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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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Law-of-the-Wall Scaling Relations<br />

Length LLs ∼ z<br />

Time τLs ∼ zu ∗ −1<br />

Velocity wLs ∼ u ∗<br />

Dissipation of turbulent kinetic energy εLs ∼ u∗ 3 (κz) −1<br />

Temperature (fluctuations) Ls ∼ Fth/(ρcpu ∗ )<br />

found by Friedmann (see Friedmann–Lemaître<br />

cosmological models) <strong>and</strong> several contributions<br />

to relativistic cosmology based on these models.<br />

His other achievements include the theory<br />

of “primaeval atom” — an overall vision<br />

of the origin <strong>and</strong> evolution of the universe (now<br />

replaced by the more detailed <strong>and</strong> better confirmed<br />

observationally Big Bang theory), several<br />

papers on physics of cosmic rays (which he<br />

interpreted as remnants of what is now called the<br />

Big Bang), mathematical physics, celestial mechanics,<br />

<strong>and</strong> automated computing (even before<br />

electronic computers were invented).<br />

Lemaître–Tolman cosmological model Inhomogeneous<br />

cosmological model first described<br />

in 1933 by G. Lemaître, but now commonly<br />

called the Tolman model. See Tolman<br />

model.<br />

lengthofday Thelengthofday hasdecreased<br />

with geological time. The rotational period of<br />

the Earth has slowed due to tidal dissipation.<br />

lens A transparent solid through which light<br />

can pass, <strong>and</strong> which has engineered-in propertiestodeflectorfocusthelight.<br />

Seegravitational<br />

lens.<br />

Lense–Thirring precession The dragging of<br />

space <strong>and</strong> time by a rotating mass, most evident<br />

in cases of rapidly rotating compact objects,<br />

such as Kerr black holes. Predicted using<br />

the equations of general relativity by J. Lense<br />

<strong>and</strong> H. Thirring in 1918, the effect has been<br />

presumably detected by the extremely tiny effects<br />

on satellites orbiting Earth, <strong>and</strong> around<br />

distant, rotating objects with very intense gravitational<br />

field, such as neutron stars <strong>and</strong> black<br />

holes. The Lense–Thirring effect gives rise to<br />

a precessional motion if an object is not orbiting<br />

in the equatorial plane of the massive body.<br />

© 2001 by CRC Press LLC<br />

Lewis number<br />

In the vicinity of a rotating black hole, within<br />

the ergosphere, the dragging is strong enough to<br />

force all matter to orbit in the equatorial plane<br />

of the black hole. See accretion disk, Kerr black<br />

hole.<br />

lepton A fundamental spin 1/2 fermion that<br />

does not participate in strong interactions. The<br />

electrically charged leptons are the electron, the<br />

muon, the tau, <strong>and</strong> their antiparticles. Electrically<br />

neutral leptons are called neutrinos <strong>and</strong><br />

have very small (or zero) mass. The neutrinos<br />

are observed to have only one helicity state<br />

(left-h<strong>and</strong>ed). Their antiparticles have positive<br />

helicity.<br />

leveling (survey) A geodetic measurement<br />

to obtain height difference between two points.<br />

The height difference between the two points<br />

can be obtained by erecting leveling rods at two<br />

distant points from several to tens of several<br />

meters, <strong>and</strong> then by reading scales of the leveling<br />

rods using a level that is placed horizontally<br />

at the intermediate distance between the<br />

two points. Repeating this operation, height difference<br />

between substantially distant two points<br />

can be measured. Height above the sea at a<br />

point can be obtained from control points whose<br />

height above the sea has already been determined<br />

(bench marks) or from height difference<br />

between the point <strong>and</strong> tide gage stations. This<br />

kind of leveling is referred to as direct leveling,<br />

whereas trigonometric leveling <strong>and</strong> barometric<br />

leveling are called indirect leveling.<br />

Lewis number The non-dimensional ratio<br />

LC = DC/DT, where DC is molecular diffusivity<br />

of substance C <strong>and</strong> DT is molecular diffusivity<br />

of heat, expresses the ratio of the rate of<br />

transfer of molecules of C to that of heat. LC<br />

in water is strongly temperature-dependent <strong>and</strong><br />

of the order of 0.01. The turbulent Lewis num-<br />

277

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