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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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<strong>and</strong> its density 2.8 g cm −3 . Its geometric albedo<br />

is not well determined, <strong>and</strong> it orbits Jupiter (retrograde)<br />

once every 692 Earth days.<br />

Carnot cycle An ideal thermodynamic reversible<br />

cycle over a substance which consists<br />

of the following four processes: 1. isothermal<br />

expansion, in which the substance does work<br />

<strong>and</strong> there is inflow of heat Q2 at a constant temperature<br />

T2; 2. adiabatic expansion, in which<br />

the substance is thermally insulated <strong>and</strong> does<br />

work, there is no heat flow, <strong>and</strong> the temperature<br />

of the substance decreases; 3. isothermal compression,<br />

work is done on the system <strong>and</strong> there<br />

is outflow of heat Q1 at a constant temperature<br />

T1; 4. adiabatic compression, the substance is<br />

thermally insulated, <strong>and</strong> work is done on the<br />

substance, there is no heat flow, temperature of<br />

the substance increases, <strong>and</strong> at the end of this<br />

process the substance returns to its initial state.<br />

By applying the second law of thermodynamics<br />

to the Carnot cycle, one shows that the ratio<br />

of heat inflow <strong>and</strong> heat outflow Q2/Q1 for a<br />

substance undergoing a Carnot cycle depends<br />

only on the temperatures T2 <strong>and</strong> T1 <strong>and</strong> is independent<br />

of the substance. Applying the Carnot<br />

cycle to an ideal gas, one further shows that the<br />

ratio of heat outflow <strong>and</strong> heat inflow is equal<br />

to the ratio of the corresponding temperatures,<br />

i.e., Q1/Q2 = T1/T2. One can then represent<br />

an arbitrary reversible cyclic process by a series<br />

of Carnot cycles <strong>and</strong> show that <br />

rev dQ/T = 0<br />

for any reversible process. This in turn leads<br />

to the definition (up to an arbitrary constant) of<br />

entropy S = <br />

rev<br />

dQ/T as a thermodynamic<br />

function of state. Named after Nicolas Léonard<br />

Sadi Carnot (1796–1832).<br />

Carnot efficiency The ratio between the<br />

work done <strong>and</strong> the amount of heat introduced<br />

into a system going through a Carnot cycle. The<br />

Carnot efficiency is equal to the difference between<br />

the two temperatures of the isothermal<br />

steps of the cycle divided by the higher of the<br />

two temperatures.<br />

Carnot engine An ideal heat engine whose<br />

working substance goes through the Carnot cycle.<br />

A heat engine receives heat at a given temperature,<br />

does work, <strong>and</strong> gives out heat at a lower<br />

temperature. The efficiency of a Carnot engine<br />

© 2001 by CRC Press LLC<br />

Carter–Peter model<br />

or Carnot efficiency is the maximum efficiency<br />

possible for a heat engine working between two<br />

given temperatures.<br />

Carrington longitude A fixed meridian on<br />

the sun as measured from a specified st<strong>and</strong>ard<br />

meridian. Measured from east to west (0 ◦ to<br />

360 ◦ ) along the sun’s equator. Carrington longitude<br />

rotates with the sun <strong>and</strong> is a particularly<br />

useful coordinate when studying long-lived features<br />

on the sun. When combined with a Carrington<br />

rotation number, the Carrington longitude<br />

is commonly used as an alternative to specifying<br />

a time.<br />

Carrington rotation The period of time covering<br />

360 ◦ of Carrington longitude. Used to<br />

provide a temporal reference frame where the<br />

time unit is a solar rotation period. For example,<br />

Carrington rotation 1917 corresponds to the<br />

time period 9 December 1996 to 5 January 1997,<br />

while Carrington rotation 1642 relates to the rotation<br />

between 28 May 1976 <strong>and</strong> 23 June 1976.<br />

Carter–Peter model The dynamics of a superconducting<br />

cosmic string is macroscopically<br />

describable by means of the duality formalism.<br />

This formalism only requires the knowledge of a<br />

Lagrangian function L depending on a state parameter<br />

w, the latter being interpretable as the<br />

squared gradient of a phase φ, namely<br />

w = κ0γ ab ∂aφ∂bφ ,<br />

with κ0 a normalization coefficient, γ ab the inverse<br />

of the induced metric on the string surface,<br />

<strong>and</strong> the superscripts a, b representing coordinates<br />

on the worldsheet. In the Carter–Peter<br />

(1995) model for describing a conducting cosmic<br />

string of the Witten kind, the Lagrangian<br />

function involves two separate mass scales, m<br />

<strong>and</strong> m⋆ say, respectively describing the energy<br />

scale of cosmic string formation <strong>and</strong> that of current<br />

condensation; it takes the form<br />

L =−m 2 − m2⋆ 2 ln<br />

<br />

1 + w<br />

m2 <br />

.<br />

⋆<br />

This model implies the existence of a first order<br />

pole in the current, as is the case in realistic conducting<br />

string models taking into account the<br />

microscopic field structure. The figure shows

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