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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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inferior conjunction<br />

the figure) in the inertial subrange is given by<br />

Kolmogorov’s “k −5/3 ”law<br />

(k) =Aɛ 2/3 k −5/3<br />

where k is the wavenumber <strong>and</strong> ɛ is the dissipation<br />

rate of turbulent kinetic energy. The parameter<br />

A is a universal constant that is valid for<br />

all turbulent flows, <strong>and</strong> A 0.3 for the streamwise<br />

components of (k) <strong>and</strong> A 1.5 for the<br />

cross-stream components.<br />

normalized turbulence spectrum<br />

log Φ<br />

1<br />

2<br />

3<br />

4<br />

5<br />

0<br />

5<br />

k 5/3<br />

inertial subrange<br />

equilibrium range<br />

4 3 2 1<br />

log (k/k )<br />

η<br />

dissipation<br />

range<br />

Typical wavenumber spectrum observed in the ocean<br />

plotted against the Kolmogorov wavenumber.<br />

inferior conjunction See conjunction.<br />

inferior mirage A spurious image of an object<br />

formed below its true position by atmospheric<br />

refraction when temperature decreases<br />

strongly with height. See superior mirage.<br />

infinitesimal canonical transformation In<br />

classical mechanics, a canonical transformation<br />

in which the change between old canonical variables<br />

{q k ,pl} with Hamiltonian H(q k ,pl ,t)<br />

<strong>and</strong> new canonical variables {Q k ,Pm} with<br />

Hamiltonian K(Q m ,Pn,t)is infinitesimal, so<br />

that squares of differences can be neglected.<br />

A basic form of canonical transformation postulates<br />

a generating function F(q k ,Pl,t) <strong>and</strong><br />

© 2001 by CRC Press LLC<br />

242<br />

0<br />

then solves<br />

pk = ∂F<br />

∂qk Q l = ∂F<br />

∂Pl<br />

K = ∂F<br />

∂t +H<br />

Notice that F =qkPk (summed on k) generates<br />

the identity transformation: Qk =qk ,Pl=pl<br />

via the above equation.<br />

The generator for an infinitesimal canonical<br />

transformation is then:<br />

F=q k <br />

Pk+ɛG q k <br />

,Pm,t<br />

where ɛ is a small parameter (so that ɛ2 terms<br />

are ignored). From the previous equations,<br />

pk = Pk +ɛ ∂G<br />

∂qk Q l = q l +ɛ ∂G<br />

.<br />

∂Pl<br />

The terms on the right involve derivatives of G,<br />

which are functions of qk ,Pl, <strong>and</strong> t. However,<br />

because of the small parameter ɛ,G(qk ,Pl,t)<br />

differs only at first order in ɛ from G(qk ,pl,t)<br />

(the same function, evaluated at a slightly different<br />

argument). Hence we can write, to first<br />

order in ɛ,<br />

Pk =pk −ɛ ∂<br />

∂q k<br />

<br />

G q l <br />

,pn,t .<br />

This is an infinitesimal canonical transformation,<br />

<strong>and</strong> G is the generator of the infinitesimal<br />

canonical transformation. Compared to the<br />

general form, it has the great advantage of being<br />

explicit. A full nonlinear transformation<br />

can be carried out by integrating infinitesimal<br />

transformations. See canonical transformation,<br />

Hamilton–Jacobi Theory.<br />

inflation In cosmology, a period of rapid<br />

universal expansion driven by a matter source<br />

whose energy density falls off slowly in time or<br />

not at all. The simplest example appears in the<br />

behavior of the scale a(t) for an isotropic, homogeneous<br />

universe (a cosmology modeled by<br />

a Robertson–Walker cosmology):<br />

3<br />

˙a<br />

a<br />

2<br />

= 8πGρ<br />

c 2<br />

k<br />

− + <br />

a2

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