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A Neutral Atmosphere

For a neutral atmopshere the lapse rate is exactly equal to the DALR. In this case rising or sinking unsaturated air would cool or warm at the same rate as the air around it. At every layer in the atmosphere it would have the same temperature and density as the air aurrounding it and so the air would neither tend to rise or sink. The atmosphere is said to be neutrally stable. 

 

For saturated air, neutral stability exists when the environemtal lapse rate is equal to the moist adiabatic rate. 

© 2015 by UniMet.

* All information on this site has come from lecture notes and the associated course text books: 'Atmospheric Science: An introductory survey, 2nd edition, J. M. Hobbs and P. V. Wallace' and 'Meteorology Today: An Introduction to Weather, Climate and the Environment, 10th edition (International), C. D. Ahrens.' Some sections may have been rephrased and altered slightly but all content came from the above mentioned sources unless otherwise stated. 

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