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...to absorb moisture from the atmosphere and below which it will not absorb atmospheric moisture. [[Category:Atmospheric thermodynamics]] ...

...fter [[David Brunt]] and [[Vilho Väisälä]]. It can be used as a measure of atmospheric stratification. where the Brunt–Väisälä frequency <math>N</math> is:<ref>{{Cite book|title=Atmospheric and oceanic fluid dynamics: fundamentals and large-scale circulation|last=V ...

...path permeable to [[heat]]. Thermal equilibrium obeys the [[zeroth law of thermodynamics]]. A system is said to be in thermal equilibrium with itself if the tempera ....H., Yngvason, J. (1999). The physics and mathematics of the second law of thermodynamics, ''Physics Reports'', '''314''..a': 1–96, p. 55–56.</ref> ...

{{Thermodynamics|cTopic='''[[Material properties (thermodynamics)|Material properties]]'''}} In [[thermal physics]] and [[thermodynamics]], the '''heat capacity ratio''', also known as the '''adiabatic index''', ...

{{Thermodynamics|expanded=Potentials}} ...y]], etc.). The change in the free energy is the maximum amount of [[Work (thermodynamics)|work]] that the system can perform in a [[Thermodynamic process|process]] ...

{{Thermodynamics}} ...ned in terms of [[microscopic]] constituents by [[statistical mechanics]]. Thermodynamics applies to a wide variety of topics in [[science]] and [[engineering]], esp ...

In [[thermodynamics]], the '''Joule–Thomson effect''' (also known as the '''Joule–Kelvin effect |title=Fundamentals of Classical and Statistical Thermodynamics ...

{{Thermodynamics|expanded=Potentials}} ...e [[maximum]] amount of [[Work (thermodynamics)|work]], other than [[Work (thermodynamics)#Pressure–volume work|pressure-volume work]], that may be performed by a [[ ...

{{Thermodynamics |potentials}} In [[thermodynamics]], '''enthalpy''' {{IPAc-en|ˈ|ɛ|n|θ|əl|p|i|audio=en-US-enthalpy.ogg}}, is t ...

...he nozzle is choked, the pressure at the nozzle exit plane is greater than atmospheric pressure, and extra terms must be added to the above equation to account fo ...eb.mit.edu/16.unified/www/SPRING/propulsion/notes/node139.html 16.Unified: Thermodynamics and Propulsion, Prof. Z. S. Spakovszky]. Scroll down to "Performance of Tur ...

* [[Atmospheric physics]] – the study of the application of physics to the atmosphere * [[Thermodynamics]] – the branch of physical science concerned with heat and its relation to ...

...omponent or source. (This is to be distinguished from Temperature Noise in Thermodynamics or Principal Interferrometric Analysis Over Cross-Type Interference Between ...temperature is much higher, such as an antenna at lower frequencies where atmospheric noise dominates. Then there will be little degradation of the SNR. On the o ...

...s physical explanations for many phenomena of everyday life, such as why [[atmospheric pressure]] changes with [[altitude]], why wood and oil float on water, and ...Bettini|first1=Alessandro|title=A Course in Classical Physics 2—Fluids and Thermodynamics|date=2016|publisher=Springer|isbn=978-3-319-30685-8|page=8}}</ref><ref>{{ci ...

...Sears and Salinger, 1975: Thermodynamics, Kinetic Theory, and Statistical Thermodynamics. Third edition. Addison-Wesley Publishing Co.</ref> The "[[rotational tempe ...K for N₂ and 2156 K for O₂.<ref name=":0" /> Typical atmospheric temperatures are not high enough to activate vibration in N₂ and ...

...close to [[absolute zero]]; a pressure of more than twenty times normal [[atmospheric pressure]] is necessary. ==Thermodynamics== ...

From the laws of [[thermodynamics]]: ...ng-diverging nozzle used. It varies slightly with altitude due to changing atmospheric pressure, but can be up to 70%. Most of the remainder is lost as heat in th ...

{{Short description|Atmospheric phenomenon causing planetary warming}} {{about|the atmospheric phenomenon causing planetary warming|the general heating or cooling of Eart ...

{{Thermodynamics sidebar |material}} In [[thermodynamics]], the '''specific heat capacity''' (symbol {{mvar|''c''}}) of a substance ...

{{Thermodynamics}} ...st1=Gordon |last2=Sonntag |first2=Richard |title=Fundamentals of Classical Thermodynamics |date=1978 |publisher=John Wiley & Sons |location=Chapter 4.7, Definition o ...

...forms its planetary [[atmosphere]]. The atmosphere of [[Earth]] creates [[Atmospheric pressure|pressure]], absorbs most [[meteoroid]]s and [[ultraviolet]] [[Sola ..., and 0.4% over the entire atmosphere. Air composition, temperature, and [[atmospheric pressure]] vary with altitude. Within the atmosphere, air suitable for use ...