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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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thermocline<br />

to isopycnal surfaces. As a result, meso-scale<br />

eddies lead to a diapycnal flux. In contrast to<br />

cabbeling, where mixing is involved, the thermobaric<br />

effect arises from displacement only<br />

<strong>and</strong> does not require mixing.<br />

thermocline The region of large temperature<br />

gradient in oceans or lakes. Often there is<br />

a region of large temperature gradient near the<br />

surface of the ocean that appears only in summer<br />

<strong>and</strong> autumn; this is called seasonal thermocline.<br />

In low <strong>and</strong> middle latitudes, there is an<br />

ocean thermocline present all the time at depths<br />

between 200 <strong>and</strong> 1000 m, called the main or permanent<br />

thermocline. The e-folding thermocline<br />

depth scale in the ocean is about 1 km; in lakes<br />

it is much less <strong>and</strong> depends on the clarity of the<br />

water.<br />

thermohaline circulation A circulation that<br />

is driven by the buoyancy force. See also winddriven<br />

circulation.<br />

thermosphere See ionosphere.<br />

Theta aurora Rare form of the aurora extending<br />

across the polar cap from night- to dayside.<br />

Viewed from a high flying satellite, this arc<br />

combined with the auroral oval closely resembles<br />

the Greek letter (Theta). Observations of<br />

Theta aurora are limited to time periods when<br />

the interplanetary magnetic field has a northward<br />

component. See polar cap arc.<br />

thick-target A plasma in which a nonthermal<br />

population of energetic electrons is thermalized<br />

while generating radiation. The thermalization<br />

may be due to Coulomb collisions of<br />

the electrons with ambient particles or collective<br />

interactions with each other.<br />

thin-target A plasma that has no appreciable<br />

effect on an injected spectrum of non-thermal<br />

particles passing through it. A thin-target scenario<br />

would be applicable to electrons injected<br />

outwards through the corona.<br />

30 Doradus A star formation region in the<br />

Large Magellanic Cloud. It is located at RA =<br />

5.6 h <strong>and</strong> dec = −69.1 ◦ , <strong>and</strong> the main cluster<br />

subtends approximately 7 arcmin. This is a re-<br />

© 2001 by CRC Press LLC<br />

476<br />

gion of very active <strong>and</strong> current star formation,<br />

often referred to as a “starburst” <strong>and</strong> is the closest<br />

<strong>and</strong> most visible example of such a region. It<br />

contains a large collection of very early O-type<br />

<strong>and</strong> Wolf–Rayet stars. The core of the cluster, R<br />

136 (HD 38268), was once thought to be a single<br />

supermassive star but has now been resolved<br />

into a very dense cluster of young stars.<br />

Thompson circulation theorem See Kelvin<br />

circulation theorem.<br />

Thomson scattering Scattering of electromagnetic<br />

radiation by a charged particle that<br />

moves nonrelativistically in the process. For unpolarized<br />

incident radiation:<br />

<br />

dσ/d = e 2 /mc 2 2<br />

(1/2)(1 + cos θ) ,<br />

where θ is the scattering angle, <strong>and</strong> e <strong>and</strong> m are<br />

the charge <strong>and</strong> mass of the scatterer.<br />

The total Thomson cross-section is<br />

<br />

σT = 8π/3 e 2 /mc 2 2<br />

for electrons.<br />

= 0.665 × 10 −24 cm 2<br />

t’Hooft–Polyakov monopole (1974) A<br />

particular exactly describable magnetic-like<br />

monopole involving a vector Higgs field φ a a =<br />

1, 2, 3 (connected to a phase transition from<br />

a higher temperature configuration), in which<br />

each of the field components φ a is equal in value<br />

to the corresponding spatial coordinate x a . See<br />

cosmic topological defect, inflation, monopole,<br />

monopole excess problem, winding number.<br />

Thorpe displacement The distance a water<br />

parcel must be moved vertically so that it is<br />

in stable equilibrium with the surrounding water.<br />

Turbulence can generate local overturns of<br />

water parcels that lead to inversions of the density<br />

profile. If a water parcel at depth z1 must<br />

be moved to depth z2 to generate a monotonically<br />

increasing density profile, the displacement<br />

d1 = z2 −z1 is called the Thorpe displacement.<br />

Thorpe displacements are useful as an aid<br />

for defining the vertical extent of oceanic mixing<br />

events <strong>and</strong> overturns. However, since ocean

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