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instability

 
American Heritage Dictionary:

in·sta·bil·i·ty

(ĭn'stə-bĭl'ĭ-tē) pronunciation
n., pl., -ties.
  1. Lack of physical stability; unsteadiness.
  2. The quality or condition of being erratic or undependable: emotional instability; political instability.

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Roget's Thesaurus:

instability

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noun

  1. The quality or condition of being physically unsteady: precariousness, ricketiness, shakiness, unstableness, unsteadiness, wobbliness. See flexible/rigid.
  2. The quality or condition of being erratic and undependable: insecureness, insecurity, precariousness, shakiness, unstableness, unsteadiness, unsureness. See change/persist, strong/weak.

Antonyms by Answers.com:

instability

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n

Definition: imbalance, inconstancy
Antonyms: balance, constancy, soundness, stability, steadfastness

The condition of a parcel of air which has positive buoyancy, and thus a tendency to rise through the atmosphere. It is the temperature of the parcel relative to the ambient air which is critical, since this affects densities. A parcel remains unstable if it cools more slowly than the surrounding, stationary air. Absolute instability occurs when an air parcel, displaced vertically, is hastened in the direction of the displacement, and such a move will be checked when the temperature of the parcel is at one with its surroundings. The potential instability of a parcel of air can be calculated using a tephigram.

Conditional instability occurs when a parcel of air would become unstable if lifted by some other force. This can take place when a lower, stable parcel of air is overlain by an unstable layer. If any agency, such as a mountain, or the moistening of the lower-level air, can ‘nudge’ it upwards, it will become unstable. Convective instability is a tendency of an air parcel towards instability when it has been lifted bodily until completely saturated. This will often occur when it responds to the inevitable stirrings in the atmosphere.

The atmosphere is said to be unstable if the environmental lapse rate is greater than both the dry and saturated adiabatic lapse rates; that is, when the fall of temperature with height of the environmental air is more rapid than that experienced by a rising air parcel, so that the air parcel continues to be less dense than the ambient air.

In a structure, the sudden loss of stiffness that limits its load-carrying capability, and in some cases results in the structure’s failure.


Lack of stability in a joint, often through lax ligaments associated with hyperflexibility. Joint instability predisposes an athlete to injuries such as recurrent dislocations.

i. A state of the atmosphere in which a parcel of air will continue to rise, if for any reason, it is pushed up. Any instability in the atmosphere means turbulent conditions exist. The environmental lapse rate (ELR) in this case will be higher than both dry and saturated adiabatic lapse rates. Dry adiabatic lapse rate (DALR) is the rate of decrease of temperature with height of a parcel of dry air lifted adiabatically. Its value is 3°/1000 ft. Saturated adiabatic lapse rate (SALR) is the lapse rate of a parcel of saturated air and its value is 1.5°/1000 ft.

Picture 1 of instability


ii. A tendency of a body to continue moving away from its original state when disturbed by an external force and to continue after that force has been withdrawn.
iii. The failure of structures, such as the buckling of plates and panels under compression, and the failure of struts under end loads.

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Wikipedia on Answers.com:

Instability

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A ball on the top of a hill is an unstable situation.

In numerous fields of study, the component of instability within a system is generally characterized by some of the outputs or internal states growing without bounds. Not all systems that are not stable are unstable; systems can also be marginally stable or exhibit limit cycle behavior.

In control theory, a system is unstable if any of the roots of its characteristic equation has real part greater than zero (or if zero is a repeated root). This is equivalent to any of the eigenvalues of the state matrix having either real part greater than zero, or, for the eigenvalues on the imaginary axis, the algebraic multiplicity being larger than the geometric multiplicity.

In structural engineering, a structure can become unstable when excessive load is applied. Beyond a certain threshold, structural deflections magnify stresses, which in turn increases deflections. This can take the form of buckling or crippling. The general field of study is called structural stability.

Atmospheric instability is a major component of all weather systems on Earth.

Contents

Fluid instabilities

Unstable flow structure generated from the collision of two impinging jets.

Fluid instabilities occur in liquids, gases and plasmas, and are often characterized by the shape that form; they are studied in fluid dynamics and magnetohydrodynamics. Fluid instabilities include:

Plasma instabilities

Plasma instabilities can be divided into two general groups (1) hydrodynamic instabilities (2) kinetic instabilities. Plasma instabilities are also categorised into different modes - see this paragraph in plasma stability.

Instabilities of stellar systems

Galaxies and star clusters can be unstable, if small perturbations in the gravitational potential cause changes in the density that reinforce the original perturbation. Such instabilities usually require that the motions of stars be highly correlated, so that the perturbation is not "smeared out" by random motions. After the instability has run its course, the system is typically "hotter" (the motions are more random) or rounder than before. Instabilities in stellar systems include:

See also

Plasma stability

Notes

  1. ^ Shengtai Li, Hui Li "Parallel AMR Code for Compressible MHD or HD Equations" (Los Alamos National Laboratory) [1]
  2. ^ Merritt, D.; Sellwood, J. (1994), "Bending Instabilities of Stellar Systems", The Astrophysical Journal 425: 551–567, Bibcode 1994ApJ...425..551M, doi:10.1086/174005 

External links


Translations:

Instability

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Dansk (Danish)
n. - usikkerhed, ustadighed, instabilitet

Nederlands (Dutch)
onevenwichtigheid, labiliteit, onvastheid

Français (French)
n. - instabilité, (Mécan) déséquilibrage, (Météo) instabilité, manque de solidité, mobilité, instabilité (de caractère)

Deutsch (German)
n. - Instabilität, Labilität

Ελληνική (Greek)
n. - αστάθεια, ρευστότητα

Italiano (Italian)
instabilità

Português (Portuguese)
n. - instabilidade (f)

Русский (Russian)
неустойчивость

Español (Spanish)
n. - inestabilidad, desequilibrio

Svenska (Swedish)
n. - instabilitet, obeständighet

中文(简体)(Chinese (Simplified))
不安定, 基础薄弱, 不稳定

中文(繁體)(Chinese (Traditional))
n. - 不安定, 基礎薄弱, 不穩定

한국어 (Korean)
n. - 불안정, 변하기 쉬움

日本語 (Japanese)
n. - 不安定, 不安定状態

العربيه (Arabic)
‏(الاسم) عدم استقرار‏

עברית (Hebrew)
n. - ‮חוסר יציבות, חוסר שיווי-משקל, אי-סדירות‬


 
 
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