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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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energy for stars as early as 1925 by Sir Arthur<br />

Eddington <strong>and</strong> Hans Bethe <strong>and</strong> others. The interaction<br />

between two protons or a proton <strong>and</strong><br />

a heavier nucleus is a quantum mechanical process<br />

in which barrier penetration must occur. As<br />

a result, hydrogen burning occurs at a temperature<br />

of 10 to 20 million K in stars of low to<br />

high mass (0.085 to 100 solar masses). Lower<br />

mass configurations do not reach this temperature<br />

range, derive little or no energy from hydrogen<br />

burning, <strong>and</strong> are called brown dwarfs. See<br />

brown dwarf, CNO cycle, main sequence star,<br />

proton-proton chain, red giant.<br />

hydrograph A plot showing discharge vs.<br />

time. Commonly used to illustrate flood events<br />

on rivers or creeks.<br />

hydrographic survey A term often used synonymously<br />

with bathymetric survey. A survey<br />

of the geometry of the seafloor. Typically involves<br />

one system for establishment of horizontal<br />

position <strong>and</strong> another for vertical position or<br />

water depth. Traditionally performed from a<br />

boat, but amphibious vehicles, sleds, <strong>and</strong> helicopters<br />

have also been used.<br />

hydrologic equation A water balance equation<br />

often used in catchment hydrology based<br />

on the law of mass conservation that states that<br />

basin outputs are related to basin inputs plus or<br />

minus changes in storage, <strong>and</strong> written in simplified<br />

form as Q=P−ET ±S, where Q<br />

is surface water runoff at the basin outlet, P is<br />

precipitation input to the basin, ET are evapotranspiration<br />

losses of water from the basin, <strong>and</strong><br />

S is the change in storage of water in the basin.<br />

hydromagnetic Pertaining to the macroscopic<br />

behavior of a magnetized electrically<br />

conducting fluid or plasma. Hydromagnetic<br />

phenomena are generally associated with large<br />

length scales compared with the Larmor radii<br />

<strong>and</strong> long time scales compared with the Larmor<br />

periods of the particles that comprise the<br />

fluid. Theoretical descriptions of such phenomena<br />

may be based on magnetohydrodynamics<br />

or kinetic theory. See magnetohydrodynamics,<br />

Vlasov–Maxwell equations.<br />

© 2001 by CRC Press LLC<br />

hydromagnetic turbulence<br />

hydromagnetics See magnetohydrodynamics.<br />

hydromagnetic shock wave An abrupt transition<br />

between two regions in a magnetized<br />

plasma, analogous to the acoustic shock wave in<br />

air. Hydromagnetic shock waves propagate relative<br />

to the plasma, <strong>and</strong> may be regarded as the<br />

short-wavelength limit of large-amplitude magnetoacoustic<br />

waves. There are fast <strong>and</strong> slow<br />

shock waves that correspond, respectively, to<br />

the fast <strong>and</strong> slow magnetoacoustic wave modes;<br />

a large-amplitude wave of either mode may<br />

steepen to form a shock.<br />

In a reference frame in which a shock is at<br />

rest, the flow speed of the plasma upstream of<br />

the shock is greater than the (fast or slow) magnetoacoustic<br />

wave speed, <strong>and</strong> downstream this<br />

inequality is reversed. As in the case of shocks<br />

in an ordinary gas, plasma flowing through a<br />

hydromagnetic shock undergoes heating <strong>and</strong> associated<br />

entropy production. In ideal magnetohydrodynamics<br />

a shock is infinitely thin; real<br />

hydromagnetic shocks have a structured transition<br />

region of finite thickness, comparable to the<br />

ion Larmor radius in many situations.<br />

Hydromagnetic shock waves are routinely<br />

observed in situ in collisionless plasmas in<br />

space. The high-speed solar wind passes<br />

through a bow shock when it encounters a planetary<br />

or cometary obstacle. From time to time<br />

material ejected from the solar corona drives<br />

transient shock waves into the heliosphere; if<br />

such a shock encounters a planetary magnetic<br />

field, it may produce magnetic storms <strong>and</strong> aurorae<br />

in the planetary magnetosphere <strong>and</strong> upper<br />

atmosphere. Shock waves can also be produced<br />

internally in the solar wind as fast streams catch<br />

up with slower streams; these shocks are frequently<br />

observed from about 3 to about 10 astronomical<br />

units from the sun. See hydromagnetic<br />

wave.<br />

hydromagnetic turbulence The turbulent,<br />

irregular fluctuations that can arise in a magnetized<br />

fluid or plasma. Just as turbulence arises at<br />

high Reynolds number in an ordinary unmagnetized<br />

fluid, hydromagnetic turbulence is associated<br />

with high magnetic Reynolds number (the<br />

ordinary Reynolds number with kinematic viscosity<br />

replaced by electrical resistivity). Mag-<br />

233

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