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advection

   Also found in: Encyclopedia, Wikipedia 0.04 sec.
ad·vec·tion  (d-vkshn)
n.
1. The transfer of a property of the atmosphere, such as heat, cold, or humidity, by the horizontal movement of an air mass: Today's temperatures were higher due to the advection of warm air into the region.
2. The rate of change of an atmospheric property caused by the horizontal movement of air.
3. The horizontal movement of water, as in an ocean current.

[Latin advecti, advectin-, act of conveying, from advectus, past participle of advehere, to carry to : ad-, ad- + vehere, to carry; see wegh- in Indo-European roots.]

ad·vective adj.

advection
Noun
Physics the transferring of heat in a horizontal stream of gas [Latin ad- to + vehere to carry]

advection  (d-vkshn)
1. The transfer of a property of the atmosphere, such as heat, cold, or humidity, by the horizontal movement of an air mass.
2. The rate of change of an atmospheric property caused by the horizontal movement of air.
3. The horizontal movement of water, as in an ocean current.

advection
the horizontal movement of elements of the atmosphere. Cf. convection. — advective, adj.
See also: Atmosphere
ThesaurusLegend:  Synonyms Related Words Antonyms
Noun1.advection - (meteorology) the horizontal transfer of heat or other atmospheric properties
meteorology - the earth science dealing with phenomena of the atmosphere (especially weather)
temperature change - a process whereby the degree of hotness of a body (or medium) changes


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All atmospheric models are composed of a dynamical core, which represents advection, the pressure gradient force, and gravitational acceleration; and of a set of parameterizations that represent all other physical processes in the model.
In addition, Clemson University's new melt-folding technology, called "chaotic advection," can create a repeatable stack of up to 1000 semi-continuous microlayers (see "Learn More" box) in a feedblock-like device called a SmartBlender.
The liberated ions move, via advection or diffusion, to areas of lower stress, either just adjacent to the area of dissolution or elsewhere in the pore system, where the dissolved material may reprecipitate, forming burial-diagenetic cements.
 
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