Encyclopedia

dry adiabat

dry adiabat

[¦drī ′ad·ē·ə‚bat]
(meteorology)
A line of constant potential temperature on a thermodynamic diagram.
McGraw-Hill Dictionary of Scientific & Technical Terms, 6E, Copyright © 2003 by The McGraw-Hill Companies, Inc.
References in periodicals archive
The dry adiabat is followed upward (blue arrow) to the LCL, where the saturation mixing ratio line intersects it.
In studies of the general circulation and of tropical convection, he always extolled the importance of vertical mixing by cumulonimbus convection, and became known for his catch-phrase "up moist-down dry," referring to the upward motion in a convective core following a moist adiabat, and the large-scale downward motion in the Hadley Cell and trade wind regions following the dry adiabat. There was also the famous expression known as "the Bill Gray question," where after a theoretical or dry presentation, he would congratulate the author on his insights, enthusiasm, and hard work, but would ask, "But what does it all mean?"
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