User:Milton Beychok/Sandbox: Difference between revisions

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{{Image|Lapse rates.png|right|292px|Diagram of the various lapse rates defining the change of atmospheric temperature with altitude.}}
{{Image|Lapse rates.png|right|292px|Diagram of the various lapse rates defining the change of atmospheric temperature with altitude.}}


The decrease of an atmospheric variable with height, the variable being temperature, unless otherwise specified.
The '''lapse rate''' (symbol <math>\Gamma</math>) refers to the change of an atmospheric variable with a change of altitude, the variable being [[temperature]] unless another variable is specified (such as [[pressure]], [[Density (chemistry)|density]], [[humidity]] or [[wind speed]]).<ref>The atmospheric lapse rate is very often defined as the negative change of temperature with a change of altitude. That leads to statements such as "A positive lapse rate indicates temperatures cooling as height increases while a negative lapse rate indicates warming as height increases" which is counter-intuitive since lapse rates are usually expressed as a negative number (i.e., - 6.5 K/km)</ref> While usually applied to Earth's atmosphere, the concept of lapse rates can be extended to atmospheres (if any) that exist on other planets.
 
 
 
 
 








<ref>{{cite book|author=Mark Zachary Jacobson|title=Fundamentals of Atmospheric Modeling|publisher=Cambridge University Press|edition=2nd|year=2005|isbn=0-521-83970-X}}</ref><br/>
<ref>{{cite book|author=C. Donald Ahrens|title=Meteorology Today|publisher=Brooks/Cole Publishing|edition=8th|year=2006|isbn=0-495-01162-2}}</ref>


== References ==
== References ==
{{reflist}}
{{reflist}}
== Hold items ==
<ref>{{cite book|author=Mark Zachary Jacobson|title=Fundamentals of Atmospheric Modeling|publisher=Cambridge University Press|edition=2nd|year=2005|isbn=0-521-83970-X}}</ref><br/>
<ref>{{cite book|author=C. Donald Ahrens|title=Meteorology Today|publisher=Brooks/Cole Publishing|edition=8th|year=2006|isbn=0-495-01162-2}}</ref>

Revision as of 18:41, 21 August 2009

(CC) Diagram: Milton Beychok
Diagram of the various lapse rates defining the change of atmospheric temperature with altitude.

The lapse rate (symbol ) refers to the change of an atmospheric variable with a change of altitude, the variable being temperature unless another variable is specified (such as pressure, density, humidity or wind speed).[1] While usually applied to Earth's atmosphere, the concept of lapse rates can be extended to atmospheres (if any) that exist on other planets.






References

  1. The atmospheric lapse rate is very often defined as the negative change of temperature with a change of altitude. That leads to statements such as "A positive lapse rate indicates temperatures cooling as height increases while a negative lapse rate indicates warming as height increases" which is counter-intuitive since lapse rates are usually expressed as a negative number (i.e., - 6.5 K/km)

Hold items

[1]
[2]

  1. Mark Zachary Jacobson (2005). Fundamentals of Atmospheric Modeling, 2nd. Cambridge University Press. ISBN 0-521-83970-X. 
  2. C. Donald Ahrens (2006). Meteorology Today, 8th. Brooks/Cole Publishing. ISBN 0-495-01162-2.