Temperature Inversion 2 : A layer of the atmosphere in which the temperature is constant or increases with height. Such layers are usually stable against convection and mixing from below
A. Barrie Pittock (Commonwealth Scientific and Industrial Research Organization Division of Atmospheric Research), Thomas P. Ackerman (National Aeronautics and Space Administration Ames Research Center), Paul J. Crutzen (Max Planck InstitUl fUr Chemie), Michael C. MacCracken (Lawrence Livermore National Laboratory), Charles S. Shapiro (San Francisco State University and Lawrence Livermore National Laboratory), Richard P. Turco (Rand D Associates In collaboration with: v. Aleksandrov, P. Connell, G. Golitsyn, T. Harvey, S. Kang, K. Peterson, and G. Tripoli), Scientific Committee on Problems of the Environment SCOPE 28, Environmental Consequences of Nuclear War Volume I. Physical and Atmospheric Effects, Appendix 2: Glossary, Published on behalf of the Scientific Committee on Problems of the Environment SCOPE (The International Council of Scientific Unions ICSU) by John Wiley & Sons, New York, USA 1986. http://dge.stanford.edu/SCOPE/SCOPE_28_1/SCOPE_28- 1_3.2_Appendix2_309-322.pdf, (Env Consequences of Nucl War - Phys & Atm Effects - Amer) {996}
