lapse$43355$ - definizione. Che cos'è lapse$43355$
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Cosa (chi) è lapse$43355$ - definizione

VERTICAL RATE OF CHANGE OF TEMPERATURE IN ATMOSPHERE
Absolute stable air; Temperature lapse rate; Moist adiabatic lapse rate; Dry adiabatic lapse rate; Absolute Stable Air; Lapse Rate; Adiabatic lapse rate; Adiabatic lapse; Environmental lapse rate; Atmospheric adiabatic cooling; Adiabatic Lapse; Atmospheric lapse rate; DALR
  • The latent heat of vaporization adds energy to clouds and storms.
  • [[Emagram]] diagram showing variation of dry adiabats (bold lines) and moist adiabats (dash lines) according to pressure and temperature
  • Polish]] side of the [[Tatra mountains]], May 2019.

Lapse rate         
The lapse rate is the rate at which an atmospheric variable, normally temperature in Earth's atmosphere, falls with altitude. Lapse rate arises from the word lapse, in the sense of a gradual fall.
lapse rate         
¦ noun the rate at which air temperature falls with increasing altitude.
time-lapse         
  • geraniums]]; 2 hours are compressed into a few seconds
  • [[Mung bean]] seeds germinating, a 10-day time-lapse in roughly 1 minute
  • newspaper=ESO Announcement}}</ref>
FILM TECHNIQUE WHERE THE FRAME RATE IS LOWER THAN THAT USED TO VIEW THE SEQUENCE
Fast motion; Time lapse photography; Time Lapse Photography; Time lapse; Time-Lapse Cinematography; Undercranking; Timelapse; Timelapse photography; Time lapse video; Time lapsed; Time-lapse; Time-lapse camera; Timelapse video; Timelapse recording; Shutter drag; History of time-lapse photography; Fast Motion; Time-lapse photo; Time-lapse imaging
¦ adjective denoting the photographic technique of taking a sequence of frames at set intervals to record changes that take place slowly over time.

Wikipedia

Lapse rate

The lapse rate is the rate at which an atmospheric variable, normally temperature in Earth's atmosphere, falls with altitude. Lapse rate arises from the word lapse, in the sense of a gradual fall. In dry air, the adiabatic lapse rate is 9.8 °C/km (5.4 °F per 1,000 ft). At Saturated Air Lapse Rate (SALR), where value is 1.1 °C/1000ft - 2.8 °C/1000ft as obtained from ICAO.

It corresponds to the vertical component of the spatial gradient of temperature. Although this concept is most often applied to the Earth's troposphere, it can be extended to any gravitationally supported parcel of gas.