long-period oscillation - Definition. Was ist long-period oscillation
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Was (wer) ist long-period oscillation - definition

COOL TEMPERATE CLIMATIC INTERSTADIAL
Bølling period; Bølling interstadial; Bølling/Allerød; Bolling period; Bolling/Allerod; Bolling Oscillation; Bolling interstadial; Bølling Oscillation; Bolling oscillation; Bölling oscillation

Long-period variable star         
  • Light curves of four [[Mira variable]]s in the [[galaxy]] [[Centaurus A]]
DESCRIPTION FOR CERTAIN COOL LUMINOUS PULSATING VARIABLE STARS
Long-Period Variable Star; Long-period variables; Long period variable; Long period variables; Long-period variable stars; Long period variable star; Long period variable stars; Long-period-variable stars; Long-period-variable star; Long-period-variable; Long-period-variables; LPV star; LPV stars; Long-period variable; OGLE small amplitude red giant
The descriptive term long-period variable star refers to various groups of cool luminous pulsating variable stars. It is frequently abbreviated to LPV.
Self-oscillation         
  • Schematic representation of a self-oscillation as a positive feedback loop.  The oscillator ''V'' produces a feedback signal ''B''.  The controller at ''R'' uses this signal to modulate the external power ''S'' that acts on the oscillator.  If the power is modulated in phase with the oscillator's velocity, a negative damping is established and the oscillation grows until limited by nonlinearities.
Self oscillation; Self-exciting oscillation; Self‑oscillation; Self-oscillator
Self-oscillation is the generation and maintenance of a periodic motion by a source of power that lacks any corresponding periodicity. The oscillator itself controls the phase with which the external power acts on it.
Bølling oscillation         
The Bølling oscillation, also Bølling interstadial,Whittow, John (1984). Dictionary of Physical Geography.

Wikipedia

Bølling oscillation

The Bølling oscillation, also Bølling interstadial, was a cool temperate climatic interstadial between the glacial Oldest Dryas and Older Dryas stadials, between 14,700 and 14,100 BP, near to the end of the last glacial period. It is named after a peat sequence discovered at Bølling lake in central Jutland, Denmark. It is used to describe a period of time in relation to Pollen zone Ib—in regions where the Older Dryas is not detected in climatological evidence, the Bølling–Allerød is considered a single interstadial period.