathline<br />

which could have led to the formation of the<br />

patera.<br />

pathline A line drawn through a region of<br />

fluid that indicates the path followed by a particular<br />

particle within the fluid.<br />

P-Cygni profile An emission/absorption line<br />

profile which is the result of an exp<strong>and</strong>ing shell<br />

of gas around a star; the star P Cyg is the prototype.<br />

Its visible spectrum shows lines that have<br />

a wide emission component <strong>and</strong> an absorption<br />

component, with the absorption blue shifted <strong>and</strong><br />

the emission line approximately at the star’s rest<br />

velocity. A simple explanation is that the absorption<br />

arises in material in front of the star<br />

along our line of sight toward the continuum<br />

source. Since this material is exp<strong>and</strong>ing directly<br />

at us, we see the absorption line blue shifted with<br />

respect to the star’s rest frame. The part of the<br />

exp<strong>and</strong>ing gas that is moving at right angles to<br />

our line of sight, on either side of the star, withoutthestellarcontinuuminthebackground,produces<br />

emission lines that are roughly centered at<br />

the star’s rest velocity. The degree in which the<br />

absorption portion is shifted depends on the velocity<br />

of the gas that is producing the lines, <strong>and</strong><br />

thus these lines allow the measurement of wind<br />

velocities in astronomical objects. The winds in<br />

OB stars <strong>and</strong> in cataclysmic variables were originally<br />

detected through the observation of these<br />

line profiles in their spectrum.<br />

Peclet number A dimensionless number<br />

quantifying the importance of advective heat<br />

transfer. It is the ratio of heat flux by advection<br />

to heat flux by conduction. For example, if the<br />

characteristic flow velocity in the direction of<br />

heat conduction isv over a characteristic length<br />

L, the Peclet number is defined asPe=vL/κ,<br />

where κ is the thermal diffusivity. If Pe≫ 1,<br />

heat transfer is mainly advective. If Pe≪ 1,<br />

heat transfer is mainly conductive.<br />

peculiar motion In astronomy, the physical<br />

or angular velocity of a source with reference to<br />

afixedframeofinterest. Forstars, thetransverse<br />

peculiar motion is typically given in seconds of<br />

arc per century. For extragalactic objects, transverse<br />

motion is not measurable, but the radial<br />

© 2001 by CRC Press LLC<br />

354<br />

peculiar motion is measured by means of red<br />

shifts, <strong>and</strong> reported in terms of km/sec.<br />

peculiar velocity See peculiar motion.<br />

peeling property The Weyl tensor (a form<br />

of the curvature tensor) of an asymptotically<br />

flat space-time, when exp<strong>and</strong>ed in power series<br />

of the affine parameter r of outgoing null<br />

geodesics, has the form<br />

Cijkl = Nijkl<br />

r<br />

IIIijkl<br />

+<br />

r2 IIijkl<br />

+<br />

r3 + Iijkl<br />

+O<br />

r4 1<br />

r 5<br />

where the coefficients Nijkl , IIIijkl , etc. are of<br />

the Petrov type indicated by the kernel letter.<br />

In particular, gravitational radiation encoded in<br />

Nijkl has an amplitude falloff ofr −1 . See Petrov<br />

types.<br />

penetrative convection Sinking plumes in<br />

a convectively mixing surface layer (or rising<br />

plumes in a convectively mixing bottom layer)<br />

impinge with their characteristic velocity scale<br />

onto the adjacent stratified fluid. As the plumes<br />

have momentum, they reach a limited penetration<br />

of the depth scale before the plumes stop<br />

due to entrainment <strong>and</strong> buoyancy. For instance,<br />

substantial, convective motions are present in<br />

the upper layer of the sun. At the base of the<br />

convection zone there is a gradual transition to<br />

the stable, radiative interior, the convective penetration<br />

zone. Below it, energy is transported<br />

outwards entirely by radiative diffusion. At the<br />

penetrative convection depth, the gas becomes<br />

suddenly less opaque, becomes unstable, <strong>and</strong><br />

convective transport becomes dominant.<br />

Penman equation (or combination equation)<br />

Evaporation (E) can be estimated by combining<br />

mass-transfer <strong>and</strong> energy-balance approaches in<br />

a theoretically sound <strong>and</strong> dimensionally homogeneous<br />

relation:<br />

E = s (Ta) (K + L) + γKEρwλvua [esat (Ta)] (1 − RH)<br />

<br />

ρwλv s (Ta) + γ <br />

where s(Ta) is the slope of the saturation vapor<br />

pressure vs. air temperature (Ta), K is net shortwave<br />

radiation, L is net longwave radiation, γ is

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