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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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special relativity, such a vector has zero length<br />

even though its components are non-zero. In<br />

psuedo-Reimannian geometry, an element ℓ of<br />

a linear space with metricg such thatg(ℓ,ℓ) ≡<br />

gabℓ a ℓ b = 0.<br />

numerical cosmology (computational cosmology)<br />

The technique, <strong>and</strong> a collection<br />

of models of the universe obtained by solving<br />

Einstein’s equations numerically. Because<br />

they proceed in terms of discretization, these<br />

models are approximate, but well-formulated<br />

models show a convergence as the discretization<br />

is refined. For reasonable resolution in<br />

3-dimensional simulations, large computers are<br />

required.<br />

numerical model A set of discretized mathematical<br />

equations, solved on a computer, which<br />

represent the behavior of a physical system.<br />

numerical relativity The study <strong>and</strong> solutions<br />

of the differential equations of general relativity<br />

by discretization of the equations <strong>and</strong> the computational<br />

solution of the resulting finite algebraic<br />

problem. In many cases without overall<br />

symmetry, analytic methods fail <strong>and</strong> numerical<br />

relativity is the only method to elucidate <strong>and</strong> underst<strong>and</strong>genericsolutionsforspacetimesingeneral<br />

relativity. Computational simulation has<br />

become a real research tool, for instance, the<br />

critical behavior <strong>and</strong> naked singularity found by<br />

Choptuik. Similarly, the naked singularity that<br />

may exist in some circumstances at the center of<br />

the Lemaître–Tolman cosmological model was<br />

first identified in numerical calculations. Numerical<br />

investigations have amassed considerable<br />

knowledge about problems too complicated<br />

for analytical treatment: collisions of rotating<br />

black holes, emission of gravitational waves<br />

by rotating nonsymmetric bodies or by binary<br />

systems, collapse of a binary system to a single<br />

body, etc. See binary black holes, critical<br />

© 2001 by CRC Press LLC<br />

nutation<br />

phenomena in gravitational collapse, gravitational<br />

wave.<br />

Nusselt number A dimensionless number<br />

quantifying the efficiency of heat transfer in a<br />

convecting system. It is the ratio of total heat<br />

flux to the conductive heat flux. For example,<br />

the conductive heat flux across a uniform layer<br />

of thickness h with differential temperature T<br />

is λT /h. If the total heat flux including convective<br />

heat transfer is q, the Nusselt number in<br />

this case is<br />

q<br />

Nu =<br />

λT /h .<br />

nutation This is a variation of the orientation<br />

(the obliquity) of the Earth’s axis of rotation associated<br />

with the Earth’s forced precession. In<br />

the theory of the rapid rotation of a rigid body,<br />

it is used to imply an analog of the free (i.e., unforced)<br />

precession of a body in the case where<br />

there is also a forced precession, which causes<br />

the body’s axis with the largest principal moment<br />

of inertia to “nod” backwards <strong>and</strong> forwards<br />

even as it is precessing. On Earth, this effect is<br />

known as the Ch<strong>and</strong>ler wobble, <strong>and</strong> the term nutation<br />

may also refer to motions due to the fact<br />

that the Earth is deformable <strong>and</strong> its layers imperfectly<br />

coupled, as well as motions caused by<br />

time variations in the torque acting on the Earth.<br />

This happens because the couple is produced<br />

by the tidal interactions with the moon <strong>and</strong> sun,<br />

which vary because the relative orientations of<br />

the Earth, moon <strong>and</strong> sun change with time in various<br />

different ways. There are nutations at various<br />

periods, the largest nutation being at 18.6<br />

years. Nutation is one of the contributors to the<br />

Milankovich cycles which cause climatic variations.<br />

In the case of the Earth, nutation causes<br />

the obliquity to vary from 21 ◦ to 24 ◦ (the current<br />

value of Earth’s obliquity is 23.5 ◦ ) over a period<br />

of 41,000 years. See precession.<br />

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