use of back air trajectories in interpreting atmospheric chemistry data
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use of back air trajectories in interpreting atmospheric chemistry data a review and bibliography by John M. Miller

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Published by National Oceanic and Atmospheric Administration, Environmental Research Laboratories in [Boulder, Colo.?] .
Written in English

Subjects:

  • Atmospheric chemistry.,
  • Transport theory -- Mathematical models.,
  • Air -- Pollution -- Mathematical models.,
  • Atmospheric diffusion -- Mathematical models.

Book details:

Edition Notes

StatementJohn M. Miller.
SeriesNOAA technical memorandum ERL ARL -- 155.
ContributionsEnvironmental Research Laboratories (U.S.)
The Physical Object
Pagination28 p. :
Number of Pages28
ID Numbers
Open LibraryOL17673611M

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In The use of back air trajectories in interpreting atmospheric chemistry data: A review and bibliography. NOAA Tech Mem ERL ARL National Oceanic and Atmospheric Administration, Silver Spring, Md. 28 p. Google ScholarCited by: 8. (4) Numerical transport methods use atmospheric dispersion modeling (e.g., air mass back trajectories) to study the advection regimes with subsequent distinction in periods with potential. A replacement for simple back trajectory calculations in the interpretation of atmospheric trace substance measurements Article in Atmospheric Environment 36(29) October with On the Construction, Comparison, and Variability of Airsheds for Interpreting Semivolatile Organic Compounds in Passively Sampled Air.

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The discussion is limited to a single plane because the physical principle can be demonstrated adequately in this way and because evaluation of the threedimensional momentum flux requires use of second-order tensors which are not used in this book. For the important atmospheric case of vertical shear of the x component, Eq. M.F. Larsen, in Encyclopedia of Atmospheric Sciences (Second Edition), Other Techniques. There are a few techniques that do not rely on telemetry. One used extensively is the chemical release technique in which a chemical tracer is released from the rocket payload as it traverses a range of altitude in the atmosphere. The tracer is then tracked photographically from two more sites on the. Thus the use of current hr upper-air data may produce significant biases in atmospheric transport calculations. Models that utilize the hydrodynamic equations of motion are capable of resolving smaller-scale features (Anthes and Warner ), but the computational expense of using these models is often prohibitive for long-term pollution Cited by: 8. Cambridge Core - Regional and World History: General Interest - Climate Change and the Course of Global History - by John L. BrookeAuthor: John L. Brooke.