29.03.2013 Views

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

interplanetary dust particles (IDPs)<br />

namic temperature to be determined from operational<br />

measurements.<br />

interplanetary dust particles (IDPs) The<br />

small debris that exists between the planets.<br />

Most of this material comes from comets <strong>and</strong><br />

from collisions between asteroids. Study of interplanetary<br />

dust particles provides information<br />

about the primitive material out of which the solar<br />

system formed, material which has not been<br />

subsequently processed by heat, pressure, <strong>and</strong><br />

chemical reactions as has happened on the larger<br />

bodies of the solar system. Sunlight reflecting<br />

off the IDPs gives rise to the zodiacal light <strong>and</strong><br />

gegenschein.<br />

interplanetary magnetic field See heliospheric<br />

magnetic field.<br />

interplanetary magnetic sector A contiguous<br />

region observed in interplanetary space,<br />

usually near Earth, where for locally observed<br />

magnetic field lines, the ends anchored on the<br />

sun have all the same polarity. If those ends<br />

are directed towards the sun, the region is a “towards<br />

sector”; if away from it, it is an “away<br />

sector”. Sector structure is caused by the waviness<br />

of the heliospheric current sheet (HCS) <strong>and</strong><br />

the regions above the sun’s poles <strong>and</strong> away from<br />

the HCS do not experience sector variations as<br />

the sun rotates.<br />

Since the Earth’s orbit is inclined to the solar<br />

magnetic equator, near sunspot minimum, when<br />

the waviness of the HCS is small, the Earth generally<br />

samples two different sectors. At times<br />

of greater solar activity, when the solar magnetic<br />

field is more complex, the HCS becomes<br />

rather wavy, <strong>and</strong> the Earth can cross 4, 6, or even<br />

8 sectors per solar rotation.<br />

interplanetary propagation The propagation<br />

of energetic charged particles through the<br />

interplanetary medium is influenced by the following<br />

processes:<br />

(a) pitch-angle scattering of particles at the<br />

solar wind turbulence is a stochastic process, described<br />

by the pitch-angle diffusion coefficient<br />

κ(µ) which depends on pitch-angle µ, particle<br />

rigidity, level of interplanetary turbulence, <strong>and</strong><br />

location. In addition, pitch-angle diffusion coefficients<br />

might be different for electrons <strong>and</strong><br />

© 2001 by CRC Press LLC<br />

248<br />

nuclei of the same rigidity. Pitch angle scattering<br />

is a stochastic process. See pitch angle<br />

diffusion, quasi-linear theory, slab model.<br />

(b) focusing in the diverging interplanetary<br />

magnetic field is a systematic process decreasing<br />

the particle’s pitch angle as it propagates<br />

outward. See focusing.<br />

(c) field-parallel propagation of the particle.<br />

See focused transport equation.<br />

(d)convectionofparticleswiththesolarwind<br />

leads, in particular for particles with speeds in<br />

the order of the solar wind speed, to a more efficient<br />

propagation outwards rather than inwards.<br />

See convection.<br />

(e) adiabatic deceleration leads to a cooling<br />

of the cosmic ray gas as it exp<strong>and</strong>s with the exp<strong>and</strong>ing<br />

solar wind that is a transport in momentum.<br />

See adiabatic deceleration. The transport<br />

equation then reads<br />

streaming:<br />

convection:<br />

+ ∂<br />

∂z<br />

focusing:<br />

+ ∂<br />

<br />

v E ′<br />

∂µ 2ζ E<br />

∂F(µ,s,p,t)<br />

∂t<br />

<br />

1 − µ<br />

+ ∂<br />

∂z µvF<br />

2 v2<br />

c2 differential convection:<br />

− ∂<br />

∂µ vsowi<br />

scattering:<br />

deceleration:<br />

<br />

vsowisecψF<br />

+ µvsowi<br />

v secψ<br />

<br />

· (1 − µ 2 )F<br />

<br />

cos ψ d<br />

d rsecψ<br />

− ∂ κ ∂ E<br />

∂µ 2 ∂µ<br />

′<br />

E F<br />

− ∂<br />

∂p pvsowi·<br />

<br />

secψ<br />

·<br />

2ζ (1 − µ2 ) + cos ψ d<br />

source:<br />

= Q(µ,s,t,s,v)<br />

<br />

· µ(1 − µ 2 )F<br />

dr secψµ2<br />

<br />

F

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!