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As it measures moisture content in the atmosphere, the dew point depression is also an important indicator in agricultural and forest meteorology, particularly in predicting
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activity. Conversely, instability is increased when there is a mid-level dry layer (large dew point depression) known as a "
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increasing as dew point depression decreases. LCL height also factors in
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For a constant temperature, the smaller the difference, the more
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370:(LCL). LCL height is an important factor modulating severe
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46:. Unsourced material may be challenged and removed.
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629:Convective available potential energy (CAPE)
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426:Hakim, Gregory J.; Patoux, Jérôme (2017).
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106:Learn how and when to remove this message
343:temperature at a certain height in the
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44:adding citations to reliable sources
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591:Convective condensation level (CCL)
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797:Equivalent potential temperature (
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649:Conditional symmetric instability
495:Meteorological data and variables
996:Meteorological data and networks
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596:Lifting condensation level (LCL)
335:) is the difference between the
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581:Cloud condensation nuclei (CCN)
428:Weather: A Concise Introduction
31:needs additional citations for
844:Wet-bulb potential temperature
686:Level of free convection (LFC)
430:. Cambridge University Press.
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991:Severe weather and convection
887:Pressure-gradient force (PGF)
809:Sea surface temperature (SST)
644:Convective momentum transport
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354:there is, and the higher the
939:. You can help Knowledge by
701:Bulk Richardson number (BRN)
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905:Maximum potential intensity
671:Free convective layer (FCL)
634:Convective inhibition (CIN)
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986:Atmospheric thermodynamics
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839:Wet-bulb globe temperature
696:Maximum parcel level (MPL)
460:Atmospheric thermodynamics
394:", which is favorable for
368:lifted condensation levels
1001:Atmospheric science stubs
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819:Thermodynamic temperature
753:Forest fire weather index
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229:Thermodynamic equilibrium
741:Equivalent temperature (
654:Convective temperature (
538:Surface weather analysis
238:Measures and instruments
788:Potential temperature (
533:Surface solar radiation
374:. One example concerns
122:Humidity and hygrometry
778:Relative humidity (RH)
666:Equilibrium level (EL)
639:Convective instability
398:if the lower layer is
55:"Dew point depression"
867:Atmospheric pressure
834:Wet-bulb temperature
736:Dry-bulb temperature
731:Dew point depression
329:dew point depression
288:Wet-bulb temperature
151:Dew point depression
40:improve this article
933:atmospheric science
931:This article about
829:Virtual temperature
814:Temperature anomaly
508:Adiabatic processes
455:Wet-bulb depression
601:Precipitable water
199:Humidity buffering
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356:relative humidity
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137:Specific concepts
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57: –
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51:Find sources:
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29:This article
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941:expanding it
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783:Mixing ratio
758:Haines Index
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568:Condensation
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267:H. indicator
257:Mixing ratio
214:Liquid water
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96:January 2024
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38:Please help
33:verification
30:
872:Baroclinity
719:Dew point (
711:Temperature
611:Water vapor
364:cloud bases
360:troposphere
337:temperature
194:Evaporation
980:Categories
849:Wind chill
763:Heat index
621:Convection
558:Wind shear
543:Visibility
523:Lapse rate
413:References
396:convection
388:microburst
345:atmosphere
279:Hygrometer
247:Heat index
224:Nucleation
66:newspapers
548:Vorticity
528:Lightning
513:Advection
407:wildfires
392:dry punch
384:downburst
380:tornadoes
341:dew point
146:Dew point
897:Velocity
859:Pressure
773:Humidity
676:Helicity
518:Buoyancy
449:See also
352:moisture
209:Pressure
768:Humidex
681:K Index
501:General
400:buoyant
207:)
184:Density
80:scholar
434:
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935:is a
576:Cloud
87:JSTOR
73:books
937:stub
553:Wind
432:ISBN
386:and
366:and
339:and
333:T-Td
327:The
272:card
205:Atm.
59:news
586:Fog
284:Dry
189:Dew
174:Air
42:by
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