Encyclopedia of Physical Science and Technology, Volume 2Academic Press, 1992 - Physical sciences |
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Page 282
... PLUME INSTANTANEOUS PLUME MEAN WIND DIRECTION = TIME MEAN AXIS OF PLUME FIG . 1. Comparison of an instantaneous plume with a time - averaged plume . FIG . 2. Earth - boundary problem . Stability class A B C D E F Urban 0.15 0.15 0.20 ...
... PLUME INSTANTANEOUS PLUME MEAN WIND DIRECTION = TIME MEAN AXIS OF PLUME FIG . 1. Comparison of an instantaneous plume with a time - averaged plume . FIG . 2. Earth - boundary problem . Stability class A B C D E F Urban 0.15 0.15 0.20 ...
Page 288
... plume . This higher temperature causes the plumes to be buoyant and induces the phenomenon called plume rise . Some plumes are emitted at about ambient temperature but are made up of gases whose composition and density are much ...
... plume . This higher temperature causes the plumes to be buoyant and induces the phenomenon called plume rise . Some plumes are emitted at about ambient temperature but are made up of gases whose composition and density are much ...
Page 289
... plume centerline is the total excess heat of the plume . Breakup Phase . It has been observed that plume rise continues after the thermal phase , progressing to a situation in which atmospheric turbulence begins to dominate the mixing ...
... plume centerline is the total excess heat of the plume . Breakup Phase . It has been observed that plume rise continues after the thermal phase , progressing to a situation in which atmospheric turbulence begins to dominate the mixing ...
Contents
Guide to Using the Encyclopedia ix Atomic Physics | 339 |
Approximations and Expansions 1 Atomic Spectrometry | 357 |
Archaeological Geology 31 Atomic Spectroscopy | 381 |
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