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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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coastally trapped waves<br />

coastally trapped waves Waves generated<br />

by wind blowing over a stratified ocean with a<br />

shelf topography. These are hybrid waves with<br />

characteristics of both Kelvin <strong>and</strong> continental<br />

shelf waves. In the northern hemisphere, waves<br />

propagate alongshore with the coast on the right.<br />

coastal ocean Shallow water generally situated<br />

over continental shelves; often, but not<br />

always, case 2 waters. See case 2 water.<br />

coastal upwelling or downwelling The resultant<br />

ocean volume transport in the Ekman<br />

layer is at right angles to <strong>and</strong> to the right of the<br />

winddirectioninthenorthernhemisphere. Ifthe<br />

wind blows parallel to the coast <strong>and</strong> is directed<br />

with the coast on the right/left in the northern/southern<br />

hemisphere, water in the Ekman<br />

layer will tend to move away from the coast <strong>and</strong><br />

will be replaced by water moving upward from<br />

below the layer. This is called the coastal upwelling.<br />

Regions particularly noted for coastal<br />

upwelling are the coast of Peru, the U.S. West<br />

Coast, <strong>and</strong> the coasts of Northwest <strong>and</strong> Southwest<br />

Africa. There is also upwelling off Somalia<br />

<strong>and</strong> Arabia during the Southwest Monsoon.<br />

Likewise, if the wind blows parallel to the<br />

coast <strong>and</strong> is directed with the coast on the<br />

left/right in the northern/southern hemisphere,<br />

water in the Ekman layer will tend to move toward<br />

the coast <strong>and</strong> will move downward to replace<br />

water below the layer. This is called the<br />

coastal downwelling.<br />

Coastal Zone Color Scanner (CZCS) A<br />

multi-spectral line scanner operational from October<br />

1978 to June 1986, which had four channels<br />

devoted to ocean color, each of 20 nm<br />

b<strong>and</strong>width <strong>and</strong> centered at 443, 520, 550, <strong>and</strong><br />

670 nanometers.<br />

cobble A sediment particle between 64 <strong>and</strong><br />

250 mm in diameter (definitions vary). Generally<br />

rounded due to abrasive action.<br />

coble creep (grain-boundary diffusion creep)<br />

A deformation mechanism for the diffusion<br />

creep of a fine-grained polycrystal, in which the<br />

creep rate is controlled by diffusion along the<br />

grain boundary. It was first proposed by Coble<br />

© 2001 by CRC Press LLC<br />

in 1963. For a spherical grain Coble found<br />

ε= DGBδσ<br />

αd 3 kT<br />

where (ε) is the creep rate, DGB is the grain<br />

boundary self-diffusion coefficient, δ is the<br />

thickness, σ is the differential stress, d is the<br />

grain size, is the atomic volume, k is Boltzmann’s<br />

constant,α is a numerical coefficient depending<br />

on the grain shape <strong>and</strong> the boundary<br />

conditions for σ , <strong>and</strong> T is the temperature. It is<br />

a linear rheology (n = 1, n is stress sensitivity<br />

of creep rate at steady-state stage) with a high<br />

sensitivity to grain-size (strain rate depends on<br />

the grain size as ε ∝ 1/d 3 ).<br />

cobpoint Short for “connection of observer<br />

point”, describing the point on a shock to which<br />

the observer is connected magnetically. See<br />

connection longitude.<br />

coda wave A wave group following P- <strong>and</strong> Swaves<br />

on a seismogram. For a near earthquake,<br />

there are many cases in which the directions of<br />

arrival of coda waves cannot be determined. The<br />

coda waves are considered to consist mainly of<br />

incoherent waves scattered in a small-scale heterogeneous<br />

structure in the Earth. The spectrum<br />

of coda waves hardly depends on hypocentral<br />

distances or ray paths of seismic waves. Coda Q<br />

as a measure of energy redistribution <strong>and</strong> magnitude<br />

of earthquakes can be determined from, respectively,<br />

decreasing rate of amplitude of coda<br />

waves <strong>and</strong> their duration time.<br />

coefficient of thermal conductivity A measure<br />

of the ability of a material to transport<br />

thermal energy. In solar physics the coefficient<br />

of thermal conductivity, usually denoted κ, is<br />

used in the calculation of heat flux transfer in a<br />

fully ionized medium. When a magnetic field<br />

is present, the coefficient of thermal conductivity<br />

depends on whether one is considering<br />

the heat transfer parallel (κ) or perpendicular<br />

(κ⊥) tothefield. In the solar corona, the ratio<br />

of these two coefficients is κ⊥/κ 10 −13 ,<br />

<strong>and</strong> so for most situations, κ⊥ is ignored <strong>and</strong><br />

we have κ = κ0 = 9 × 10 −12 T 5/2 Wm −1<br />

K −1 (the Spitzer conductivity). The T 5/2 dependence<br />

of κ0 makes energy transport by thermal<br />

conduction negligible for low temperature

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