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Source: The Open Library

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1Eddy diffusivities for sensible heat, ozone, and momentum from eddy correlation and gradient measurements

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“Eddy diffusivities for sensible heat, ozone, and momentum from eddy correlation and gradient measurements” Metadata:

  • Title: ➤  Eddy diffusivities for sensible heat, ozone, and momentum from eddy correlation and gradient measurements
  • Author:
  • Language: English
  • Number of Pages: Median: 44
  • Publish Date:

“Eddy diffusivities for sensible heat, ozone, and momentum from eddy correlation and gradient measurements” Subjects and Themes:

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Access and General Info:

  • First Year Published: 1993
  • Is Full Text Available: Yes
  • Is The Book Public: Yes
  • Access Status: Public

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    Deposition (aerosol physics)

    It can be divided into two sub-processes: dry and wet deposition. The rate of deposition, or the deposition velocity, is slowest for particles of an intermediate

    Acid rain

    seeking to determine long-term trends, and established a network for dry deposition. Using a statistically based sampling design, NAPAP quantified the effects

    List of atmospheric dispersion models

    conditions (high turbulence). Algorithms for plume depletion by wet and dry deposition are also included in the model. This model was in development for approximately

    Kuwaiti oil fires

    into the atmosphere and then precipitated or fell out of the air via dry deposition and by rain. The pillar-like plumes frequently broadened and joined

    Precipitation

    2010-01-21. Unsworth, M H; Wilshaw, J C (September 1989). "Wet, occult and dry deposition of pollutants on forests". Agricultural and Forest Meteorology. 47 (2–4):

    Wadi

    the stream bed, causing an abrupt loss of energy and resulting in vast deposition. Wadis may develop dams of sediment that change the stream patterns in

    Dry ice

    process is called deposition, where CO2 changes from the gas to solid phase (dry ice). At atmospheric pressure, sublimation/deposition occurs at 194.7 K

    NOx

    the atmosphere may undergo dry or wet deposition and return to land in the form of HNO3/NO−3. Through this way, the deposition leads to nitrogen fertilization

    Fused filament fabrication

    suspension of solid powder particles in a liquid medium, which is dried after deposition. In this case, the material is generally pushed towards the nozzle

    Saharan dust

    (2010). "Iron speciation, solubility and temporal variability in wet and dry deposition in the Eastern Mediterranean". Marine Chemistry. 120 (1–4): 100–107