TROPOSPHERIC AND STRATOSPHERIC TEMPERATURE CHANGES ASSOCIATED WITH PRESSURE CHANGES

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  • 1 Massachusetts Institute of Technology
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Abstract

The hypothesis is investigated that there is a physical difference between the development and motion components of a surface pressure change. Temperature changes indicate that deepening and filling are accompanied by high-level heating and cooling, respectively, while the motion part of pressure changes is associated with low-level temperature variations.

Abstract

The hypothesis is investigated that there is a physical difference between the development and motion components of a surface pressure change. Temperature changes indicate that deepening and filling are accompanied by high-level heating and cooling, respectively, while the motion part of pressure changes is associated with low-level temperature variations.

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